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Sample records for earth moessbauer spectroscopy

  1. {sup 57}Fe Moessbauer spectroscopy applied to the study of rare-earth iron permanent magnets

    Energy Technology Data Exchange (ETDEWEB)

    Persiano, A.I.C. [Departamento de Fisica-UFMG (Brazil)], E-mail: persiano@fisica.ufmg.br

    1999-11-15

    A survey of some important applications of {sup 57}Fe Moessbauer spectroscopy to the study of local magnetic and structural characteristics of the main phases in the rare-earth-transition metal (RE-TM) class of materials used in the development of the new generations of high performance permanent magnets is presented. A brief history of the hard magnets evolution in the last decades is followed by the description and interpretation of the main effects on the hyperfine interactions revealed by the Moessbauer technique. The contribution of the distinct crystallographic iron sites to the saturation magnetization of the rare-earth iron compounds is discussed in terms of the corresponding types of magnetic coupling, based mainly on the iron-iron distances, the number of iron neighbors and the respective hyperfine fields. These features are inferred from the energy of the resonant absorption by the iron sites 4e/4c/8j{sub 1}/8j{sub 2}/16k{sub 1}/16k{sub 2} in the Nd{sub 2}Fe{sub 14}B, sites 6c/9d/18f/18h in the light RE{sub 2}Fe{sub 17}N{sub 3} and 8f/8i/8j in the RE(Fe{sub 12-x}TM{sub x}) phases. The direction of the easy axis of magnetization is discussed taking into account the effects due to the interaction between the local magnetization vector and the electric field gradients. Some other characteristics such as the occupancy of the TM atoms in the 1 : 12 compounds as well as in some hybrid (Fe +TM) 2 : 17 structures are also discussed in terms of the changes in the relative subspectral areas. The effects regarding charge transfers and lattice expansions due to the incorporation of nitrogen and also of other different interstitial elements to the 2 : 17 rhombohedral structure are discussed considering the relative changes of the isomer shifts in comparison with the alterations in the parameter due exclusively to the respective volume expansions.

  2. Moessbauer spectroscopy with actinide elements

    Energy Technology Data Exchange (ETDEWEB)

    Potzel, W.; Moser, J.; Asch, L.; Kalvius, G.M. (Technische Univ. Muenchen, Garching (Germany, F.R.)

    1983-01-01

    Although formally equivalent to the lanthanide (4f) elements, the light actinides show a much more varied behaviour due to the larger spatial extent and ionizability of the 5f electrons. The application of Moessbauer spectroscopy for the determination of electronic properties of the actinides is outlined. Emphasis is put on high pressure Moessbauer experiments using the 60 keV transition in /sup 237/Np to study questions of delocalization of 5f electrons.

  3. Moessbauer spectroscopy as a tool in astrobiology

    Energy Technology Data Exchange (ETDEWEB)

    Schroeder, Christian, E-mail: schroedc@uni-mainz.de; Klingelhoefer, Goestar, E-mail: klingel@mail.uni-mainz.de [Johannes Gutenberg-Universitaet, Institut fuer Anorganische Chemie und Analytische Chemie (Germany); Bailey, Brad E., E-mail: bebailey@ucsd.edu; Staudigel, Hubert, E-mail: hstaudigel@ucsd.edu [University of California San Diego, Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography (United States)

    2005-11-15

    Two miniaturized Moessbauer spectrometers are part of the Athena instrument package of the NASA Mars Exploration Rovers, Spirit and Opportunity. The primary objectives of their science investigation are to explore two sites on the surface of Mars where water may once have been present, and to assess past environmental conditions at those sites and their suitability for life. Aqueous minerals - jarosite at Meridiani Planum, Opportunity's landing site, and goethite in the Columbia Hills in Gusev Crater, Spirit's landing site - were identified by Moessbauer spectroscopy, thus providing in situ proof of water being present at those sites in the past. The formation of jarosite in particular puts strong constraints on environmental conditions during the time of formation and hence on the evaluation of potential habitability. On Earth Moessbauer spectroscopy was used to investigate microbially induced changes in Fe oxidation states and mineralogy at the Loihi deep sea mount, a hydrothermal vent system, which might serve as an analogue for potential habitats in the Martian subsurface and the sub-ice ocean of Jupiter's icy moon Europa.

  4. Moessbauer spectroscopy of actinide intermetallics

    Energy Technology Data Exchange (ETDEWEB)

    Kalvius, G.M.; Potzel, W.; Moser, J.; Litterst, F.J.; Asch, L.; Zaenkert, J.; Potzel, U.; Kratzer, A.; Wunsch, M. (Technische Univ. Muenchen, Garching (Germany, F.R.). Fakultaet fuer Physik); Gal, J.

    1985-04-01

    Due to their wider radical extent the 5f electrons may form bands of different width and hybridization in metallic compounds of the light actinides. This leads to a broad spectrum of magnetic properties ranging from the localized magnetism of the lanthanides to the itinerant electron magnetism often found in transition metal compounds. Also, the influence of the crystalline electric field tends to be more pronounced than in rare earth compounds, but is usually not as dominant as in the 3d series. Magnetic structures and the question of 5f electron delocalization will be reviewed with respect to actinide Moessbauer data and new results will be presented. In particular the influence of applying external pressure will be discussed.

  5. Hyperfine Interactions in Iron Meteorites: Comparative Study by Moessbauer Spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Oshtrakh, M. I., E-mail: oshtrakh@mail.utnet.ru [Ural State Technical University - UPI, Faculty of Physical Techniques and Devices for Quality Control (Russian Federation); Milder, O. B. [Ural State Technical University - UPI, Faculty of Experimental Physics (Russian Federation); Grokhovsky, V. I. [Ural State Technical University - UPI, Faculty of Physical Techniques and Devices for Quality Control (Russian Federation); Semionkin, V. A. [Ural State Technical University - UPI, Faculty of Experimental Physics (Russian Federation)

    2004-11-15

    The iron meteorites Sikhote-Alin, Bilibino, Chinga and Dronino with different Ni concentration and terrestrial age were studied by Moessbauer spectroscopy. Different Moessbauer hyperfine parameters were determined for studied meteorites and possible Fe-Ni phases were supposed.

  6. Moessbauer spectroscopy in neptunium compounds

    Energy Technology Data Exchange (ETDEWEB)

    Nakamoto, Tadahiro; Nakada, Masami; Masaki, Nobuyuki; Saeki, Masakatsu [Japan Atomic Energy Research Inst., Tokyo (Japan)

    1997-03-01

    Moessbauer effects are observable in seven elements of actinides from {sup 232}Th to {sup 247}Cm and Moesbauer spectra have been investigated mainly with {sup 237}Np and {sup 238}U for the reasons of availability and cost of materials. This report describes the fundamental characteristics of Moessbauer spectra of {sup 237}Np and the correlation between the isomer shift and the coordination number of Np(V) compounds. The isomer shifts of Np(V) compounds had a tendency to increase as an increase of coordination number and the isomer shifts of Np(V) compounds showed broad distribution as well as those of Np(VI) but {delta} values of the compounds with the same coordination number were distributed in a narrow range. The {delta} values of Np(VI) complexes with O{sub x} donor set suggest that the Np atom in its hydroxide (NpO{sub 2}(OH){center_dot}4H{sub 2}O)might have pentagonal bipyramidal structure and at least, pentagonal and hexagonal bipyramidal structures might coexist in its acetate and benzoate. Really, such coexistence has been demonstrated in its nitrate, (NpO{sub 2}){sub 2}(NO{sub 3}){sub 2}{center_dot}5H{sub 2}O. (M.N.)

  7. Moessbauer spectroscopy study of interfaces for spintronics

    Energy Technology Data Exchange (ETDEWEB)

    Mantovan, R., E-mail: roberto.mantovan@mdm.infm.it; Wiemer, C.; Lamperti, A.; Georgieva, M.; Fanciulli, M. [Laboratorio Nazionale MDM CNR-INFM (Italy); Goikhman, A.; Barantsev, N.; Lebedinskii, Yu.; Zenkevich, A. [Moscow Engineering Physics Institute (Russian Federation)

    2009-06-15

    The submonolayer sensitivity and element-specificity of conversion electron Moessbauer spectroscopy, combined with the use of {sup 57}Fe enriched tracer layers, enable to carefully investigate thin films and interfaces at the atomic-scale. This paper reports on the main achievements we obtained so far in the study of structural, chemical, and magnetic properties of a variety of interfaces between oxides and Fe-based films having potential interest in the field of spintronics.

  8. Moessbauer Spectroscopy in South American Archaeology

    Energy Technology Data Exchange (ETDEWEB)

    Wagner, U.; Haeusler, W.; Wagner, F. E. [Technische Universitaet Muenchen, Physik-Department E15 (Germany); Shimada, I. [Southern Illinois University, Institute of Anthropology (United States)

    2003-06-15

    We report on an interdisciplinary approach to the study of early pottery finds from the Poma Archaeological Reserve, North Coast of Peru. The material is from a Formative kiln site at Batan Grande (1000-800 BC) and a ceramics workshop at Huaca Sialupe pertaining to the Middle Sican period (900-1100 AD). Moessbauer spectroscopy, neutron activation analysis, optical thin-section microscopy and X-ray diffraction were used to characterize the material. Numerous sherds of Sican black- and redware, bricks, moulds and kiln linings were studied. Local clay from the kiln site at Batan Grande, lumps of clay, and unfired sherds from Huaca Sialupe were used as model material for firing experiments under controlled conditions. By comparing the Moessbauer spectra from laboratory and field firings with the ancient materials, methods of early pottery making can be assessed.

  9. Moessbauer spectroscopy and scanning electron microscopy of the Murchison meteorite

    Science.gov (United States)

    Brown, Christopher L.; Oliver, Frederick W.; Hammond, Ernest C., Jr.

    1989-01-01

    Meteorites provide a wealth of information about the solar system's formation, since they have similar building blocks as the Earth's crust but have been virtually unaltered since their formation. Some stony meteorites contain minerals and silicate inclusions, called chondrules, in the matrix. Utilizing Moessbauer spectroscopy, we identified minerals in the Murchison meteorite, a carbonaceous chondritic meteorite, by the gamma ray resonance lines observed. Absorption patterns of the spectra were found due to the minerals olivine and phyllosilicate. We used a scanning electron microscope to describe the structure of the chondrules in the Murchison meteorite. The chondrules were found to be deformed due to weathering of the meteorite. Diameters varied in size from 0.2 to 0.5 mm. Further enhancement of the microscopic imagery using a digital image processor was used to describe the physical characteristics of the inclusions.

  10. Application of Moessbauer Spectroscopy to the Study of Corrosion

    Energy Technology Data Exchange (ETDEWEB)

    Cook, Desmond C. [Old Dominion University, Department of Physics (United States)

    2004-03-15

    Corrosion research, and the need to fully understand the effects that environmental conditions have on the performance of structural steels, is one area in which Moessbauer spectroscopy has become a required analytical technique. This is in part due to the need to identify and quantify the nanophase iron oxides that form on and protect certain structural steels, and that are nearly transparent to most other spectroscopic techniques. A review is given of the most recent Moessbauer characterization of rusts that have formed on structural steels exposed to different environments. Moessbauer spectroscopy is playing an important role in a new corrosion program in the United States in which steel bridges, old and new, are being evaluated for corrosion problems that may reduce their serviceable lifetimes. Moessbauer spectroscopy has been used to characterize the corrosion products that form the protective patina on weathering steel, as well those that form in adverse environments in which the oxide coating is not adherent or protective to the steel. Moessbauer spectroscopy has also become an important analytical technique for investigating the corrosion products that have formed on archeological artifacts, and it is providing guidance to aid in the removal of the oxides necessary for their preservation.

  11. Characterization of magnetic nano materials by Moessbauer spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Thakur, Sangeeta; Katyal, S C [Jaypee University of information technology, Waknaghat, Solan 173215 (India); Gupta, A; Reddy, V R [UGC-DAE Consortium for scientific research, Khandwa Road, Indore 452017 (India); Singh, M, E-mail: megha2k6@gmail.co [Department of physics, Himachal Pradesh University, Shimla 171005 (India)

    2010-03-01

    The use of a non-destructive nuclear-physical method, namely {sup 57}Fe Moessbauer spectroscopy, is discussed for the investigation of magnetic and structural arrangement of Fe-based nano-crystalline nickel-zinc-indium ferrites (NZIFO). Nano NZIFO particles (Ni{sub 0.58}Zn{sub 0.42}In{sub x}Fe{sub 2-x}O{sub 4}) with varied quantities of indium (x = 0, 0.1, 0.2) have been chemically synthesized through a reverse micelle reaction and investigated by X-ray diffraction, transmission electron microscopy and by magnetic and Moessbauer spectral studies. Here a comparison between low-temperature and room temperature Moessbauer spectra is presented. Well defined sextets at 5 K provide information about the structure and magnetic states of atoms located in different structural positions. The dependence of Moessbauer parameters, viz, isomer shift, quadrupole splitting, linewidth and hyperfine magnetic field on In{sup 3+} concentration have been discussed. Detailed Moessbauer results, as well as the interest of these materials both for applied science perspectives are presented. Moessbauer results are also supported by magnetization data. With these interesting ferromagnetic properties Indium substituted nano nickel-zinc ferrites have potential applications in magnetic storage data.

  12. High pressure Moessbauer spectroscopy of perovskite iron oxide

    CERN Document Server

    Nasu, S; Morimoto, S; Kawakami, T; Kuzushita, K; Takano, M

    2003-01-01

    High-pressure sup 5 sup 7 Fe Moessbauer spectroscopy using a diamond anvil cell has been performed for perovskite iron oxides SrFeO sub 3 , CaFeO sub 3 and La sub 1 sub / sub 3 Sr sub 2 sub / sub 3 O sub 3. The charge states and the magnetic dependency to pressure were determined. Pressure magnetic phase diagrams of these perovskite iron oxides are determined up to about 70 GPa. To be clear the magnetic ordered state, they are measured up to 7.8 T external magnetic fields at 4.5K. The phase transition of these perovskite oxides to ferromagnetisms with high magnetic ordered temperature is observed. In higher pressure, high spin-low spin transition of oxides besides CaFeO sub 3 is generated. The feature of Moessbauer spectroscopy, perovskite iron oxide and Moessbauer spectroscopy under high pressure are explained. (S.Y.)

  13. Fast data acquisition in Moessbauer spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Kalvius, G.M. (Technische Universitaet Muenchen, Garching, Ger.); Potzel, W.; Koch, W.; Forster, A.; Asch, L.; Wagner, F.E.; Halder, N.

    1977-01-01

    Three different gamma-ray detection systems for Moessbauer measurements at count rates above 10/sup 5/ s/sup -1/ are described. The first uses the fast output of an uncooled NaI(Tl) scintillation counter and will still provide energy discrimination at total pulse rates up to 10/sup 6/ s/sup -1/. Count rates up to some 10/sup 7/ s/sup -1/ can be handled by a tin-loaded plastic scintillation detector, but only with very limited energy resolution. For even higher photon intensities, the method of current integration is available. The various techniques are illustrated and compared on the basis of measurements with the Moessbauer resonances in /sup 170/Yb (84 keV), /sup 199/Hg (158 keV) and /sup 237/Np (60 keV).

  14. Anelastic Relaxation Mechanisms Characterization by Moessbauer Spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Soberon Mobarak, Martin Jesus, E-mail: msoberon@sep.gob.mx [Secretaria de Educacion Publica (Mexico)

    2005-02-15

    Anelastic behavior of crystalline solids is generated by several microstructural processes. Its experimental study yields valuable information about materials, namely: modulus, dissipation mechanisms and activation enthalpies. However, conventional techniques to evaluate it are complicated, expensive, time consuming and not easily replicated. As a new approach, in this work a Moessbauer spectrum of an iron specimen is obtained with the specimen at repose being its parameters the 'base parameters'. After that, the same specimen is subjected to an alternated stress-relaxation cycle at frequency {omega}{sub 1} and a new Moessbauer spectrum is obtained under this excited condition; doing the same at several increasing frequencies {omega}{sub n} in order to scan a wide frequencies spectrum. The differences between the Moessbauer parameters obtained at each excitation frequency and the base parameters are plotted against frequency, yielding an 'anelastic spectrum' that reveals the different dissipation mechanisms involved, its characteristic frequency and activation energy. Results are in good agreement with the obtained with other techniques

  15. Lattice dynamic studies from {sup 151}Eu-Moessbauer spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Katada, Motomi [Tokyo Metropolitan Univ., Hachioji (Japan). Faculty of Science

    1997-03-01

    New complexes {l_brace}(Eu(napy){sub 2}(H{sub 2}O){sub 3})(Fe(CN){sub 6})4H{sub 2}O{r_brace}{sub x}, bpy({l_brace}(Eu(bpy)(H{sub 2}O){sub 4})(Fe(CN){sub 6})1.5bpy4H{sub 2}O{r_brace}{sub x}) and ({l_brace}(Eu(phen){sub 2}(H{sub 2}O){sub 2})(Fe(CN){sub 6})2phen{r_brace}{sub x}) etc were synthesized using phenanthroline and bipyridine. Lattice dynamic behaviors of Eu and Fe atom in the complexes were investigated by Moessbauer spectroscopy. By {sup 151}Eu-Moessbauer spectrum and parameters of new complexes, bpy complex showed the largest quadrupole splitting value, indicating bad symmetry of Eu ligand in the environment. Molecular structure of napy, bpy and phen complex were shown. These complexes are consisted of Eu atom coordinated with ligand and water molecule, of which (Fe(CN){sub 6}){sup 3-} ion formed one dimentional polymer chain and naphthyridines formed stacking structure. New complexes were observed by {sup 57}Fe-Moessbauer spectroscopy, too. The quadrupole splitting values were very different each other, indicating change of symmetry of Fe atom in the environment and three valence low spin state of Fe in the complex. (S.Y.)

  16. Moessbauer spectroscopy of the SNC meteorite Zagami

    Science.gov (United States)

    Agerkvist, D. P.; Vistisen, L.

    1993-01-01

    We have performed Mossbauer spectroscopy on two different pieces of the meteorite Zagami belonging to the group of SNC meteorites. In one of the samples we found a substantial amount of olivine inter grown with one kind of pyroxene, and also another kind of pyroxene very similar to the pyroxene in the other sample we examined. Both samples showed less than 1 percent of Fe(3+) in the silicate phase. The group of SNC meteorites called shergottites, to which Zagami belongs, are achondrites whose texture, mineralogy and composition resembles those of terrestrial diabases. The results from the investigation are presented.

  17. Study of iron valence state and position in sub-site by Moessbauer spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Uhm, Young Rang; Lim, Jae Cheong; KIm, Chul Sung [Korea Atomic Energy Research Institute, Daejeon (Korea, Republic of); Son, Kwang Jae [Kookmin Univ., Seoul (Korea, Republic of)

    2014-05-15

    The magnetic ordering temperature and the magnitude of the magnetic fields at the iron sites of YIG can be influenced by substituting, either partially or totally, the Fe{sup 3+} ions at the octahedral and/or the tetrahedral sites with magnetic or diamagnetic ions, and/or by substitution the Y{sup 3+} ions at the dodecahedral sites with magnetic rare earth ions. It has been known for some time that Moessbauer spectroscopy is a powerful method by which iron-containing garnets can be studied. We report here on the synthesis of the compounds with garnet-related structures of composition Y{sub 3}Fe{sub 4.5}Cr{sub 0.5}O{sub 12} and its examination by {sup 57}Fe Moessbauer spectroscopy. The chromium in compounds of the Y{sub 3}Fe{sub 4.5}Cr{sub 0.5}O{sub 12} is distributed at an octahedral site. The Moessbauer spectra can be analyzed using 3 or 4 sets of six Lorentzians with increasing amount of Cr{sup 3+} compounds in this system. It results from the distribution ({sub 4}C{sub n}) of Fe{sup 3+} and Cr{sup 3+} at an octahedral site. A comparative study of ferrous tablets of Dynabi was carried out using Moessbauer spectroscopy. The obtained results revealed the presence of ferrous (Fe{sup 2+}) gluconate and ferrous fumarate in a sample. This observation is important to better control the iron state in such medicaments because their pharmaceutical effect in the body is related to the form and valence of iron. The Cr-containing yttrium iron garnet (YIG), and the exchange interactions and site distributions were studied using {sup 57}Fe Moessbauer spectroscopy. The obtained results revealed the presence of ferrous (Fe{sup 2+}) gluconate and ferrous fumarate in the sample. This observation is important better control the iron state in such medicaments because their pharmaceutical effect in the body is related to the form and valence of iron.

  18. Comparative Study of Human Liver Ferritin and Chicken Liver by Moessbauer Spectroscopy. Preliminary Results

    Energy Technology Data Exchange (ETDEWEB)

    Oshtrakh, M. I. [Ural State Technical University - UPI, Division of Applied Biophysics, Faculty of Physical Techniques and Devices for Quality Control (Russian Federation); Milder, O. B.; Semionkin, V. A. [Ural State Technical University - UPI, Faculty of Experimental Physics (Russian Federation); Prokopenko, P. G. [Russian State Medical University, Faculty of Biochemistry (Russian Federation); Malakheeva, L. I. [Simbio Holding, Science Consultation Department (Russian Federation)

    2004-12-15

    A comparative study of normal human liver ferritin and livers from normal chicken and chicken with Marek disease was made by Moessbauer spectroscopy. Small differences of quadrupole splitting and isomer shift were found for human liver ferritin and chicken liver. Moessbauer parameters for liver from normal chicken and chicken with Marek disease were the same.

  19. Moessbauer and EXAFS spectroscopy investigation of iron and arsenic adsorption to lettuce leaves

    Energy Technology Data Exchange (ETDEWEB)

    Vasconcelos, Igor F., E-mail: ifvasco@ufc.br [Universidade Federal do Ceara, Dep. Eng. Metalurgica e de Materiais (Brazil); Silva, Gabriela C.; Carvalho, Regina P.; Dantas, Maria Sylvia S.; Ciminelli, Virginia S. T. [Universidade Federal de Minas Gerais, Dep. Eng. Metalurgica e de Materiais (Brazil)

    2010-01-15

    The accumulation of iron and arsenic from aqueous solution by lettuce leaves biomass was investigated using Moessbauer and EXAFS spectroscopic techniques. Moessbauer spectroscopy results show that iron is oxidized during sorption while EXAFS results indicate that iron is coordinated by approximately 6 oxygen and 2 carbon atoms while arsenic is coordinated by approximately 4 oxygen atoms with iron as a second neighbor.

  20. In-situ Moessbauer spectroscopy with MIMOS II

    Energy Technology Data Exchange (ETDEWEB)

    Fleischer, Iris, E-mail: fleischi@uni-mainz.de; Klingelhoefer, Goestar [Institute of Inorganic and Analytical Chemistry, Johannes Gutenberg University of Mainz (Germany); Morris, Richard V. [NASA Johnson Space Center (United States); Schroeder, Christian [University of Bayreuth and University of Tuebingen (Germany); Rodionov, Daniel [Institute of Inorganic and Analytical Chemistry, Johannes Gutenberg University of Mainz (Germany); Souza, Paulo A. de [Tasmanian ICT Centre (Australia); Collaboration: MIMOS II Team

    2012-03-15

    The miniaturized Moessbauer spectrometer MIMOS II was developed for the exploration of planetary surfaces. Two MIMOS II instruments were successfully deployed on the martian surface as payload elements of the NASA Mars Exploration Rover (MER) mission and have returned data since landing in January 2004. Moessbauer spectroscopy has made significant contributions to the success of the MER mission, in particular identification of iron-bearing minerals formed through aqueous weathering processes. As a field-portable instrument and with backscattering geometry, MIMOS II provides an opportunity for non-destructive in-situ investigations for a range of applications. For example, the instrument has been used for analyses of archaeological artifacts, for air pollution studies and for in-field monitoring of green rust formation. A MER-type MIMOS II instrument is part of the payload of the Russian Phobos-Grunt mission, scheduled for launch in November 2011, with the aim of exploring the composition of the martian moon Phobos. An advanced version of the instrument, MIMOS IIA, that incorporates capability for elemental analyses, is currently under development.

  1. Pottery from a Chimu Workshop Studied by Moessbauer Spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Tschauner, H. [Harvard University, Department of Anthropology (United States); Wagner, U. [Technische Universitaet Muenchen, Physik-Department E15 (Germany)

    2003-09-15

    Ceramic finds from a pottery workshop in the Lambayeque valley were studied by neutron activation analysis, Moessbauer spectroscopy and X-ray diffraction in an attempt to assess an advanced division of labour on the North Coast of Peru during the Chimu period (AD 1350-1460). The study suggests that the material was predominantly fired in a reducing environment with partial reoxidation at the end of the firing cycles, although firing in an oxidising atmosphere has taken place occasionally. The observed variation of firing conditions is characteristic for the use of pit kilns. The results of the archaeometric studies confirm the stylistic studies and show that pottery was no status symbol and far less important as a carrier of Chimu style than metal artefacts.

  2. Application of Moessbauer spectroscopy on corrosion products of NPP

    Energy Technology Data Exchange (ETDEWEB)

    Dekan, J., E-mail: julius.dekan@stuba.sk; Lipka, J.; Slugen, V. [Institute of Nuclear and Physical Engineering, Faculty of Electrical Engineering and Information Technology, SUT (Slovakia)

    2013-04-15

    Steam generator (SG) is generally one of the most important components at all nuclear power plants (NPP) with close impact to safe and long-term operation. Material degradation and corrosion/erosion processes are serious risks for long-term reliable operation. Steam generators of four VVER-440 units at nuclear power plants V-1 and V-2 in Jaslovske Bohunice (Slovakia) were gradually changed by new original 'Bohunice' design in period 1994-1998, in order to improve corrosion resistance of SGs. Corrosion processes before and after these design and material changes in Bohunice secondary circuit were studied using Moessbauer spectroscopy during last 25 years. Innovations in the feed water pipeline design as well as material composition improvements were evaluated positively. Moessbauer spectroscopy studies of phase composition of corrosion products were performed on real specimens scrapped from water pipelines or in form of filters deposits. Newest results in our long-term corrosion study confirm good operational experiences and suitable chemical regimes (reduction environment) which results mostly in creation of magnetite (on the level 70 % or higher) and small portions of hematite, goethite or hydrooxides. Regular observation of corrosion/erosion processes is essential for keeping NPP operation on high safety level. The output from performed material analyses influences the optimisation of operating chemical regimes and it can be used in optimisation of regimes at decontamination and passivation of pipelines or secondary circuit components. It can be concluded that a longer passivation time leads more to magnetite fraction in the corrosion products composition.

  3. Fifty years of Moessbauer spectroscopy: from alloys and oxides to glasses and nanoparticles

    Energy Technology Data Exchange (ETDEWEB)

    Johnson, C. E., E-mail: cjohnson@utsi.edu [University of Tennessee Space Institute, Center for Laser Applications (United States); Johnson, J. A. [University of Tennessee Space Institute, Department of Mechanical, Aerospace and Biomedical Engineering (United States)

    2012-03-15

    The Moessbauer Effect was discovered in 1957. In 1960 Moessbauer spectroscopy was born when two important papers appeared on (i) the magnetic hyperfine interaction and (ii) the electric monopole (isomer shift) and quadrupole interactions. These transformed an interesting phenomenon into a method for probing solids. Applications to magnetism, metals and alloys, chemical compounds, biological molecules, geology, archaeology and other sciences followed and are still of current interest. Two areas of research where Moessbauer spectroscopy is making unique contributions are in determining oxidation states in (i) glasses and (ii) nanoparticles. Some recent measurements are described.

  4. A study of human liver ferritin and chicken liver and spleen using Moessbauer spectroscopy with high velocity resolution

    Energy Technology Data Exchange (ETDEWEB)

    Oshtrakh, M. I., E-mail: oshtrakh@mail.utnet.ru [Ural State Technical University-UPI, Faculty of Physical Techniques and Devices for Quality Control (Russian Federation); Milder, O. B.; Semionkin, V. A. [Ural State Technical University-UPI, Faculty of Experimental Physics (Russian Federation)

    2008-01-15

    Lyophilized samples of human liver ferritin and chicken liver and spleen were measured at room temperature using Moessbauer spectroscopy with high velocity resolution. An increase in the velocity resolution of Moessbauer spectroscopy permitted us to increase accuracy and decrease experimental error in determining the hyperfine parameters of human liver ferritin and chicken liver and spleen. Moessbauer spectroscopy with high velocity resolution may be very useful for revealing small differences in hyperfine parameters during biomedical research.

  5. Moessbauer and infrared spectroscopy as a diagnostic tool for the characterization of ferric tannates

    Energy Technology Data Exchange (ETDEWEB)

    Jaen, Juan A., E-mail: jjaen@ancon.up.ac.p [Universidad de Panama, Depto. de Quimica Fisica, CITEN, Lab. No. 105, Edificio de Laboratorios Cientificos-VIP (Panama); Navarro, Cesar [Universidad de Panama, Escuela de Quimica, Facultad de Ciencias Naturales, Exactas y Tecnologia (Panama)

    2009-07-15

    Fourier transform infrared spectroscopy and Moessbauer spectroscopy are use for the characterization and qualitative analysis of hydrolysable and condensed tannates. The two classes of tannates may be differentiated from the characteristic IR pattern. Moessbauer proof that a mixture of mono- and bis-type ferric tannate complexes, and an iron(II)-tannin complex are obtained from the interaction of hydrolysable tannins (tannic acid and chestnut tannin) and condensed tannins (mimosa and quebracho) with a ferric nitrate solution. At pH 7, a partially hydrolyzed ferric tannate complex was also obtained.

  6. Using Moessbauer spectroscopy as key technique in the investigation of nanosized magnetic particles for drug delivery

    Energy Technology Data Exchange (ETDEWEB)

    Morais, P. C., E-mail: pcmor@unb.br [Universidade de Brasilia, Nucleo de Fisica Aplicada, Instituto de Fisica (Brazil)

    2008-01-15

    This paper describes how cobalt ferrite nanoparticles, suspended as ionic or biocompatible magnetic fluids, can be used as a platform to built complex nanosized magnetic materials, more specifically magnetic drug delivery systems. In particular, the paper is addressed to the discussion of the use of the Moessbauer spectroscopy as an extremely useful technique in supporting the investigation of key aspects related to the properties of the hosted magnetic nanosized particle. Example of the use of the Moessbauer spectroscopy in accessing information regarding the nanoparticle modification due to the empirical process which provides long term chemical stability is included in the paper.

  7. Performance of new solid state {gamma}-detectors in {sup 57}Fe Moessbauer spectroscopy experiments

    Energy Technology Data Exchange (ETDEWEB)

    Dellmann, Til; Klauss, Hans-Henning [Institute of Solid State Physics, TU Dresden (Germany)

    2011-07-01

    Usually, proportional counter tubes are used in {sup 57}Fe Moessbauer spectroscopy for the detection of the 14.4 keV transition line. % and further signal processing. The recent developement of Si-based solid state detectors led to commercially available drift detectors (SDD) and high purity PiN diodes without the necessity of cooling with liquid nitrogen. First applications of SDD detectors in the analysis of minerals are already highly promising. In this talk, we present a detailed comparison between the three detector types and their use in Moessbauer spectroscopy using a standard absorber-source-combination (metallic iron with a 2.0 GBq {sup 57}Co/Rh source) in absorbtion geometry. Starting with the definition of a global efficiency function, which optimises the goodness of a Moessbauer spectrum and thus the required measurement time, we examined the influence of the intrinsic detector parameters on the global efficiency.

  8. Characterization of the firing conditions of archaeological Marajoara pottery by Moessbauer spectroscopy and X-ray diffraction

    Energy Technology Data Exchange (ETDEWEB)

    Munayco, P., E-mail: mpablo@cbpf.br; Scorzelli, R. B. [Centro Brasileiro de Pesquisas Fisicas (Brazil)

    2013-08-15

    Here we report on a study of samples from fragments of Marajoara ceramics using {sup 57}Fe Moessbauer spectroscopy and XRD. The Moessbauer spectra were measured at room temperature (RT) and at liquid helium temperature (4.2 K). Despite a certain variability of the Moessbauer spectra, dominant features could be established, which allowed the samples to be classified into characteristic types (Moess-types) according to their Moessbauer patterns. The different Moess-types were defined on account of the presence and intensity or the absence of certain components, mainly in the RT spectra. The analysis is complemented by data obtained by X-ray diffraction.

  9. The big and little of fifty years of Moessbauer spectroscopy at Argonne.

    Energy Technology Data Exchange (ETDEWEB)

    Westfall, C.

    2005-09-20

    Using radioactive materials obtained by chance, a turntable employing gears from Heidelberg's mechanical toy shops, and other minimal equipment available in post World War II Germany, in 1959 Rudolf Moessbauer confirmed his suspicion that his graduate research had yielded ground-breaking results. He published his conclusion: an atomic nucleus in a crystal undergoes negligible recoil when it emits a low energy gamma ray and provides the entire energy to the gamma ray. In the beginning Moessbauer's news might have been dismissed. As Argonne nuclear physicist Gilbert Perlow noted: ''Everybody knew that nuclei were supposed to recoil when emitting gamma rays--people made those measurements every day''. If any such effect existed, why had no one noticed it before? The notion that some nuclei would not recoil was ''completely crazy'', in the words of the eminent University of Illinois condensed matter physicist Frederich Seitz. Intrigued, however, nuclear physicists as well as condensed matter (or solid state) physicists in various locations--but particularly at the Atomic Energy Research Establishment at Harwell in Britain and at Argonne and Los Alamos in the U.S.--found themselves pondering the Moessbauer spectra with its nuclear and solid state properties starting in late 1959. After an exciting year during which Moessbauer's ideas were confirmed and extended, the physics community concluded that Moessbauer was right. Moessbauer won the Nobel Prize for his work in 1961. In the 1960s and 1970s Argonne physicists produced an increasingly clear picture of the properties of matter using the spectroscopy ushered in by Moessbauer. The scale of this traditional Moessbauer spectroscopy, which required a radioactive source and other simple equipment, began quite modestly by Argonne standards. For example Argonne hosted traditional Moessbauer spectroscopy research using mostly existing equipment in the early days and

  10. Application of {sup 57}Co emission Moessbauer spectroscopy to studying biocomplexes in frozen solutions

    Energy Technology Data Exchange (ETDEWEB)

    Kamnev, A. A., E-mail: aakamnev@ibppm.sgu.ru [Laboratory of Biochemistry of Plant-Bacterial Symbioses, Institute of Biochemistry and Physiology of Plants and Microorganisms, Russian Academy of Sciences (Russian Federation); Kulikov, L. A.; Perfiliev, Yu. D. [M.V. Lomonosov Moscow State University, Laboratory of Nuclear Chemistry Techniques, Department of Radiochemistry, Faculty of Chemistry (Russian Federation); Antonyuk, L. P. [Laboratory of Biochemistry of Plant-Bacterial Symbioses, Institute of Biochemistry and Physiology of Plants and Microorganisms, Russian Academy of Sciences (Russian Federation); Kuzmann, E.; Vertes, A. [Eoetvoes Lorand University, Research Group for Nuclear Techniques in Structural Chemistry, Hungarian Academy of Sciences, Department of Nuclear Chemistry (Hungary)

    2005-09-15

    Emission Moessbauer spectroscopy with the {sup 57}Co isotope was used to study very dilute rapidly frozen aqueous solutions of cobalt(II) complexes with low-molecular-weight biomolecules (aromatic amino acids - anthranilic acid and L-tryptophan) and within a sophisticated biopolymer, bacterial glutamine synthetase, a key enzyme of nitrogen metabolism. The appearance of after-effects of the {sup 57}Co{sup {yields}57}Fe nuclear transformation as well as the coordination properties of the cation and the ligands in the complexes are discussed on the basis of their Moessbauer parameters.

  11. Nanophase mixed-valence iron minerals in meteorites identified by cryogenic Moessbauer spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Burns, R.G. [Massachusetts Inst. of Tech., Cambridge, MA (United States). Dept. of Earth, Atmospheric and Planetary Sciences; Fisher, D.S. [Massachusetts Inst. of Tech., Cambridge, MA (United States). Dept. of Earth, Atmospheric and Planetary Sciences

    1994-11-01

    Determination of oxidation states and the crystal chemistry of iron-bearing minerals in carbonaceous chondrites by Moessbauer spectroscopy is complicated by thermally-induced electron-hopping in cronstedtite, superparamagnetism of hydrous ferric oxides and ill-defined contributions from an incommensurate layered iron sulfide phase believed to be tochilinite. Moessbauer spectra measurements at 30 K of several terrestrial cronstedtite and tochilinite specimens have enables modal proportions of these minerals, as well as Fe{sup 3+}/Fe{sup 2+} ratios, to be determined quantitatively in a suite of CM-type meteorites. (orig.)

  12. Use of Moessbauer spectroscopy to study reaction products of polyphenols and iron compounds

    Energy Technology Data Exchange (ETDEWEB)

    Gust, J. (Building Research Inst., Warsaw (Poland)); Suwalski, J. (Atomic Energy Inst., Otwock-Swierk (Poland))

    1994-05-01

    Moessbauer spectroscopy was used to study parameters of the reaction products of iron compounds (Fe[sup III]) and polyphenols with hydroxyl (OH) groups in ortho positions. Polyphenols used in the reaction were catechol, pyrogallol, gallic acid, and oak tannin. The Fe-containing compounds were hydrated ferric sulfate (Fe[sub 2][SO[sub 4

  13. Selected applications of {sup 57}Fe Moessbauer spectroscopy to mineral studies

    Energy Technology Data Exchange (ETDEWEB)

    Grave, E. de; Eeckhout, S.G. [University of Gent, Department of Subatomic and Radiation Physics (Belgium); McCammon, C.A. [University of Bayreuth, Bayerisches Geoinstitut (Germany)

    1999-11-15

    The microscopic models which are commonly used to interpret the temperature variations of the centre shifts and quadrupole splittings observed from the Moessbauer spectra of iron-containing minerals are briefly presented and illustrated using the results of recent studies of ortho- and clinopyroxenes. The importance of applied-field Moessbauer spectroscopy for the determination of the electric field gradient is indicated. Aspects of the magnetic spectra of Fe{sup 2+}-bearing minerals emphasise the benefit of using external fields to elucidate the nature of the magnetic ordering. Two Fe{sup 3+} minerals, bernalite and franklinite, serve as examples to illustrate this point. Finally, two applications of the Moessbauer milliprobe technique are presented: the characterisation of inclusions in diamond, and the determination of the oxidation state of a new iron uranyl sulfate mineral, deliensite.

  14. Moessbauer spectroscopy evidence of intrinsic non-stoichiometry in iron telluride single crystals

    Energy Technology Data Exchange (ETDEWEB)

    Kiiamov, Airat G.; Tayurskii, Dmitrii A. [Institute of Physics, Kazan Federal University (Russian Federation); Centre for Quantum Technologies, Kazan Federal University (Russian Federation); Lysogorskiy, Yury V.; Vagizov, Farit G. [Institute of Physics, Kazan Federal University (Russian Federation); Tagirov, Lenar R. [Institute of Physics, Kazan Federal University (Russian Federation); E.K. Zavoisky Physical-Technical Institute, Russian Academy of Sciences, Kazan (Russian Federation); Croitori, Dorina [Institute of Applied Physics, Academy of Sciences of Moldova, Chisinau (Moldova, Republic of); Tsurkan, Vladimir [Institute of Applied Physics, Academy of Sciences of Moldova, Chisinau (Moldova, Republic of); Experimental Physics V, University of Augsburg (Germany); Loidl, Alois [Experimental Physics V, University of Augsburg (Germany)

    2017-04-15

    The FeTe parent compound for iron-superconductor chalcogenides was studied applying Moessbauer spectroscopy accompanied by ab initio calculations of electric field gradients at the iron nuclei. Room-temperature (RT) Moessbauer spectra of single crystals have shown asymmetric doublet structure commonly ascribed to contributions of over-stoichiometric iron or impurity phases. Low-temperature Moessbauer spectra of the magnetically ordered compound could be well described by four hyperfine-split sextets, although no other foreign phases different from Fe{sub 1.05}Te were detected by XRD and microanalysis within the sensitivity limits of the equipment. Density functional ab initio calculations have shown that over-stoichiometric iron atoms significantly affect electron charge and spin density up to the second coordination sphere of the iron sub-lattice, and, as a result, four non-equivalent groups of iron atoms are formed by their local environment. The resulting four-group model consistently describes the angular dependence of the single crystals Moessbauer spectra as well as intensity asymmetry of the doublet absorption lines in powdered samples at RT. We suppose that our approach could be extended to the entire class of Fe{sub 1+y}Se{sub 1-x}Te{sub x} compounds, which contain excess iron atoms. (copyright 2016 by WILEY-VCH Verlag GmbH and Co. KGaA, Weinheim)

  15. Firing of Clays Studied by X-ray Diffraction and Moessbauer Spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Haeusler, W. [Technische Universitaet Muenchen, Physik-Department E15 (Germany)

    2004-06-15

    Three bentonites of varying purity were fired in air under controlled conditions up to 1300{sup o}C in an attempt to provide data for the assessment of firing techniques used in prehistoric pottery making. X-ray diffraction of samples heated at increasing temperatures allows to study the mineral transformations, the breakdown of the clay structure and the formation of new minerals in the high-temperature region. Moessbauer spectroscopy reveals the change of valence state and of the environment of the iron atoms on heating. Non iron-bearing minerals are only accessible by X-ray diffraction, while iron-containing oxidic and amorphous phases may be difficult to detect, due to poor crystallinity and small particle size. The combination of X-ray diffraction and Moessbauer spectroscopy therefore has a considerable potential in the study of the chemical and physical transformations occurring in pottery clays during firing.

  16. Iron-nickel alloy from iron meteorite Chinga studied by Moessbauer spectroscopy with high velocity resolution

    Energy Technology Data Exchange (ETDEWEB)

    Oshtrakh, M. I., E-mail: oshtrakh@mail.utnet.ru; Grokhovsky, V. I.; Abramova, N. V. [Ural State Technical University-UPI, Faculty of Physical Techniques and Devices for Quality Control (Russian Federation); Semionkin, V. A. [Ural State Technical University-UPI, Faculty of Experimental Physics (Russian Federation); Milder, O. B. [Ural State Technical University-UPI, Radio-Technical Department (Russian Federation)

    2009-04-15

    Study of iron-nickel alloy from iron meteorite Chinga using Moessbauer spectroscopy with improved velocity resolution (measurement and presentation in 4,096 channels) revealed six magnetic components which may be related to various {alpha}-Fe(Ni, Co) and {gamma}-Fe(Ni, Co) phases while previous study with low velocity resolution (in 512 channels) revealed only three magnetic components. This new result was in agreement with the scanning electron microscopy study.

  17. Mineral identification in Colombian coals using Moessbauer spectroscopy and X-ray diffraction

    Energy Technology Data Exchange (ETDEWEB)

    Fajardo, M. [Universidad del Valle, A.A, Departamento de Fisica (Colombia); Mojica, J. [Instituto Nacional de Investigaciones en Geociencia, Mineria y Quimica (INGEOMINAS) (Colombia); Barraza, J. [Universidad del Valle, A.A, Departamento de Procesos Quimicos, Facultad de Ingenieria (Colombia); Perez Alcazar, G.A.; Tabares, J.A. [Universidad del Valle, A.A, Departamento de Fisica (Colombia)

    1999-11-15

    Minerals were identified in three Colombian coal samples from the Southwest of the country using Moessbauer spectroscopy and X-ray diffraction. Original and sink separated coal fractions of specific gravity 1.40 and 1.60 with particle size less than 600 {mu}m were used in the study. Using Moessbauer spectroscopy, the minerals identified in the original coal samples were pyrite jarosite, ankerite, illite and ferrous sulfate, whereas by means of X-ray diffraction, minerals identified were kaolinite, quartz, pyrite, and jarosite. Differences in mineral composition were found in the original and sink separated fractions using both techniques. Moessbauer spectra show that the mineral phases in low concentrations such as illite, ankerite and ferrous sulfate do not always appear in the spectra of sink coals, despite of those minerals occurring in the original coal, due to the fact that they are associated with the organic matter and not liberated in the grinding process. X-ray results show that the peak intensity grows as the specific gravity is increased indicating that the density separation method could be an effective process to clean coal.

  18. In situ{sup 119}Sn Moessbauer spectroscopy study of Sn-based electrode materials

    Energy Technology Data Exchange (ETDEWEB)

    Aboulaich, Abdelmaula, E-mail: abdelmaula.aboulaich@univ-mont2.fr; Robert, Florent; Lippens, Pierre Emmanuel; Aldon, Laurent; Olivier-Fourcade, Josette [Universite Montpellier II, Laboratoire des Agregats Moleculaires et Materiaux Inorganiques (UMR 5072-CNRS) (France); Willmann, Patrick [Centre National d' Etudes Spatiales (France); Jumas, Jean-Claude [Universite Montpellier II, Laboratoire des Agregats Moleculaires et Materiaux Inorganiques (UMR 5072-CNRS) (France)

    2006-01-15

    Sn-based composite materials were synthetized by a conventional melt-quenching method, and studied by X-ray diffraction, electrochemistry and in situ{sup 119}Sn Moesssbauer spectroscopy. Tin was dispersed ex situ into a matrix formed from B{sub 2}O{sub 3}:P{sub 2}O{sub 5}. XRD and {sup 119}Sn Moessbauer spectroscopy show the formation of an interface between the active species (Sn{sup 0}) and the matrix. This amorphous interface acts as a 'buffer-zone' which compensates volume changes during the tin-lithium alloy formation and avoids aggregation of tin particles.

  19. Reclassification of CK chondrites confirmed by elemental analysis and Fe-Moessbauer spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Kubuki, Shiro, E-mail: kubuki@tmu.ac.jp; Iwanuma, Jun; Akiyama, Kazuhiko; Isa, Miki; Shirai, Naoki; Ebihara, Mitsuru [Tokyo Metropolitan University, Department of Chemistry, Graduate School of Science and Engineering (Japan); Nishida, Tetsuaki [Kinki University, Department of Biological and Environmental Chemistry, Faculty of Humanity-Oriented Science and Engineering (Japan)

    2012-03-15

    Twenty CK chondrites collected in the Antarctica Continent were characterized by inductively-coupled plasma mass spectrometry (ICP-MS), prompt gamma ray analysis (PGA), instrumental neutron activation analysis (INAA), X-ray diffractometry (XRD) and {sup 57}Fe-Moessbauer spectroscopy. As a result of elemental analysis, it was revealed that 18.2{approx}26.4 mass% of iron was included in the each chondrite. Moessbauer spectrum of LEW86258, classified as a typical CK chondrite, was found to be composed of two paramagnetic doublets and two magnetic sextets. Moessbauer spectra were assigned to the absorption due to forsterite (Mg{sub 1.36}Fe{sub 0.64}SiO{sub 4}) and magnetite (Fe{sub 3}O{sub 4}), as also confirmed by XRD. XRD study of LAP03834, reclassified from CK to R chondrite, revealed the presence of crystalline phase due to forsterite. These results indicate that LAP03834 and related chondrites, i.e., MET01149, LAP03923 and MAC02453, should be reclassified as R or LL chondrite.

  20. Extraterrestrial Moessbauer spectroscopy: more than 3 years of Mars exploration and developments for future missions

    Energy Technology Data Exchange (ETDEWEB)

    Schroeder, Christian, E-mail: christian.schroeder-1@nasa.gov [NASA Johnson Space Center, Astromaterials Research and Exploration Science, Mail Code KR (United States); Klingelhoefer, Goestar, E-mail: klingel@mail.uni-mainz.de [Johannes Gutenberg-Universitaet, Institut fuer Anorganische und Analytische Chemie (Germany); Morris, Richard V., E-mail: richard.v.morris@nasa.gov [NASA Johnson Space Center, Astromaterials Research and Exploration Science, Mail Code KR (United States); Rodionov, Daniel S., E-mail: rodionov@iki.rssi.ru; Fleischer, Iris, E-mail: fleischi@uni-mainz.de; Blumers, Mathias, E-mail: mblumers@uni-mainz.de [Johannes Gutenberg-Universitaet, Institut fuer Anorganische und Analytische Chemie (Germany)

    2008-02-15

    After almost 4 years of operating on the surface of Mars, Moessbauer spectroscopy has become a mature technique for robotic planetary exploration. The combination of quantitative information about the distribution of Fe among its oxidation and coordination states, identification of Fe-bearing phases, and relative distribution of Fe among those phases provides valuable contributions to the search for past water activity, the assessment of past environmental conditions, and the suitability for life of the two NASA Mars Exploration Rover landing sites. Experience from the Mars Exploration Rover Mission highlights needs for improvement of the instruments for future missions such as the Russian Phobos-Grunt and the European ExoMars rover.

  1. Gold-surface binding of molecular switches studied by Moessbauer spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Homenya, Patrick, E-mail: patrick.homenya@acd.uni-hannover.de [Leibniz Universitaet Hannover, Institut fuer Anorganische Chemie (Germany); Messerschmidt, Markus; Tahir, Muhammad Nawaz [Johannes Gutenberg-Universitaet Mainz, Institut fuer Anorganische Chemie und Analytische Chemie (Germany); Martinez, Victor [University of Valencia, Institut de Ciencia Molecular (Spain); Cheng, Yajun [Johannes Gutenberg-Universitaet Mainz, Institut fuer Anorganische Chemie und Analytische Chemie (Germany); Gutmann, Jochen S. [Max Planck-Institut fuer Polymerforschung (Germany); Klein, Michael; Jung, Stefan; Wolff, Morris; Saadat, Reza; Nariaki, Driss [Leibniz Universitaet Hannover, Institut fuer Anorganische Chemie (Germany); Boca, Roman [Slovak Technical University (FCHPT), Institute of Inorganic Chemistry (Slovakia); Klingelhoefer, Goestar; Tremel, Wolfgang [Johannes Gutenberg-Universitaet Mainz, Institut fuer Anorganische Chemie und Analytische Chemie (Germany); Renz, Franz, E-mail: franz.renz@acd.uni-hannover.de [Leibniz Universitaet Hannover, Institut fuer Anorganische Chemie (Germany)

    2012-03-15

    The nonanuclear coordination compound [Mo{sup IV}{l_brace}(CN)Fe{sup III}(3-methyl-saldptn){r_brace}{sub 8}]Cl{sub 4} exhibits multiple spin transitions (3-methyl-saldptn = N,N Prime -bis(3 Prime Prime -methyl-2 Prime Prime -hydroxy-benzyliden)-1,7-diamino-4-azaheptane). This spin crossover cluster is bound via a self-assembled monolayer onto a two dimensional array gold surface. Moessbauer spectroscopy indicates that the thermally and optically induced spin crossover of the compound is maintained. Thereby, the foundation for its potential practical application (e.g. in the field of information storage) was laid.

  2. Iron-57 Moessbauer spectroscopy studies of meteorites recovered from Roosevelt County, USA

    Energy Technology Data Exchange (ETDEWEB)

    Berry, F.J. (Dept. of Chemistry, Open Univ., Milton Keynes (United Kingdom)); Bland, P.A. (Dept. of Earth Sciences, Open Univ., Milton Keynes (United Kingdom)); Oates, G. (Dept. of Chemistry, Open Univ., Milton Keynes (United Kingdom)); Pillinger, C.T. (Dept. of Earth Sciences, Open Univ., Milton Keynes (United Kingdom))

    1994-02-01

    Some H5 ordinary chondrite meteorites recovered from the desert region of Roosevelt County in New Mexico, USA and [sup 14]C dated to determine the terrestrial age have been examined by [sup 57]Fe Moessbauer spectroscopy. The preliminary results suggest the increasing oxidation of Fe[sup 0] in the iron-nickel alloy phase and of Fe[sup 2+] in the iron-sulphide and -silicate phases as a result of terrestrial weathering over ca. 38 000 years and which induces the formation of macroscopic iron oxide/oxyhydroxide phases. (orig.)

  3. Coupling Nuclear Induced Phonon Propagation with Conversion Electron Moessbauer Spectroscopy

    Science.gov (United States)

    2015-06-18

    by analogy, the nucleus) recoils with a recoil energy ER when firing a bullet (the γ-ray). A more in-depth discussion of the recoil energy loss can...Number of Mössbauer Peaks 1 The next consideration was the geometry of the absorber. The absorber not only had to fit in the CEMS detector opening ...Methodology, vol. 7. Plenum Press, New York. (1971) 24. Spikerman, J.J. Mossbauer Spectroscopy Instruction Manual for the MS-1200. Ranger Scientific

  4. Very high pressure Moessbauer spectroscopy using diamond anvil cells

    Energy Technology Data Exchange (ETDEWEB)

    Pasternak, M.P.; Taylor, R.D.

    1988-01-01

    The technique of generating very high pressure by means of Diamond Anvil Cells (DAC) for Mossbauer Effect applications is outlined. A comprehensive description is presented of the principles of DAC, modification for the use in M/umlt o/ssbauer Spectroscopy (MS), the Merrill--Bassett and Bassett cells, of pressure measurements, of gasketing and collimation, and of hydrostatic media. Examples of /sup 151/Eu, /sup 119/Sn and /sup 129/I are given showing the feasibility of DAC applications in MS. Other isotopes with potential use for high pressure MS using DAC are suggested. 27 refs., 9 figs.

  5. Characterization of the Roraima savanna across of X-ray diffraction, thermomagnetic analysis and Moessbauer spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Silva, Gilmar A.; Araujo, R.C.; Sergio, C.S. [Universidade Federal de Roraima (UFRR), Boa Vista, RR (Brazil)

    2012-07-01

    Full text: The technique of X-ray diffraction has great resolving power to determine the phases present in crystalline material, thereby enabling it to determine the elements present in the materials as well as changes in structure that they can suffer when subjected to various physical processes and/or chemical means. The research had as objective to characterize the mineralogy of iron oxides, silicon, aluminum and other minerals in the soil of five points of the Roraima savannah. The points where samples were collected are five municipalities in the state of Roraima. The area of sampling is part of the savanna in Roraima. The samples were collected. We analyzed samples from five points from the collection of natural soil in the locations listed. The samples were placed in a mill to a uniform grain size. After the milling process, the magnetic material was separated using a permanent magnet. Then the samples were analyzed by x-ray diffraction, thermomagnetic analysis and Moessbauer spectroscopy. Preliminary results of XRD showed the occurrence of phases of oxides of iron, silicon, aluminum and other phases less. Thermomagnetic analysis show that the magnetic phases are magnetite and hematite. The results of the Moessbauer spectroscopy indicates the reliability in the two prior art and confirmed the presence of the phases of oxides of iron present in the soil analyzed. (author)

  6. Moessbauer Spectroscopy of Mineral Separates from SNC Meteorites

    Science.gov (United States)

    Dyar, M. D.

    2003-01-01

    Numerous workers have recently focused attention on the issue of the oxygen fugacity (f(sub O2)) of martian samples. Estimates of fO2 based on Fe-Ti oxides and D(sub Eu)/D(sub Gd) and D(sub Eu)/D(sub Sm) ratios suggest a range of fO2 values for SNC meteorites from IW+2.5 - IW+3.5 for Shergotty to IW- 2.0 - IW+0.2 for QUE94201. Fe(3+)/Fe(2+) is also a function of f(sub O2), and synchrotron micro-XANES values for olivine, pyroxene, and feldspar Fe(3+) have been reported. However, the relationship between the reported Fe(3+) values and the other methods for estimating f(sub O2) is not clear, and further measurements of Fe(3+)/Fe(2+) by a more conventional technique have been needed. Accordingly, in this project, new Mossbauer spectroscopy data on mineral separates handpicked from 10 SNC meteorites are reported.

  7. Investigation by sup 5 sup 7 Fe- Moessbauer spectroscopy of some pyrite samples of different Romanian natural deposits

    CERN Document Server

    Constantinescu, S; Calogero, S

    2002-01-01

    Extracted pyrites from four Romanian geological deposits have been investigated by Moessbauer spectroscopy. The room temperature results of this investigation have been correlated with the data of sulfur isotope ratio and minor elements analysis of pyrite samples. The presence of three signals is identified in the Moessbauer spectra. They correspond to the two crystalline structure of FeS sub 2 while the third is suggested to be assigned to one of the components of the iron-sulfur-arsenic series of investigated minerals. (authors)

  8. Studies of Fe-binding sites within multiwall carbon nanotubes using Moessbauer spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Luberda-Durnas, Katarzyna; Nieznalska, Magdalena; Matlak, Krzysztof; Korecki, Jozef; Burda, Kvetoslava [Faculty of Physics and Applied Computer Science, AGH - University of Science and Technology, Krakow (Poland); Mazurkiewicz, Marta; Malolepszy, Artur [Faculty of Material Science and Engineering, Warsaw University of Technology, Warsaw (Poland); Khachataryan, Gohar; Khachataryan, Karen; Tomasik, Piotr; Michalski, Oskar [Department of Chemistry, Agricultural University, Krakow (Poland); Stobinski, Leszek [Faculty of Material Science and Engineering, Warsaw University of Technology, Warsaw (Poland); Institute of Physical Chemistry, Polish Academy of Sciences, Warsaw (Poland)

    2011-08-15

    The potential applications of carbon nanotubes (CNTs) are strongly related to their physical and chemical properties. In this work, results of different methods for the oxidation of crude CNTs are reported. These methods changed Fe binding sites within multiwall carbon nanotubes (MWCNTs). Moessbauer spectroscopy was used to detect the chemical properties of the Fe-phases in MWCNTs. Signals from the iron carbide Fe{sub 3}C were the main components in the Moessbauer spectra of unmodified MWCNTs revealing magnetic ordering even at 300 K. In oxidized MWCNTs, the amount of Fe{sub 3}C decreased and {gamma}-Fe and {alpha}-Fe, ferrihydrates of iron oxides and different forms of goethite appeared. In MWCNTs oxidized with HClO{sub 4}, a significant fraction ({proportional_to}24%) of magnetically ordered Fe{sub 2}O{sub 3} particles was detected. This study showed that traces of iron catalyst embedded in MWCNTs could be used as a sensitive probe to monitor various MWCNT modifications. (Copyright copyright 2011 WILEY-VCH Verlag GmbH and Co. KGaA, Weinheim)

  9. Application of Moessbauer spectroscopy to the study of tannins inhibition of iron and steel corrosion

    Energy Technology Data Exchange (ETDEWEB)

    Jaen, Juan A., E-mail: jjaen@ancon.up.ac.pa [Universidad de Panama, CITEN, Depto. de Quimica Fisica (Panama); Obaldia, J. De; Rodriguez, M. V. [Universidad de Panama, Escuela de Quimica, Facultad de Ciencias Naturales, Exactas y Tecnologia (Panama)

    2011-11-15

    The inhibitory effect of tannins was investigated using, among others, potentiodynamic polarizations and Moessbauer spectroscopy. These techniques confirmed that the nature, pH and concentration of tannic solution are of upmost importance in the inhibitory properties of the solutions. It is observed that at low tannin concentration or pH, both, hydrolizable and condensed tannins, effectively inhibit iron corrosion, due to the redox properties of tannins. At pH Almost-Equal-To 0, Moessbauer spectra of the frozen aqueous solutions of iron(III) with the tannin solutions showed that iron is in the form of a monomeric species [Fe(H{sub 2}O){sub 6}]{sup 3 + }, without coordination with the functional hydroxyl groups of the tannins. The suspended material consisted of amorphous ferric oxide and oxyhydroxides, though with quebracho tannin partly resulted in complex formation and in an iron (II) species from a redox process. Other tannins, such as chestnut hydrolysable tannins, do not complex iron at this low pH. Tannins react at high concentrations or pH (3 and 5) to form insoluble blue-black amorphous complexes of mono-and bis-type tannate complexes, with a relative amount of the bis-ferric tannate generally increasing with pH. Some Fe{sup 2 + } in the form of hydrated polymeric ferrous tannate could be obtained. At pH 7, a partially hydrolyzed ferric tannate complex was also formed. The latter two phases do not provide corrosion protection. Tannin solutions at natural pH react with electrodeposited iron films (approx. 6 {mu}m) to obtain products consisting only on the catecholate mono-complex of ferric tannate. Some aspects of the mechanism of tannins protection against corrosion are discussed.

  10. Charge structure and cation distribution on Fe-Ga chalcogenide spinel by neutron diffraction and Moessbauer spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Kim, Sam Jin; Son, Bae Soon; Shim, In Bo; Kim, Chul Sung [Kookmin University, Seoul (Korea, Republic of); Hong, Kun Pyo [Korea Atomic Energy Research Institute, Taejon (Korea, Republic of)

    2005-07-01

    FeGa{sub x}Cr{sub 2-x}S{sub 4} (x=0.1 and 0.3) have been studied with x-ray, neutron difraction, and Moessbauer spectroscopy. Rietveld refinement of x-ray, neutron diffraction, and Moessbauer spectroscopy lead to the conclusion that the samples are in inverse spinel type, where the majority of Ga ions are present at tetrahedral site (A). The neutron diffractions on FeGa{sub x}Cr{sub 2-x}S{sub 4} (x=0.1) above 10 K show long range interaction behaviors and reveal an antiferromagnetic ordering, with the magnetic moment of Fe{sup 2+}(- 3.45 {mu}{sub B}) aligned antiparallel to Cr{sup 3+} (+2.89 {mu}{sub B}) at 10 K. Fe ions migrate from the tetrahedral (A) site to the octahedral (B) site with increase of Ga substitutions. The electric quadrupole splittings of the A and B sites in Moessbauer spectra give a direct evidence that Ga ion stimulate asymmetric charge distribution of Fe ions in the A site.

  11. Unfolding the role of iron in Li-ion conversion electrode materials by {sup 57}Fe Moessbauer spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Tirado, Jose L., E-mail: iq1ticoj@uco.es; Lavela, Pedro; Perez Vicente, Carlos; Leon, Bernardo; Vidal-Abarca, Candela [Universidad de Cordoba, Laboratorio de Quimica Inorganica (Spain)

    2012-03-15

    {sup 57}Fe Moessbauer spectroscopy is particularly useful in the study of oxide and oxalate conversion anode materials for Li-ion batteries. After reduction in lithium test cells, all these materials showed Moessbauer spectra ascribable to iron atoms in two different environments with superparamagnetic relaxation. The spectra recorded at 12 K revealed the ferromagnetic character in agreement with particle sizes of ca. 5 nm. The two types of iron can be ascribed then to surface and core atoms. Core iron atoms play an important role to retain high faradic capacity values for a large number of cycles. These atoms are preserved from irreversible reactions with the electrolyte and hence they promote a high reversibility and rate capability.

  12. DyNi{sub 2}Mn-magnetisation and Moessbauer spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Wang Jianli; Campbell, Stewart James, E-mail: stewart.campbell@adfa.edu.au [University of New South Wales, School of Physical, Environmental and Mathematical Sciences (Australia); Kennedy, Shane Joseph [ANSTO, Bragg Institute (Australia); Dou Shixue [University of Wollongong, Institute for Superconductivity and Electronic Materials (Australia); Wu Guangheng [Chinese Academy of Science, Institute of Physics (China)

    2012-03-15

    The physical properties of DyNi{sub 2}Mn doped with {sup 57}Fe have been investigated by X-ray diffraction, magnetisation (10-300 K) and {sup 57}Fe Moessbauer spectroscopy measurements (5-300 K). DyNi{sub 2}Mn({sup 57}Fe) crystallizes in the MgCu{sub 2}-type cubic structure (Fd{sup }-3m space group). The ordering temperature is found to be T{sub C} = 99(2) K, much higher than those of DyNi{sub 2} ({approx}22 K) and DyMn{sub 2} ({approx}35 K). Analyses of isothermal M-H curves and the related Arrott plots confirm that the magnetic phase transition at T{sub C} is second order. The magnetic entropy change around T{sub C} is 4.0 J/kg K for a magnetic field change of 0 T to 5 T. The spectra above T{sub C} exhibit features consistent with quadrupolar effects while below T{sub C} the spectra exhibit magnetic hyperfine splitting. The Debye temperature for DyNi{sub 2}Mn has been determined as {theta}{sub D} = 200(20) K from a fit to the variable temperature isomer shift IS(T).

  13. Microstructure of Fe implanted yttria stabilised zirconia studied by Moessbauer spectroscopy and TEM

    Energy Technology Data Exchange (ETDEWEB)

    Burggraaf, A.J.; Scholten, D.; Hassel, B.A. van

    1988-05-01

    Single crystalline and ceramic solid solutions of (1-0.chi)(ZrO/sub 2/)-(0.chi)(YO/sub 1.5/) with chi = 14-17 were implanted with high doses of Fe. Specific profile shapes were realised. The microstructure of the material before and after annealing was studied by conversion electron Moessbauer spectroscopy (CEMS), ion channeling and transmission electron microscopy (TEM). Initially Fe is present as metallic particles Fe/sup 0/ and as Fe/sup 2+/ and Fe/sup 3+/ ions. Their relative abundancy depends on the implantation conditions. Annealing leads to complete oxidation (Fe/sup 3+/) at low temperature and to the formation of microprecipitates of Fe/sub 2/O/sub 3/ (< 5 nm). A maximum of 4.5x10/sup 21/ Fe cm/sup -3/ can be substitutionally incorporated for Zr. This Fe is present in a metastable state. Ion channeling and electron diffraction experiments revealed that high fluence Fe implantation does not result in amorphisation but in recrystallisation of the matrix.

  14. Characterization of a mechanochemically activated titanium-hematite mixture: Moessbauer spectroscopy study

    Energy Technology Data Exchange (ETDEWEB)

    Cristobal, A.A. [Division Ceramicos - INTEMA, Universidad Nacional de Mar del Plata - CONICET, Av. J.B.Justo 4302, B7608FDQ Mar del Plata (Argentina); Ramos, C.P., E-mail: ciramos@cnea.gov.a [GIyA - CAC - CNEA, Av. Gral. Paz 1499, 1650 San Martin, Bs. As. (Argentina); CONICET (Argentina); Botta, P. [Division Ceramicos - INTEMA, Universidad Nacional de Mar del Plata - CONICET, Av. J.B.Justo 4302, B7608FDQ Mar del Plata (Argentina); Aglietti, E.F. [Centro de Tecnologia de Recursos Minerales y Ceramica - CETMIC, CONICET- CIC, Camino Parque Centenario y 506, B1897ZCA M.B.Gonnet (Argentina); Saragovi, C. [GIyA - CAC - CNEA, Av. Gral. Paz 1499, 1650 San Martin, Bs. As. (Argentina); Porto, J.M. [Division Ceramicos - INTEMA, Universidad Nacional de Mar del Plata - CONICET, Av. J.B.Justo 4302, B7608FDQ Mar del Plata (Argentina)

    2009-10-01

    Mechanochemical processes involving reactions between metals and crystalline oxides are of interest because of their potential technological applications in structural, magnetic or electric materials. In addition they can contribute to the understanding of the natural occurring processes that lead to the formation of minerals and soils. The controlled studies of how the distribution of cations in the titanomagnetites takes place can help toward building a model for the nature of their magnetism and, since they are the primary carriers of rock and soil magnetism, are therefore intensively investigated in many experimental and theoretical studies. In behalf of a better comprehension of the thermal, physical-chemical, magnetic and hyperfine behavior, we have considered a titanium and hematite mixture, with molar ratio Ti:Fe{sub 2}O{sub 3} of 1:2, mechanochemically activated during different activation times. We have studied the development of new phases by X-ray diffraction, scanning electron microscopy and Moessbauer spectroscopy. The evolution from the starting materials affected by different milling times and subsequent annealing shows that Ti reduces the Fe ions in the Fe{sub 2}O{sub 3} lattice, partly to Fe{sup 2+} and partly to metallic Fe.

  15. A Moessbauer spectroscopy and magnetometry study of magnetic multilayers and oxides

    CERN Document Server

    Bland, J

    2002-01-01

    A study of the magnetic properties of thin films, multilayers and oxides has been performed using Moessbauer spectroscopy and SQUID magnetometry. The systems studied are DyFe sub 2 , HoFe sub 2 and YFe sub 2 cubic Laves Phase thin films, DyFe sub 2 /Dy and DyFe sub 2 /YFe sub 2 multilayers; Ce/Fe and U/Fe multilayers; and iron oxide powders and thin films. CEMS results at room temperature show a low symmetry magnetic easy axis for all of the Laves Phase samples studied. Analysis of the dipolar and contact hyperfine fields show that this axis is close to the [2-bar41] and [3-bar51] directions but cannot be fully determined. The spin moments lie out of plane in all samples by approximately 22 deg, indicating a significant magneto-elastic anisotropy. 2.5 kG inplane applied field measurements indicate a much larger magnitude of magnetocrystalline anisotropy in the DyFe sub 2 system than in the YFe sub 2 system. In the DyFe sub 2 /YFe sub 2 multilayer samples the anisotropy is dominated by the dysprosium single-io...

  16. Design and construction of an electromechanical velocity modulator for Moessbauer spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Velasquez, A. A., E-mail: avelas26@eafit.edu.co; Carmona, A. [Universidad EAFIT, Grupo de Electromagnetismo Aplicado (Colombia); Velasquez, D.; Angel, L. [Universidad EAFIT, Grupo de Optica Aplicada (Colombia)

    2011-11-15

    In this paper we report the design, construction and characterization of an electromechanical velocity modulator for application in Moessbauer spectroscopy. The modulator was constructed with copper coils, Neodymium magnets, steel cores and polymeric membranes. The magnetic field in the driving and velocity sensing stages was analyzed by the finite element method, which showed a linear relation between the magnetic field in the region of motion of both coils and the position of the coils within the steel cores. The results obtained by computational simulation allowed us to optimize geometries and dimensions of the elements of the system. The modulator presented its first resonance frequency at 16.7 Hz, this value was in good agreement with that predicted by a second order model, which showed a resonant frequency of 16.8 Hz. The linearity of the velocity signal of the modulator was analyzed through an optical method, based on a Michelson-Morley interferometer, in which the modulator moved one of the mirrors. Results showed a satisfactory linearity of the velocity signal obtained in the sensing coil, whose correlation with a straight line was around 0.99987 for a triangular reference waveform.

  17. Trace cobalt speciation in bacteria and at enzymic active sites using emission Moessbauer spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Kamnev, A.A.; Antonyuk, L.P.; Smirnova, V.E.; Serebrennikova, O.B. [Laboratory of Biochemistry, Institute of Biochemistry and Physiology of Plants and Microorganisms, Russian Academy of Sciences, Saratov (Russian Federation); Kulikov, L.A.; Perfiliev, Yu.D. [Laboratory of Nuclear Chemistry Techniques, Department of Radiochemistry, Faculty of Chemistry, Moscow State University (Russian Federation)

    2002-02-01

    {sup 57}Co emission Moessbauer spectroscopy (EMS) allows the chemical state of cobalt, as influenced by its coordination environment, to be monitored in biological samples at its physiological (trace) concentrations. To draw attention to EMS as a valuable tool for speciation of cobalt in biocomplexes, the process of cobalt(II) metabolism in cells of the plant growth-promoting rhizobacterium Azospirillum brasilense Sp245 was investigated using EMS of {sup 57}Co{sup II}-doped bacterial cells. EMS measurements also showed {sup 57}Co{sup II}-activated glutamine synthetase (GS, a key enzyme of nitrogen metabolism, isolated from this bacterium) to have two different cobalt(II) forms at its active sites, in agreement with data available on other bacterial GSs. Chemical after-effects following electron capture by the nucleus of the parent {sup 57}Co{sup II} during the {sup 57}Co{yields}{sup 57}Fe transition, which contribute to the formation of a stabilised daughter {sup 57}Fe{sup III} component along with the nucleogenic {sup 57}Fe{sup II} forms, are also briefly considered. (orig.)

  18. Effect of titanium ion substitution in the barium hexaferrite studied by Moessbauer spectroscopy and X-ray diffraction

    Energy Technology Data Exchange (ETDEWEB)

    Quiroz, Pamela, E-mail: pamela.quiroz-penaranda@tu-ilmenau.de; Halbedel, Bernd [Ilmenau University of Technology, Department of Inorganic-Nonmetallic Materials, Institute of Materials Engineering (Germany); Bustamante, Angel, E-mail: angelbd1@gmail.com [San Marcos National University, Laboratory of Ceramics and Nanomaterials, Faculty of Physical Sciences (Peru); Gonzalez, Juan C. [Materials Science Institute of Sevilla - CSIC, Surfaces Research Group-Interfaces and Thin Films (Spain)

    2011-11-15

    A series of M-type barium hexaferrite has been synthesized in a glass melt by partially substituting the Fe{sub 2}O{sub 3} with TiO{sub 2} for investigation of their structure. The glass melt has the basic composition (mol%): 40 BaO + 33 B{sub 2}O{sub 3} + (27-x) Fe{sub 2}O{sub 3} + x TiO{sub 2} with x = 0, 3.6, 5.4 and 7.2 mol% TiO{sub 2}. The substituted ferrites were studied by means of X-ray diffraction, Moessbauer spectroscopy and vibration sample magnetometer. X-ray diffraction studies revealed that not all samples have a single ferritic phase, a small second phase corresponding to BaTi{sub 6}O{sub 13} was also observed to form. The Moessbauer spectra changed from magnetically ordered (x = 0) to magnetically ordered with strong line broadening. Moreover, the broadening increases with TiO{sub 2} content. The Moessbauer parameters suggested that Ti{sup 4 + } occupies the 2a and 12k crystal sites, and the Ti{sup 4 + } substitution on the 2b and 4f{sub 2} site also occurs at high melt dopings. Therefore, coercivity and saturation magnetization decreased.

  19. Moessbauer Spectra of Clays and Ceramics

    Energy Technology Data Exchange (ETDEWEB)

    Wagner, F. E.; Wagner, U. [Technische Universitaet Muenchen (Germany)

    2004-06-15

    The physical, chemical and mineralogical aspects of the use of Moessbauer spectroscopy in studies of clay-based ceramics are described. Moessbauer spectra of pottery clays fired under oxidising, reducing and changing conditions are explained, and the possibilities of using Moessbauer spectra to derive information on the firing temperatures and the kiln atmosphere during firing in antiquity are discussed and illustrated by examples.

  20. Moessbauer spectroscopy of Mg(0.9)Fe(0.1)SiO3 perovskite

    Science.gov (United States)

    Jeanloz, Raymond; O'Neill, Bridget; Pasternak, Moshe P.; Taylor, R. D.; Bohlen, Steven R.

    1992-01-01

    Ambient pressure Moessbauer spectra of Mg(0.9)Fe-57(0.1)SiO3 perovskite synthesized at pressure-temperature conditions of about 50 GPa and 1700 K show that the iron is entirely high-spin Fe(2+) and appears to be primarily located in the octahedral site within the crystal structure. We observe broad Moessbauer lines, suggesting a distribution of electric-field gradients caused by disorder associated with the Fe ions. Also, the perovskite exhibits magnetic ordering at temperatures lower than 5 K, implying that there is a magnetic contribution to the absolute ('third-law') entropy of this phase.

  1. Moessbauer effect of the alkaline and alkaline earth metal nitroprusside powders

    CERN Document Server

    Yang, T H; Kim, H S; Hong, C Y; Kim, H B; Cho, H Y; Kim, D Y; Moon, Y S

    2000-01-01

    We observe Moessbauer spectra of Fe atoms centered in nitroprusside anions of sodium nitroprusside (Na sub 2 [Fe(CN) sub 5 NO] 2H sub 2 O). potassium-nitroprusside (K sub 2 [Fe(CN)] sub 5 NO centre dot 2.5H sub 2 O), rubidium nitroprusside (Rb sub 2 [Fe(CN) sub 5 NO centre dot H sub 2 O), magnesium nitroprusside (Mg[Fe(CN) sub 5 NO], calcium nitroprusside (Ca[Fe(CN) sub 5 NO]centre dot 4H sub 2 O), and barium nitroprusside (Ba[Fe(CN) sub 5 NO]centre dot 3H sub 2 O) samples which have photochromic properties. We compare the Moessbauer parameters, the values of the isomer shifts and the quadrupole splittings of the samples with those of a sodium nitroprusside single crystal which is a standard material. The values of the isomer shifts and the quadrupole splittings of the various compounds are close to each other. The values of the line broadening of all samples are between 2.1 GAMMA sub N and 2.5 GAMMA sub N. The Moessbauer Lamb factors (f) are between 0.252(1) and 0.340(2). These values are obtained from the s...

  2. Soils from the Jabal Al-Akhdar region of North East Libya: Characterisation of the iron using chemical methods and Moessbauer spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Younis, A.M.; Kilcoyne, S.H. [School of Physics and Astronomy, University of St Andrews, Scotland (United Kingdom); Yacob, M. [Omar of Elmukhtar University, Soil and Water Department (Libyan Arab Jamahiriya); Goodman, B.A. [Scottish Crop Research Institute, Invergowrie, Dundee (United Kingdom)

    1999-11-15

    Soils from North East Libya have been investigated by X-ray diffraction, chemical analysis and Moessbauer spectroscopy. Quartz, kaolinite and illite were the main components identified by XRD in all specimens. Total and poorly ordered iron oxides were estimated using dithionite-citrate-bicarbonate (DCB) and oxalate extraction methods, respectively; in all cases, the oxalate-extractable iron represents a relatively minor fraction. Moessbauer spectroscopy showed the presence of substantial quantities of haematite and goethite, both in microcrystalline forms, but there was no systematic relationship between the relative proportions of these phases and the geographical origins of the soils.

  3. Magnetic structures of vanadium iodide (VI2): long- and short-range order and Moessbauer spectroscopy.

    NARCIS (Netherlands)

    Kuindersma, S. R.; Sanchez, J. P.; Haas, C.

    1980-01-01

    Neutron diffraction data of VI2 show a magnetic phase transition at 14 K from a 120° magnetic structure to a collinear structure. The collinear structure is compatible with low-temp. Moessbauer spectra. The 120° structure is not a magnetic phase with long-range order but rather a paramagnetic phase

  4. Study on the magnetic behavior of In-doped nickel chromite by using Moessbauer spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Hyun, Sung Wook; Kim, Chul Sung [Kookmin University, Seoul (Korea, Republic of); Park, Seung Iel [Sukwon Co. Ltd., Gumi (Korea, Republic of); Oh, Young Jei [Korea Institute of Science and Technology, Seoul (Korea, Republic of)

    2011-02-15

    NiCr{sub 1.9-x} {sup 57}Fe{sub 0.1}In{sub x}O{sub 4} (x = 0.0, 0.1, 0.3, and 0.5) was prepared by using a sol-gel method. The crystal structure at room temperature was determined to be a normal cubic spinel with space group Fd3m. An analysis of the x-ray diffraction patterns was performed using a Rietveld refinement method while the Bragg R{sub B} and R{sub F} factors were below 5%. The magnetic Neel temperature decreased from 150 K to 77 K with increasing In concentration, which was confirmed by zero-field-cooled (ZFC) magnetization at applied fields under 100 Oe and by Moessbauer spectra measured at various temperatures. Magnetic hysteresis loops of the samples at 77 K showed drastically increasing magnetization and decreasing coercivity with increasing In concentration. The Moessbauer spectra of the samples were measured at various temperatures ranging from 4.2 to 295 K. The isomer shift value showed that the charge states of the iron ions are ferric. The Moessbauer spectra showed two magnetic phases with two different magnetic spin direction sites for the Cr{sup 3+} ion state. Moessbauer spectra below 77 K showed 6 sharp absorption lines and the linewidth became broader with increasing temperature, which indicates a Jahn-Teller distortion and relaxation.

  5. {sup 57}Fe Moessbauer Spectroscopy Studies of Meteorites: Implications for Weathering Rates, Meteorite Flux, and Early Solar System Processes

    Energy Technology Data Exchange (ETDEWEB)

    Bland, P. A. [Open University, Planetary Science Research Institute (United Kingdom); Berry, F. J. [Open University, Department of Chemistry (United Kingdom); Jull, A. J. T. [University of Arizona, NSF Accelerator Facility for Radioisotope Analyses (United States); Smith, T. B. [Open University, Department of Physics and Astronomy (United Kingdom); Bevan, A. W. R. [Western Australian Museum, Department of Earth and Planetary Sciences (Australia); Cadogan, J. M. [University of New South Wales, School of Physics (Australia); Sexton, A. S.; Franchi, L. A.; Pillinger, C. T. [Open University, Planetary Science Research Institute (United Kingdom)

    2002-09-15

    Ordinary chondrite finds, terrestrial age dated using {sup 14}C analyses, from different meteorite accumulation sites, have been examined by Moessbauer spectroscopy to quantitatively determine terrestrial oxidation. We observe differences in weathering rates between sites, and also between different chondrite groups. A comparison of weathering over time, and its effect in 'eroding' meteorites, together with the number and mass distribution of meteorites in each region, enables us to derive estimates of the number of meteorite falls over a given mass per year. Studies of how the oxygen isotopic composition of samples varies with weathering indicate that incipient alteration may occur without a pronounced isotopic effect, possibly due to weathering of silicates to topotactically oriented smectite confined spaces where the water volume is limited. This finding has profound implications for the use of oxygen isotopes as a tool in understanding water-rock interaction. It also may reconcile previously contradictory data regarding the nebular or asteroidal location of pre-terrestrial aqueous alteration. Finally, Moessbauer spectroscopy is also found to be a useful tool in determining mineral abundance in carbonaceous chondrites, where a fine-grained matrix makes traditional approaches inapplicable. Again, the results have implications for the modification of chondritic materials in the early solar system.

  6. Evidence of Impact at the Permian/Triassic Boundary from Moessbauer Spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Verma, H. C.; Upadhyay, C. [Indian Institute of Technology, Department of Physics (India); Tripathi, R. P. [Jai Narain Vyas University, Department of Physics (India); Shukla, A. D.; Bhandari, N. [Physical Research Laboratory, Navrangpura (India)

    2002-06-15

    Sediment samples from Spiti valley, India, deposited about 250 Million years ago during the Permian-Triassic transition, have been analysed. {sup 57}Fe Moessbauer spectroscopic studies show that iron occurs mainly as nanoparticles of hematite and goethite with a broad size distribution. The results show a high degree of resemblance with the Cretaceous-Tertiary boundary (65 My) samples where an asteroidal impact is believed to have caused mass extinction.

  7. Moessbauer spectroscopy of the Zr-rich region in Zr-Nb-Fe alloys with low Nb content

    Energy Technology Data Exchange (ETDEWEB)

    Ramos, C. [Universidad de Buenos, Facultad de Ciencias Exactas y Naturales (Argentina); Saragovi, C. [Departamento de Fisica, Comision Nacional de Energia Atomica (Argentina); Granovsky, M.; Arias, D. [Departamento de Materiales, Comision Nacional de Energia Atomica (Argentina)

    1999-11-15

    Intermetallic phases and solid solutions in the Zr-rich region of the Zr-Nb-Fe system with low Nb content are studied by Moessbauer spectroscopy complemented with X-ray diffraction, optical and scanning electron microscopy and electron microprobe analysis. The phases found in each sample were those expected from the corresponding binary Zr-Fe system. Furthermore, one of the samples showed a ternary cubic Ti{sub 2}Ni type phase with a similar stoichiometry to the tetragonal Zr{sub 2}Fe compound. Moessbauer parameters were suggested to this phase (IS: - 0.12 mm/s, QS: 0.30 mm/s), to the bcc Zr({beta}) phase (IS: (-0.11 {alpha} 0.01) mm/s, QS: (0.23 {alpha} 0.02) mm/s), and to the hcp Zr({beta}{sup T}) phase (IS: (-0.24 {alpha} 0.02) mm/s, QS: (0.45 {alpha} 0.02) mm/s)

  8. Study of the interaction of ions iron (II) with poly aniline by X-ray, Moessbauer spectroscopy and conductivity;Estudo da interacao de ions ferro (II) com polianilina por espectroscopia Moessbauer, raios-X e condutividade

    Energy Technology Data Exchange (ETDEWEB)

    Fornazier Filho, Yonis; Silva Filho, Eloi Alves da, E-mail: yonis.fornazier@gmail.co [Universidade Federal do Espirito Santo (DQ/UFES), Vitoria, ES (Brazil). Dept. de Quimica; Filho, Evaristo N. [Universidade Federal do Espirito Santo (DF/UFES), Vitoria, ES (Brazil). Dept. de Fisica

    2009-07-01

    The study of the interaction of ions Fe (II) with polyaniline was done by obtaining this polymer in the form of salt esmeraldine (Pani-ES) on addition of salt Fe(NH{sub 4}){sub 2}(SO{sub 4}){sub 2}centre dot6H{sub 2}O in equimolar quantities in the temperature environment. We used the techniques of Moessbauer spectroscopy, X-ray diffraction (XRD) and measures of conductivity with application of pressure. The results showed that the occurs formation of the complex Pani-Fe (II) and indicate that the ion Fe (II) interacted with the benzenoid nitrogens groups of the polymeric chain. (author)

  9. Iron implantation in gadolinium gallium garnet studied by conversion-electron Moessbauer spectroscopy

    CERN Document Server

    Szucs, I; Fetzer, C; Langouche, G

    1998-01-01

    Gadolinium gallium garnet single crystals were implanted with doses of sup 5 sup 7 Fe ions in the range 8x10 sup 1 sup 5 - 6x10 sup 1 sup 6 atoms cm sup - sup 2. Depending on the dose, iron with Fe sup 2 sup + or Fe sup 3 sup + charge states was found to have formed after the implantation. After a subsequent annealing in air, the iron oxidized to Fe sup 3 sup +. The Moessbauer and channelling measurements showed lattice recrystallization taking place at 600 deg. C. After recrystallization, the iron was found to have substituted for gallium ions both at the octahedral and at the tetrahedral positions. The relative concentration of the two types of iron at the two sites shifted towards the equilibrium distribution upon high-temperature annealing. (author)

  10. Study of the S phase structure on the AISI 316L steel by X-ray diffraction and Moessbauer spectroscopy; Estudo da estrutura da fase S no aco AISI 316L por difracao de raios X e espectroscopia Moessbauer

    Energy Technology Data Exchange (ETDEWEB)

    Gontijo, L.C. [Centro Federal de Educacao Tecnologica do Espirito Santo, Vitoria, ES (Brazil). Coordenadoria de Ciencia e Tecnologia; Machado, R.; Nascente, P.A.P. [Universidade Federal de Sao Carlos, SP (Brazil). Dept. de Engenharia de Materiais]. E-mail: nascente@power.ufscar.br; Miola, E.J. [Universidade Federal de Sao Carlos, SP (Brazil). Dept. de Fisica; Casteletti, L.C. [Universidade de Sao Paulo, Sao Carlos, SP (Brazil). Dept. de Engenharia de Materiais, Aeronautica e Automobilistica

    2005-07-01

    The plasma-nitriding technology has been employed in the industry with the objective of improving the surface properties of metals and alloys. By using the conventional nitriding process at low temperature, some of the properties of the austenitic stainless steels are enhanced by the formation of the S phase, also called expanded austenite. This phase is formed on the surfaces of the austenitic stainless steels nitrided under certain conditions. In the past years, an extensive research has been carried out for the understanding of the S phase, but some questions remain with no answer or with contradictory explanations. In this work, the AISI 316L steel was plasma-nitrided at 350 and 400 deg C, and the samples were characterized by X-ray diffraction (XRD) and conversion electron Moessbauer spectroscopy (CEMS) in order to investigate the S phase. XRD analysis identified the presence of a distorted cubic structure phase. The layer consists of a distribution of nitrogen austenite with different content of nitrogen, ranging from approximately 10 to 40 at-%, and also {gamma}-Fe{sub 4}N and {epsilon}-Fe{sub 2-3}N phases. Moessbauer spectroscopy corroborates these results, and shows a decrease in nitrogen austenite with the increase in nitriding temperature. This decrease is related to the transformation of the nitrogen austenite to the {gamma}-Fe{sub 4}N phase. (author)

  11. Moessbauer spectroscopy and X-ray diffraction analyses of clayey samples used as ceramic sourcing materials, in Peru

    Energy Technology Data Exchange (ETDEWEB)

    Quille, Ruben, E-mail: quilleruben@gmail.com; Bustamante, Angel [San Marcos National University, Laboratory of Ceramics and Nanomaterials, Faculty of Physical Sciences (Peru); Palomino, Ybar [National University of San Cristobal de Huamanga, Experimental Center of Ceramics (Peru)

    2011-11-15

    The ceramic industry is an important area of economic activity in the Ayacucho Region, in particular in the District of Quinua. As a consequence, there is a huge demand for clay to produce ceramic pastes in that region. This paper reports on results concerning the mineralogical characterization of four clayey samples, which were collected MAA and SPQA from the area Pampa de La Quinua with geographic coordinates 13 Degree-Sign 02 Prime 49 Double-Prime S 74 Degree-Sign 08 Prime 03 Double-Prime W, CE1M and CE2M from the Quinua locality 13 Degree-Sign 03 Prime 07 Double-Prime S 74 Degree-Sign 08 Prime 31 Double-Prime W, both in the District of Quinua, Province of Huamanga, Ayacucho, Peru. The chemical and mineralogical characterization of these samples was carried out with powder X-ray diffraction detecting quartz, albite, montmorillonite, kaolinite and glauconite mineral phases, Moessbauer spectroscopy detected iron in kaolinite, glauconite and montmorillonite minerals. Chemical analysis was performed through scanning electron microscopy and energy dispersive X-ray spectroscopy. Data obtained from the combination of these techniques provided relevant information about the morphology, chemical composition, and the mineralogy of samples.

  12. Moessbauer study of the Jilin and Xinyang meteorites

    Energy Technology Data Exchange (ETDEWEB)

    Zhang Yuchang [North Carolina Univ., Asheville, NC (United States). Moessbauer Effect Data Center; Stevens, J.G. [North Carolina Univ., Asheville, NC (United States). Moessbauer Effect Data Center; Li Yushu [FEA Management, Inc., Grand Blanc, MI (United States); Li Zhaolin [Dept. of Geology, Zhongshan Univ., Guanzhou (China)

    1994-11-01

    The Xinyang and Jilin meteorites were investigated using Moessbauer spectroscopy. In addition to troilites and silicates, the Jilin meteorite contains taenite and kamacite, while the Xinyang meteorite contains kamacite only. The Moessbauer data of these two meteorites confirm them as ordinary H chondrites. The Moessbauer parameters can be interpreted by a model based on the cooling history of these meteorites. (orig.)

  13. Moessbauer spectroscopy description of limonite from Taraco, in the Huancane Province of the Puno Region, Peru

    Energy Technology Data Exchange (ETDEWEB)

    Bustamante, A., E-mail: abustamanted@unmsm.edu.pe [San Marcos National University, School of Physical Sciences (Peru); Cabrera, J.; Garcia, V.; Urday, E. [Saint Augustine National University in Arequipa, Electron Microscopy Center (Peru); Abdu, Y. A.; Scorzelli, R. B. [Centro Brasileiro de Pesquisas Fisicas (Brazil)

    2005-11-15

    Natural iron oxides are very common in nature and are the main components of many minerals, rocks and soils. There are a great variety of these minerals in Peru, especially in the Andes region. The mineral studied was extracted from the Taraco District in the Huancane Province of the Puno Region. The extracted sample is a yellowish mineral with very small particles which is called limonite. X-ray diffraction indicates the presence of goethite as the principal mineralogical phase and quartz as the secondary phase. The {sup 57}Fe Moessbauer spectra at room temperature show broadened spectra that were fitted using a distribution model. The most probable field of the magnetic component is 21T, corresponding to the presence of small particles of goethite, confirmed by the 4.2 K spectrum. MS of the calcinated sample in air at 900 deg. C show the presence of two hematite sextets, one related to bulk particles and another to surface particles. Chemical analysis using Scanning Electron Microscopy and Energy Dispersive X-ray Spectrometer indicates that O and Fe are the major components; other elements such as Al, Si, Mg and Ca are also present.

  14. The influence of ruthenium on the magnetic properties of gamma-Fe sub 2 O sub 3 (maghemite) studied by Moessbauer spectroscopy

    CERN Document Server

    Helgason, O; Berry, F J; Mosselmans, F

    2003-01-01

    Ruthenium-doped gamma-Fe sub 2 O sub 3 has been synthesized and examined by x-ray powder diffraction, XANES, EXAFS and by sup 5 sup 7 Fe Moessbauer spectroscopy. Ruthenium K-edge x-ray absorption spectroscopy shows that ruthenium adopts a fully occupied octahedral site in the spinel related gamma-Fe sub 2 O sub 3 structure as Ru sup 4 sup +. The sup 5 sup 7 Fe Moessbauer spectra recorded in the presence of a longitudinal magnetic field of 6 T confirmed the octahedral coordination of the tetravalent ions and canting angles for the Fe sup 3 sup + ions were determined as 24 deg. for those in octahedral sites and 33 deg. for those in tetrahedral sites. The sup 5 sup 7 Fe Moessbauer spectra recorded in situ from ruthenium-doped gamma-Fe sub 2 O sub 3 showed parameters typical of maghemite up to 600 K but with a magnetic hyperfine field distribution suggesting an inhomogeneous distribution of ruthenium within particles of varied size around about 15 nm. At 700 K a phase transition from gamma-Fe sub 2 O sub 3 to alp...

  15. Room temperature {sup 57}Fe Moessbauer spectroscopy of ordinary chondrites from the Atacama Desert (Chile): constraining the weathering processes on desert meteorites

    Energy Technology Data Exchange (ETDEWEB)

    Valenzuela, M., E-mail: edvalenz@cec.uchile.cl [Universidad de Chile, Departamento de Geologia (Chile); Abdu, Y.; Scorzelli, R. B., E-mail: scorza@cbpf.br; Duttine, M. [Centro Brasileiro de Pesquisas Fisicas (CBPF/MCT) (Brazil); Morata, D. [Universidad de Chile, Departamento de Geologia (Chile); Munayco, P. [Centro Brasileiro de Pesquisas Fisicas (CBPF/MCT) (Brazil)

    2007-02-15

    We report the results of a study on the weathering products of 21 meteorites found in the Atacama Desert (Chile) using room temperature {sup 57}Fe Moessbauer spectroscopy (MS). The meteorites are weathered ordinary chondrites (OCs) with unknown terrestrial ages and include the three chemical groups (H, L, and LL). We obtained the percentage of all the Fe-bearing phases for the primary minerals: olivine, pyroxene, troilite and Fe-Ni metal, and for the ferric alteration products (composed of the paramagnetic Fe{sup 3+} component and the magnetically ordered Fe{sup 3+} components) which gives the percentage of oxidation of the samples. From the Moessbauer absorption areas of these oxides, the terrestrial oxidation of the Atacama OC was found in the range from {approx}5% to {approx}60%. The amount of silicates as well as the opaques decreases at a constant rate with increasing oxidation level.

  16. Structural and Electronic Properties Study of Colombian Aurifer Soils by Moessbauer Spectroscopy and X-ray Diffraction

    Energy Technology Data Exchange (ETDEWEB)

    Bustos Rodriguez, H., E-mail: hbustos@ut.edu.co; Rojas Martinez, Y.; Oyola Lozano, D. [Universidad del Tolima, Departamento de Fisica (Colombia); Perez Alcazar, G. A.; Fajardo, M. [Universidad del Valle, Departamento de Fisica (Colombia); Mojica, J. [Ingeominas Valle, Departamento de Geologia (Colombia); Molano, Y. J. C. [Universidad Nacional, Departamento de Geologia (Colombia)

    2005-02-15

    In this work a study on gold mineral samples is reported, using optical microscopy, X-ray diffraction (XRD) and Moessbauer spectroscopy (MS). The auriferous samples are from the El Diamante mine, located in Guachavez-Narino (Colombia) and were prepared by means of polished thin sections. The petrography analysis registered the presence, in different percentages that depend on the sample, of pyrite, quartz, arsenopyirite, sphalerite, chalcopyrite and galena. The XRD analysis confirmed these findings through the calculated cell parameters. One typical Rietveld analysis showed the following weight percent of phases: 85.0% quartz, 14.5% pyrite and 0.5% sphalerite. In this sample, MS demonstrated the presence of two types of pyrite whose hyperfine parameters are {delta}{sub 1} = 0.280 {+-} 0.002 mm/s and {Delta}{sub 1} = 0.642 {+-} 0.002 mm/s, {delta}{sub 2} = 0.379 {+-} 0.002 mm/s and {Delta}{sub 2} = 0.613 {+-} 0.002 mm/s.

  17. Evidences of the stability of magnetite in soil from Northeastern Argentina by Moessbauer spectroscopy and magnetization measurements

    Energy Technology Data Exchange (ETDEWEB)

    Causevic, H. [Department of Physics, CNEA, Av. Gral. Paz 1499, 1650, Buenos Aires (Argentina); Morras, H. [INTA-CIRN, Institute of Soils, Villa Udaondo, 1712 Castelar (Argentina); Mijovilovich, A. [Chemistry Department, University of Michigan, 930 North University Av., Ann Arbor, MI-48109-1055 (United States); Saragovi, C. [Department of Physics, CNEA, Av. Gral. Paz 1499, 1650, Buenos Aires (Argentina)]. E-mail: saragovi@cnea.gov.ar

    2004-12-31

    In red soils from southern Brazil magnetite was reported to be pedogenically unstable, weathering to maghemite. However, in similar soils from northeastern Argentina magnetite was found in all size fractions. This finding motivates the mineralogical study of an Ultisol at different depths in order to understand the influence of anthropic and natural factors in the weathering of the magnetic minerals of these subtropical soils. The sand fraction of the B{sub t22} horizon (105-155 cm depth) of a clayey red Ultisol from the subtropical forest of Misiones, Argentina, was studied by X-ray diffraction, saturation magnetization {sigma}{sub s}, optical microscopy and Moessbauer spectroscopy. Saturation magnetization for the whole sand fraction (wsf), the non-magnetic sand fraction (nmsf) and the magnetic sand fraction (msf) are 10.79, 1.50 and 16.92 JT{sup -1} kg{sup -1}, respectively. Mainly quartz, ilmenite, Al-substituted hematite, goethite, maghemite and magnetite are found. Magnetite-maghemite contents are high, and magnetite is predominant in the msf. Results are compared with those from the upper B{sub 1} horizon (10-35 cm depth) of the same soil in which a lower {sigma}{sub s(wsf)} value, and higher values of {sigma}{sub s(msf)} and of ({sigma}{sub s(msf)}-{sigma}{sub s(wsf)}) were measured. These results confirm the stability of magnetite in this soil contrasting with other results on soils from neighbouring areas.

  18. Moessbauer study of thermal metamorphosed Antarctic meteorites

    Energy Technology Data Exchange (ETDEWEB)

    Scorzelli, R.B. (Centro Brasileiro de Pesquisas Fisicas, Rio de Janeiro, RJ (Brazil)); Galvao da Silva, E. (Centro Brasileiro de Pesquisas Fisicas, Rio de Janeiro, RJ (Brazil) Dept. de Fisica, Univ. Federal de Minas Gerais, Belo Horizonte (Brazil)); Souza Azevedo, I. (Centro Brasileiro de Pesquisas Fisicas, Rio de Janeiro, RJ (Brazil))

    1994-02-01

    In this paper we report on variable temperature Moessbauer spectroscopy measurements on Yamato-82162 and Yamato-86720. These Antarctic carbonaceous chondrites contrast with other non-Antarctic carbonaceous chondrites in which no evidences of thermal metamorphism have been found. (orig.)

  19. Moessbauer studies of ternary superconductors

    Energy Technology Data Exchange (ETDEWEB)

    Kimball, C.W.; Van Landuyt, G.L.; Barnet, C.D.; Shenoy, G.K.; Dunlap, B.D.; Fradin, F.Y.

    1978-01-01

    Moessbauer studies of the ternary Chevrel phase and rare earth rhodium boride superconductors have been made. Anomalous phonon properties at the Sn site in SnMo/sub 6/S/sub 8/, SnMo/sub 6/Se/sub 8/, and La/sub 0/ /sub 98/Sn/sub 0/ /sub 02/Mo/sub 6/Se/sub 8/ have been investigated. Studies of polarization of conduction electrons at the site of the magnetic ion have been made by means of the /sup 151/Eu Moessbauer effect in Eu/sub x/Sn/sub 1-x/Mo/sub 6/S/sub 8/ and the effects of such polarization on superconducting properties discussed. The Moessbauer effect in /sup 166/Er has been used to investigate the electronic ground state in the ternary compound ErRh/sub 4/B/sub 4/ both in the superconducting and magnetically ordered states.

  20. Nuclear gamma resonance absorption (Moessbauer) spectroscopy as an archaeometric technique to assess chemical states of iron in a Tupiguarani ceramic artifact from Corinto, Minas Gerais, Brazil

    Energy Technology Data Exchange (ETDEWEB)

    Floresta, D.L.; Ardisson, J.D., E-mail: denise.floresta@ifmg.edu.br, E-mail: jdr@cdtn.br [Centro de Desenvolvimento da Tecnologia Nuclear (CDTN/CNEN-MG), Belo Horizonte, MG (Brazil); Fagundes, M.; Fabris, J.D., E-mail: marcelo.fagundes@ufvjm.edu.br, E-mail: jdfabris@ufmg.edu.br [Universidade Federal dos Vales do Jequitinhonha e Mucuri (LAEP/UFVJM), Diamantina, MG (Brazil). Lab. de Arqueologia e Estudos da Paisagem

    2013-07-01

    Archaeological ceramics of Tupiguarani Tradition are found in many parts throughout the Brazilian territory and have many similarities. Fragments of Tupiguarani pottery found in the archaeological site known as Beltrao, in the municipality of Corinto, state of Minas Gerais, were identified and collected by researchers of the LAEP/UFVJM, in Diamantina, also in Minas Gerais. A selected fragment of about 15 mm-thick, with a color gradation across the ceramic wall ranging from red, on one side, grayish in the middle and orange on the opposite side, was transversely cut and a series of subsamples of powdered materials were collected from different depths across the wall, in layer segments of ∼3 mm, from the orange side. These powdered subsamples were analyzed with X-ray fluorescence and diffraction spectroscopy and {sup 57}Fe Moessbauer spectroscopy at room temperature (298 K) and at 80 K. According to the XRF results, the elementary composition does not clearly vary with the depth in the sample. The powder XRD analysis revealed the occurrence mainly of quartz and muscovite. Results of {sup 57}Fe Moessbauer spectroscopy reveal that hematite is the magnetically ordered phase. An Fe{sup 2+} component appears for the grayish subsample. According to these results, the red subsample seems to be the external part of the pottery, representing the side that had direct contact with fire used to burn the precursor clay in air for this primitive ceramics preparation. The grayish middle layer is probably due to burning clay mixed with some ashes containing residual carbon, under milder temperature than on the external . (author)

  1. Moessbauer spectroscopy study of a mineral sample from Oshno Hill, District of Chavin de Pariarca, Huanuco Region, Peru

    Energy Technology Data Exchange (ETDEWEB)

    Bustamante, A., E-mail: abustamanted@unmsm.edu.pe [Universidad Nacional Mayor de San Marcos, Laboratorio de Ceramicos y Nanomateriales, Facultad de Ciencias Fisicas (Peru); Lovera, D. [Universidad Nacional Mayor de San Marcos, Facultad de Ingenieria Geologica, Minera, Metalurgica y Geografica (Peru); Quille, R. [Universidad Nacional Mayor de San Marcos, Laboratorio de Ceramicos y Nanomateriales, Facultad de Ciencias Fisicas (Peru); Arias, A. V.; Quinones, J. [Universidad Nacional Mayor de San Marcos, Facultad de Ingenieria Geologica, Minera, Metalurgica y Geografica (Peru)

    2010-01-15

    The analysis by X-ray diffraction of a mining sample collected from Oshno hill, which is located in the District of Chavin de Pariarca, Huamalies Province, Huanuco, Peru, indicates the presence of lepidocrocite ({gamma}-FeOOH) and goethite ({alpha}-FeOOH). The room temperature Moessbauer spectrum (MS) doublet with broad lines displays hyperfine parameters corresponding to the presence of particles of iron hydroxides smaller than 100 A in a superparamagnetic regime. The measurement of a MS at 4.2 K allowed confirming the presence of goethite and lepidocrocite (with average magnetic fields of 49.21 T and 44.59 T, respectively).

  2. Characterization of the Carancas-Puno meteorite by energy dispersive X-ray fluorescence, X-ray diffractometry and transmission Moessbauer spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Ceron Loayza, Maria L., E-mail: malucelo@hotmail.com; Bravo Cabrejos, Jorge A. [Universidad Nacional Mayor de San Marcos, Laboratorio de Analisis de Suelos, Facultad de Ciencias Fisicas (Peru)

    2011-11-15

    We report the results of the study of a meteorite that impacted an inhabited zone on 15 September 2007 in the neighborhood of the town of Carancas, Puno Region, about 1,300 km south of Lima. The analysis carried out by energy dispersive X-ray fluorescence, X-ray diffractometry and transmission Moessbauer spectroscopy (at room temperature and at 4.2 K), reveal the presence in the meteorite sample of magnetic sites assigned to taenite (Fe,Ni) and troilite (Fe,S) phases, and of two paramagnetic doublets assigned to Fe{sup 2 + }, one associated with olivine and the other to pyroxene. In accord with these results, this meteorite is classified as a type IV chondrite meteorite.

  3. Microstructure, magnetic properties and TMR effect of Fe-SiO{sub 2} granular films investigated by Moessbauer spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Ge Shihui E-mail: gesh@lzu.edu.cn; Xi Li; Zhang Zongzhi E-mail: zhangzz@lzu.edu.cn; Liu Yapi; Li Chengxian

    2001-05-01

    Fe-SiO{sub 2} granular films with various metal volume fractions ( f{sub v}) were fabricated by RF co-sputtering. The microstructure and magnetic properties as well as the tunneling magnetoresistance (TMR) were systematically investigated. The TMR exists in the samples with f{sub v}<0.5, and the Fe{sub 0.33}(SiO{sub 2}){sub 0.67} film exhibits the largest TMR value of -3.3% at room temperature under 1.3 T magnetic field. The transmission electron microscopy images indicate that these samples consist of small Fe particles with the size range from 1.0 to 15.0 nm separated by insulating SiO{sub 2} matrix and exhibit TMR effect. Moessbauer measurement reveals that more superparamagnetic Fe component and less paramagnetic Fe{sub 2}SiO{sub 4} are in favor of the higher probability of spin-dependent tunneling, thus larger TMR value. For the samples with f{sub v}{>=}0.43, Moessbauer study shows the existence of perpendicular magnetic anisotropy, and the strongest perpendicular magnetic anisotropy was observed in the sample of Fe{sub 0.47}(SiO{sub 2}){sub 0.53}. This phenomenon may be ascribed to the stress anisotropy in this film.

  4. Moessbauer study of synthetic jarosites

    Energy Technology Data Exchange (ETDEWEB)

    Kovacs, K., E-mail: kkriszti@bolyai.elte.hu [Eoetvoes Lorand University, Laboratory of Nuclear Chemistry, Institute of Chemistry (Hungary); Kuzmann, E. [Hungarian Academy of Sciences, Laboratory of Nuclear Chemistry, Chemical Research Center (Hungary); Homonnay, Z.; Vertes, A. [Eoetvoes Lorand University, Laboratory of Nuclear Chemistry, Institute of Chemistry (Hungary); Gunneriusson, L. [Lulea University of Technology, Division of Chemistry (Sweden); Sandstroem, A. [Lulea University of Technology, Division of Process Metallurgy (Sweden)

    2008-09-15

    {sup 57}Fe Moessbauer spectroscopy and PXRD were used to study artificially prepared jarosites with the compositions of KFe{sub 3}(SO{sub 4}){sub 2}(OH){sub 6-x}F{sub x}x 0 - 1.6 PXRD measurements revealed single phase jarosite samples. All Moessbauer spectra taken at room temperature exhibit a quadrupole doublet corresponding to mineral jarosite. However, at low temperature where the mineral jarosite has a well resolved sextet, the synthetic jarosite even with x = 0 F{sup -} content shows a relaxation transition. The spectra indicate that with increasing F{sup -} concentration, the paramagnetic-antiferromagnetic transition temperature is decreasing. The results can be used in the analysis of artificial jarosites or those formed during biomineralization processes.

  5. Thermal treatment of the Fe{sub 78}Si{sub 9}B{sub 13} alloy in it amorphous phase studied by means of Moessbauer spectroscopy; Tratamiento termico de la aleacion Fe{sub 78}Si{sub 9}B{sub 13} en su fase amorfa estudiado por medio de la espectroscopia Moessbauer

    Energy Technology Data Exchange (ETDEWEB)

    Cabral P, A. [ININ, 52045 Ocoyoacac, Estado de Mexico (Mexico); Lopez, A.; Garcia S, F. [Facultad de Ciencias, UAEM, 50000 Toluca, Estado de Mexico (Mexico)

    2003-07-01

    The magnetic and microhardness changes, dependents of the temperature that occur in the Fe{sub 78}Si{sub 9}B{sub 13} alloy in it amorphous state were studied by means of the Moessbauer spectroscopy and Vickers microhardness. According to the Moessbauer parameters and in particular that of the hyperfine magnetic field, this it changes according to the changes of the microhardness; i.e. if the microhardness increases, the hyperfine magnetic field increases. The registered increment of hardness in the amorphous state of this alloy should be considered as anomalous, according to the prediction of the Hall-Petch equation, the one that relates negative slopes with grain sizes every time but small. (Author)

  6. Comparative study of the iron cores in human liver ferritin, its pharmaceutical models and ferritin in chicken liver and spleen tissues using Moessbauer spectroscopy with a high velocity resolution

    Energy Technology Data Exchange (ETDEWEB)

    Alenkina, I.V.; Semionkin, V.A. [Faculty of Physical Techniques and Devices for Quality Control, Ural Federal University, Ekaterinburg (Russian Federation); Faculty of Experimental Physics, Ural Federal University, Ekaterinburg (Russian Federation); Oshtrakh, M.I. [Faculty of Physical Techniques and Devices for Quality Control, Ural Federal University, Ekaterinburg (Russian Federation); Klepova, Yu.V.; Sadovnikov, N.V. [Faculty of Physiology and Biotechnology, Ural State Agricultural Academy, Ekaterinburg, (Russian Federation); Dubiel, S.M. [Faculty of Physics and Applied Computer Science, AGH University of Science and Technology, Krakow (Poland)

    2011-07-01

    Full text: Application of the Moessbauer spectroscopy with a high velocity resolution (4096 channels) for a study of iron-containing biological species is of great interest. Improving the velocity resolution allows to reveal small variations in the electronic structure of iron, and to obtain hyperfine parameters with smaller instrumental (systematic) errors in comparison with measurements performed in 512 channels or less. It also allows a more reliable fitting of complex Moessbauer spectra. In the present study the Moessbauer spectroscopy with the high velocity resolution was used for a comparative analysis of ferritin and its pharmaceutically important models as well as iron storage proteins in a chicken liver and a spleen. The ferritin, an iron storage protein, consists of a nanosized polynuclear iron core formed by a ferrihydrite surrounded by a protein shell. Iron-polysaccharide complexes contain {beta}-FeOOH iron cores coated with various polysaccharides. The Moessbauer spectra of the ferritin and commercial products Imferon, MaltoferR and Ferrum Lek as well as those of the chicken liver and spleen tissues were measured with the high velocity resolution at 295 and 90 K. They were fitted using two models: (1) with a homogeneous iron core (an approximation using one quadrupole doublet), and (2) with a heterogeneous iron core (an approximation using several quadrupole doublets). The model (1) can be used as the first approximation fit to visualize small variations in the hyperfine parameters. Using this model, differences in the Moessbauer hyperfine parameters were obtained in both 295 and 90 K Moessbauer spectra. However, this model was considered as a rough approximation because the measured Moessbauer spectra had non-Lorentzian line shapes. Therefore, the spectra of the ferritin, Imferon, MaltoferR and Ferrum Lek as well as those of the liver and spleen tissues were fitted again using the model (2) in which a different number of the quadrupole doublets was

  7. Effect of Ti{sup 4+} substitution on the hyperfine properties of Li-Sb-Ti ferrites using Moessbauer spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Chongtham, Shivaji, E-mail: schongtham@rediffmail.com [Manipur Science and Technology Council, R and D Division (India); Soibam, Ibetombi; Phanjoubam, Sumitra; Sarma, H. N. K. [Manipur University, Department of Physics (India); Verma, H. C. [IIT Kanpur, Department of Physics (India)

    2008-11-15

    Moessbauer investigations were carried out at room temperature on the ferrite system Li{sub 0.6+0.5t}Fe{sub 2.3-1.5t}Ti{sub t}Sb{sub 0.1}O{sub 4} (0.0 {<=} t {<=} 1.0 in steps of 0.2). The effect of Ti{sup 4+} concentration on the various hyperfine interactions like Isomer shift, quadrupole splitting and internal magnetic field have been studied. The spectra exhibited well-defined Zeeman sextets at low substitution level, corresponding to the A and B sites. The sample with t = 1.0 showed paramagnetic behaviour. The results obtained have been discussed.

  8. Paramagnetic relaxation line shape in the Moessbauer spectroscopy of 1/2. -->. 3/2 transitions in axial symmetry

    Energy Technology Data Exchange (ETDEWEB)

    Dunlap, B.D. (Argonne National Lab., IL); Shenoy, G.K.; Asch, L.

    1976-01-01

    Hirst's theory for the line shape of Moessbauer spectra in the presence of paramagnetic relaxation phenomena is applied to the case of /sup 1///sub 2/ ..-->.. /sup 3///sub 2/ transitions. A detailed procedure for obtaining the lineshape is given for the case of axial symmetry, including off-diagonal terms in the hyperfine Hamiltonian. This is applicable for example, to the 14.4-keV transition in /sup 57/Fe or the 66.7-keV transition in /sup 171/Yb. The theory is used to analyze the data for /sup 171/Yb in the cubic compound Cs/sub 2/NaYbCl/sub 6/. The hyperfine parameter A = -38.7 +- 2.0 mm/s and relaxation rate W = 185 +- 24 MHz are in good agreement with previous measurements utilizing the resonance of /sup 170/Yb in this material.

  9. Influence of a thermochromic anion on the spin crossover of iron(II) trinuclear complexes probed by Moessbauer spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Robert, Francois; Naik, Anil D; Garcia, Yann, E-mail: yann.garcia@uclouvain.b [Institut de la Matiere Condensee et des Nanosciences, Universite Catholique de Louvain, Place L. Pasteur 1, 1348 Louvain-la-Neuve (Belgium)

    2010-03-01

    The insertion of thermochromic anions (1 and 2) into triazole based iron(II) trinuclear spin crossover complexes [Fe{sup II}{sub 3}(hyetrz){sub 6}(H{sub 2}O){sub 6}](1 or 2){sub 4}Cl{sub 2} paves the way to a large panel of multifunctional materials. In addition to a gradual thermo-induced spin conversion of the central metal ion on cooling below room temperature, an unexpected split of the Moessbauer signal of the external iron(II) ions as well as pronounced relaxation phenomenon for the central HS iron(II) ion was discovered. This phenomenon is suggested to be induced by the tautomeric equilibrium between enol and keto forms of the anion.

  10. Characterization of mineral phases of agricultural soil samples of Colombian coffee using Moessbauer spectroscopy and X-ray diffraction

    Energy Technology Data Exchange (ETDEWEB)

    Rodriguez, Humberto Bustos, E-mail: hbustos@ut.edu.co; Lozano, Dagoberto Oyola; Martinez, Yebrayl Antonio Rojas; Pinilla, Marlene Rivera [Universidad del Tolima, Grupo Ciencia de Materiales y Tecnologia en Plasma (Colombia); Alcazar, German Antonio Perez [Universidad del Valle, Grupo Metalurgia Fisica y Teoria de las Transiciones de Fase (Colombia)

    2012-03-15

    Soil chemical analysis, X-ray diffraction (XRD) and Moessbauer spectrometry (MS) of {sup 57}Fe were used to characterize mineral phases of samples taken from the productive layer (horizon A) of agricultural coffee soil from Tolima (Colombia). Chemical analysis shows the chemical and textural parameters of samples from two different regions of Tolima, i.e., Ibague and Santa Isabel. By XRD phases like illite (I), andesine (A) and quartz (Q) in both samples were identified. The quantity of these phases is different for the two samples. The MS spectra taken at room temperature were adjusted by using five doublets, three of them associated to Fe{sup + 3} type sites and the other two to Fe{sup + 2} type sites. According to their isomer shift and quadrupole splitting the presence of phases like illite (detected by DRX), nontronite and biotite (not detected by XRD) can be postulated.

  11. Sorption-induced reversible oxidation of Fe(2) at the smectite/water interface under strictly anoxic conditions. A Moessbauer spectroscopy study

    Energy Technology Data Exchange (ETDEWEB)

    Gehin, A.; Charlet, L. [Laboratoire de Geophysique Interne et Tectonophysique (LGIT), Universite de Grenoble, 38 - Grenoble (France); Gehin, A. [Agence Nationale pour la Gestion des Dechets Radioactifs, ANDRA, 92 - Chatenay Malabry (France); Greneche, J.M. [Laboratoire de Physique de l' Etat Condense, UMR-CNRS 6087, 72 - Le Mans (France); Brendle, J. [Universite de Haute Alsace, Lab. des Materiaux Mineraux (LMM), 68 - Mulhouse (France); Rancourt, D.G. [Ottawa Univ., Dept. of Physics, Ontario (Canada)

    2005-07-01

    Previous studies of Fe(II) sorption onto montmorillonite have been performed with the mineral extracted from the MX80 bentonite. These studies have shown that Fe(II) can be sorbed onto clay minerals in cation exchange position. The affinity of montmorillonite for Fe(II) and Ca(II) is identical. Fe(II) may also be specifically adsorbed onto montmorillonite clay edges. Moessbauer spectroscopy confirmed the high affinity of clay surfaces for Fe(II) sorption and showed that this sorption is mainly due to a two step mechanism: Fe(II) specific adsorption, followed by oxidation of the Fe(II) sorbed. The identification of the oxidizing agent was prohibited due to the complex chemistry of the natural MX80 montmorillonite. Thus, synthetic iron-free montmorillonite was used (chemical formula: Ca{sub 0.3} (A{sub 1.4}Mg{sub 0.6}) (Si{sub 4}) O{sub 10}(OH){sub 2} ). {sup 57}Fe(II) sorption experiments were conducted in a N{sub 2} atmosphere gloves-box, in strictly anoxic conditions. Solid samples were synthesized in order to confirm the clay high affinity for Fe(II), in absence of structural oxidant, and to have a better comprehension of the sorption mechanism. Moessbauer spectra were recorded for each sample. Whereas no Fe(III) is detected in solution as pH was increased and then, a significant amount of surface sorbed Fe(III) was found to be reversibly produced, which amounts for 0-3% of total Fe in the pre-sorption edge acid region, up to 7% of total Fe when all Fe is sorbed in the neutral to alkaline pH range. From pH {approx_equal} 2 to pH {approx_equal} 7, a sorption edge plateau is observed. In this plateau, the sorbed-Fe(III)/sorbed-Fe ratio increases with pH, up to 45% at pH 7. Moessbauer spectra comparison with ferrous hydroxide, synthesized in the same redox conditions at higher pH, show that this oxidation can not be due to the trace amounts Oz in the suspension. The Moessbauer spectra components of both Fe(II) and Fe(III) appears as paramagnetic doublets: iron has

  12. Moessbauer Study of Sphero-Conical Vessels from Bolgar

    Science.gov (United States)

    Ivanova, A. G.; Nuretdinova, A. R.; Pyataev, A. V.; Valiulina, S. I.; Voronina, E. V.

    2017-05-01

    Samples of sphero-conical vessels found in mass quantities in the ancient settlement Bolgar were analyzed by Moessbauer spectroscopy. Wares with relatively low annealing temperatures medieval handicraft center.

  13. Exploring the Verwey-Type Transition in GdBaFe{sub 2}O{sub 5+w} Using {sup 57}Fe Moessbauer Spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Linden, J., E-mail: jlinden@abo.fi [Abo Akademi, Physics Department (Finland); Karen, P. [University of Oslo, Department of Chemistry (Norway); Yamauchi, H.; Karppinen, M. [Tokyo Institute of Technology, Materials and Structures Laboratory (Japan)

    2004-12-15

    {sup 57}Fe Moessbauer spectroscopy was used to study the double perovskite GdBaFe{sub 2}O{sub 5+w}, which exhibits mixing of the integer valence states of iron. The valence mixing/separation process Fe{sup 2+}+Fe{sup 3+{r_reversible}}2Fe{sup 2.5+} was investigated as a function of temperature. For nearly stoichiometric compositions of w{approx}0, a two-step Verwey-type transition is registered that separates Fe{sup 2.5+} into intermediate valence- and spin states Fe{sup 2.5-elementof} and Fe{sup 2.5+elementof} and then into the integer valences Fe{sup 2+} and Fe{sup 3+}. Both steps are accompanied by a decrease in electrical conductivity, altogether by two orders of magnitude. Seebeck measurements identify holes as dominating charge carriers, with activation energy for hopping of {approx}0.10 eV in the valence-mixed state. It is inferred that the mixing electrons are not simply delocalized over the lattice, but rather form bridges connecting pairs of adjacent Fe atoms along the c axis.

  14. Kinetic study of the thermal transformation of limonite to hematite by X-ray diffraction, {mu}-Raman and Moessbauer spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Palacios, P. R., E-mail: roggerpr@gmail.com; Bustamante, Angel [Universidad Nacional Mayor de San Marcos, Laboratorio de Ceramicos y Nanomateriales, Facultad de Ciencias Fisicas (Peru); Romero-Gomez, P.; Gonzalez, J. C. [Instituto de Ciencia de Materiales de Sevilla - CSIC - Univ. Sevilla, Grupo de Investigacion de Superficies, Intercaras y Laminas Delgadas (Spain)

    2011-11-15

    A kinetic study about the phase limonite (FeO(OH)-nH{sub 2}O) was performed through X-ray diffraction, {mu}-Raman spectroscopy and Moessbauer spectroscopy. The oxide powder sample was extracted from Taraco district, Huancane province of Puno (Peru). X-ray diffraction identified the phase goethite as the main mineralogical component, and then the sample was subjected to in-situ heat treatment in the temperature range: 100 to 500 Degree-Sign C in oxidizing (air) and inert (nitrogen) atmospheres. The goethite phase remains stable in this range: room temperature to 200 Degree-Sign C. Between 200 Degree-Sign C to 250 Degree-Sign C there is a phase transition: {alpha}-Fe{sup 3 + }O(OH) {yields} {alpha}-Fe{sub 2}O{sub 3}, i.e., from goethite to hematite phase, taking as evidence the evolution of the diffraction profiles. At 200 Degree-Sign C spectra shows the start of broadened magnetic component and it was adjusted through of a magnetic distribution giving a mean field of 38.6T and a relative area of 52.9%, which is a characteristic of goethite. Also, it is noticed the presence of a small amount of hematite with a mean field of 49.0T linked with a superparamagnetic broadened doublet of relative area of 47.1% where the domains of the particles have sizes smaller than 100 A and it is evidence the superparamagnetic limit; i.e., the superparamagnetic effect tends toward a distribution of magnetic fields. Moreover, the Raman spectra of the in-situ thermal treatment, support the transition at 290 Degree-Sign C through the transformation of characteristic bands of goethite to hematite phase at the frequency range from 200 to 1,800 cm{sup - 1}.

  15. Rare earth optogalvanic spectroscopy: preliminary results

    Energy Technology Data Exchange (ETDEWEB)

    Destro, Marcelo G.; Neri, Jose W.; Rodrigues, Nicolau A.S.; Silveira, Carlos A.B.; Riva, Rudimar [Instituto de Estudos Avancados (IEAv/EFO), Sao Jose dos Campos, SP (Brazil). Div. de Fotonica]. E-mail: destro@ieav.cta.br; Victor, Alessandro R. [Instituto Tecnologico de Aeronautica (ITA), Sao Jose dos Campos, SP (Brazil)

    2008-07-01

    The IEAv has special interest in the studies of rare earth isotope applications in laser medium and integrated optics as well as aerospace research. We are starting to work with Ytterbium, Erbium, Dysprosium and Neodymium laser selective photoionization research. This paper describes the preliminary results of emission and optogalvanic spectroscopy obtained from a Neodymium hollow cathode lamps. Furthermore these results were used to setup our laser systems to work to leads a Nd isotopes selective laser photoionization. (author)

  16. Moessbauer study of Slovak meteorites

    Energy Technology Data Exchange (ETDEWEB)

    Lipka, J.; Sitek, J.; Dekan, J., E-mail: julius.dekan@stuba.sk; Degmova, J. [Slovak University of Technology, Institute of Nuclear and Physical Engineering, Faculty of Electrical Engineering and Information Technology (Slovakia); Porubcan, V. [Comenius University, Faculty of Mathematics and Physics (Slovakia)

    2013-04-15

    {sup 57}Fe Moessbauer spectroscopy was used as an analytical tool in the investigation of iron containing compounds of two meteorites (Rumanova and Kosice) out of total of six which had fallen on Slovak territory. In the magnetic fraction of the iron bearing compounds in the Rumanova meteorite, maghemite, troilite and Fe-Ni alloy were identified. In the non-magnetic fraction silicate phases were found, such as olivine and pyroxene. The paramagnetic component containing Fe{sup 3 + } ions corresponds probably to small superparamagnetic particles. The Kosice meteorite was found near the town of Kosice in February 2010. Its magnetic fraction consists of a Fe-Ni alloy with the Moessbauer parameters of the magnetic field corresponding to kamacite {alpha}-Fe(Ni, Co) and troilite. The non-magnetic part consists of Fe{sup 2 + } phases such as olivine and pyroxene and traces of a Fe{sup 3 + } phase. The main difference between these meteorites is their iron oxide content. These kinds of analyses can bring important knowledge about phases and compounds formed in extraterrestrial conditions, which have other features than their terrestrial analogues.

  17. Characterization of clays found in soils of the indian territories in Rio Grande do Sul State by using the {sup 57} Fe Moessbauer spectroscopy; Caracterizacao de argilas encontradas em solos de terras indigenas do RS com o auxilio da espectroscopia Moessbauer de {sup 57} Fe

    Energy Technology Data Exchange (ETDEWEB)

    Perez, C.A.S.; Gobbi, D.; Marcos, J.L.N. [Universidade de Passo Fundo, RS (Brazil), Inst. de Ciencias Exatas e Geociencias; Paduani, C. [Santa Catarina Univ., Florianopolis, SC (Brazil). Dept. de Fisica; Ardisson, J.D. [Centro de Desenvolvimento da Tecnologia Nuclear (CDTN), Belo Horizonte, MG (Brazil)

    2004-06-01

    Clay samples collected from soils of indian territories of the middle plateau in Rio Grande do Sul were analyzed with the aim to obtain characterization data and technical parameters for their potential use as raw material for ceramic products. The mineralogical study in samples by using the X-ray diffraction technique demonstrated that the predominant clay mineral is kaolinite. Others minerals as quartz and rutile also are present in small amounts. Chemical analysis shows low percentages for oxides of Mg, Mn, K, Na, Ca, Cu and Zn (overall percentages smaller than 0.97%). The samples also were analyzed with the {sup 57} Fe Moessbauer spectroscopy. The Moessbauer spectra at room temperature confirm the presence of the mineral kaolinite. At 77 K they reveal the existence of the minerals goethite and hematite as ultrafine magnetic particles in a superparamagnetic state. The physical tests performed in the samples show that these soils are very fine material and present appropriate granulometric characteristics and plasticity, which can be taken in advantage for the production of materials for construction or production of ornamental artifacts. (author)

  18. Development of a highly efficient conversion electron Moessbauer spectroscopy (CEMS) detector for low temperature (<20 K) measurements and tests on Fe / (Eu{sub x}Pb{sub 1-x})Te bilayers; Desenvolvimento de um detector de alta eficiencia para espectroscopia Moessbauer de eletrons de conversao (CEMS) a baixas temperaturas (<20K) e testes em bicamadas Fe / (Eu{sub x}Pb{sub 1-x})Te

    Energy Technology Data Exchange (ETDEWEB)

    Pombo, Carlos Jose da Silva Matos

    2006-07-01

    The {sup 57}Fe Moessbauer spectroscopy is a nuclear, non-destructive technique used for the investigation of structural, magnetic and hyperfine properties of several materials. It is a powerful tool in characterizing materials in physics, metallurgy, geology and biology field areas, especially magnetic materials, alloys and minerals containing Fe. Lately, the Conversion Electron Moessbauer Spectroscopy (CEMS) is widely used in making studies on ultra-thin magnetic films, as well as other nanostructured materials. In case of magnetic nanostructures, low temperature (LT) studies are especially important due to the possibility of dealing with superparamagnetic effects. In this work it was developed a CEMS measurement system for low temperatures (<20 K) based on a solid-state electron multiplier (Channeltron{sup R}) and an optical cryostat (Model SVT-400, Janis Research Co, USA), from which the project was originally conceived at the Applied Physics / Moessbauer spectroscopy Department from University of Duisburg-Essen, Germany. The LT-CEMS system was fully built, tested and successfully applied in a preliminary characterization of Fe/(Eu{sub x}Pb{sub 1-x})Te(111) bilayers with use of a 15 angstrom, {sup 57} Fe probe layer, with reasonable results at sample temperatures as low as 8 K. (author)

  19. Study on the spin crossover transition and glass transition for Fe(II) complex film, [Fe(II)(H-triazole){sub 3}]-Nafion, by means of Moessbauer spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Nakamoto, Akio; Kamebuchi, Hajime, E-mail: cc106909@mail.ecc.u-tokyo.ac.jp [University of Tokyo, Graduate School of Arts and Sciences (Japan); Enomoto, Masaya [Tokyo University of Science, Department of Chemistry, Faculty of Science Division I (Japan); Kojima, Norimichi [University of Tokyo, Graduate School of Arts and Sciences (Japan)

    2012-03-15

    [Fe(II)(H-trz){sub 3}]-Nafion (trz = triazole) is a transparent spin crossover complex film, where the spin crossover transition between the low-spin (S = 0) and the high-spin (S = 2) states takes place between 225 K and 300 K. In this film, two doublets corresponding to the low-spin and high-spin states were observed in the {sup 57}Fe Moessbauer spectra, reflecting the spin crossover transition. From the analysis of {sup 57}Fe Moessbauer spectra, the Debye temperatures of the low-spin and high-spin sites were estimated at 185 K and 176 K, respectively, in the temperature range between 10 K and 150 K. In this film, the total intensity of the Moessbauer spectra corresponding to the low-spin and high-spin sites drastically decreases above 200 K, reflecting the glass transition of Nafion, where the lattice vibration of [Fe(H-trz){sub 3}]{sub n}{sup 2n+} is softened just as in solution due to micro-Brown motion of the segment of Nafion polymer membrane.

  20. Assessment of the optimum degree of Sr{sub 3}Fe{sub 2}MoO{sub 9} electron-doping through oxygen removal: An X-ray powder diffraction and {sup 57}Fe Moessbauer spectroscopy study

    Energy Technology Data Exchange (ETDEWEB)

    Lopez, Carlos A.; Viola, Maria del C. [Area de Quimica General e Inorganica, Departamento de Quimica, Facultad de Quimica, Bioquimica y Farmacia, Universidad Nacional de San Luis, Chacabuco y Pedernera, 5700 San Luis (Argentina); Pedregosa, Jose C., E-mail: jpedreg@unsl.edu.ar [Area de Quimica General e Inorganica, Departamento de Quimica, Facultad de Quimica, Bioquimica y Farmacia, Universidad Nacional de San Luis, Chacabuco y Pedernera, 5700 San Luis (Argentina); Mercader, Roberto C., E-mail: mercader@fisica.unlp.edu.ar [Departamento de Fisica, IFLP-CONICET, Facultad de Ciencias Exactas, Universidad Nacional de La Plata, C.C. 67, 1900 La Plata (Argentina)

    2010-10-15

    We describe the preparation and structural characterization by X-ray powder diffraction (XRPD) and Moessbauer spectroscopy of three electron-doped perovskites Sr{sub 3}Fe{sub 2}MoO{sub 9-{delta}} with Fe/Mo = 2 obtained from Sr{sub 3}Fe{sub 2}MoO{sub 9}. The compounds were synthesized by topotactic reduction with H{sub 2}/N{sub 2} (5/95) at 600, 700 and 800 {sup o}C. Above 800 {sup o}C the Fe/Mo ratio changes from Fe/Mo = 2-1 < Fe/Mo < 2. The structural refinements of the XRPD data for the reduced perovskites were carried out by the Rietveld profile analysis method. The crystal structure of these phases is cubic, space group Fm3-bar m, with cationic disorder at the two different B sites that can be populated in variable proportions by the Fe atoms. The Moessbauer spectra allowed determining the evolution of the different species formed after the treatments at different temperatures and confirm that Fe ions in the samples reduced at 600, 700 and 800 {sup o}C are only in the high-spin Fe{sup 3+} electronic state.

  1. Synthesis, magnetic properties and Moessbauer spectroscopy for the pyrochlore family Bi{sub 2}BB Prime O{sub 7} with B=Cr and Fe and B Prime =Nb, Ta and Sb

    Energy Technology Data Exchange (ETDEWEB)

    Blanco, Maria C. [INFIQC (CONICET), Dpto. de Fisicoquimica, Fac. de Ciencias Quimicas, U.N.C., Cordoba (X5000HUA) (Argentina); Franco, Diego G. [INFIQC (CONICET), Dpto. de Fisicoquimica, Fac. de Ciencias Quimicas, U.N.C., Cordoba (X5000HUA) (Argentina); Centro Atomico Bariloche - CNEA, Av. E. Bustillo 9500, S.C. de Bariloche (8500), R.N. (Argentina); Jalit, Yamile; Pannunzio Miner, Elisa V. [INFIQC (CONICET), Dpto. de Fisicoquimica, Fac. de Ciencias Quimicas, U.N.C., Cordoba (X5000HUA) (Argentina); Berndt, Graciele; Paesano, Andrea [Departamento de Fisica, Universidade Estadual de Maringa, Parana (Brazil); Nieva, Gladys [Centro Atomico Bariloche - CNEA, Av. E. Bustillo 9500, S.C. de Bariloche (8500), R.N. (Argentina); Carbonio, Raul E., E-mail: carbonio@mail.fcq.unc.edu.ar [INFIQC (CONICET), Dpto. de Fisicoquimica, Fac. de Ciencias Quimicas, U.N.C., Cordoba (X5000HUA) (Argentina)

    2012-08-15

    The samples Bi{sub 2}BB Prime O{sub 7}, with B=Cr and Fe and B Prime =Nb, Ta and Sb were prepared by solid state method. The crystallographic structure was investigated on the basis of X-ray powder diffraction data. Rietveld refinements show that the crystal structure is cubic, space group Fd-3m. The Bi{sup 3+} cation on the eight-coordinate pyrochlore A-site shows displacive disorder, as a consequence of its lone pair electron configuration. There is also a considerable A-site disorder shown by Rietveld Analysis and confirmed in the case of the iron containing samples with Moessbauer spectroscopy. The magnetic measurements show paramagnetic behavior at all temperatures for the Cr oxides. The Fe pyrochlores show antiferromagnetic order around 10 K.

  2. Thermal treatment of the Fe{sub 78} Si{sub 9} B{sub 13} alloy and the analysis of it magnetic properties through Moessbauer spectroscopy and Positronium annihilation; Tratamiento termico de la aleacion Fe{sub 78} Si{sub 9} B{sub 13} y el analisis de sus propiedades magneticas mediante Espectroscopia de Moessbauer y Aniquilacion de positronio

    Energy Technology Data Exchange (ETDEWEB)

    Lopez M, A

    2005-07-01

    The present work is divided in five chapters. In the first one a general vision of the amorphous alloys is given from antecedents, structure, obtaining methods, properties and problems that at the moment, focusing us in a certain moment to the iron base alloys and the anomalous problem of hardness that it presents the alloy Fe{sub 78}Si{sub 9}B{sub 13} like previously mention us. The second chapter tries on the basic theory of the techniques of Moessbauer spectroscopy and Positron Annihilation spectroscopy, used for the characterization of our alloy as well as the complementary technique of X-ray diffraction (XRD) to observe that the amorphous phase was even studying. The third chapter describes the experimental conditions that were used to study the alloy Fe{sub 78}Si{sub 9}B{sub 13} in each one of their thermal treatments. In the fourth chapter the obtained results and their discussion are presented. In the fifth chapter the conclusions to which were arrived after analyzing the results are presented. (Author)

  3. Characterization of Zn-bearing chlorite by Moessbauer and infrared spectroscopy - occurrence associated to the Pb-Zn-Ag deposits of Canoas, PR, Brazil; Caracterizacao de clorita portadora de Zn por espectroscopia Moessbauer e espectroscopia infravermelho - uma ocorrencia associada ao deposito de Pb-Zn-Ag de Canoas, PR, Brasil

    Energy Technology Data Exchange (ETDEWEB)

    Imbernon, Rosely Aparecida Liguori [Universidade de Sao Paulo (EACH/USP), SP (Brazil). Escola de Artes, Ciencias e Humanidades; Blot, Alain [Institut de Recherche pour le Developpement (IRD), Paris (France); Pereira, Vitor Paulo [Universidade Federal do Rio Grande do Sul (UFRGS), Porto Alegre, RS (Brazil). Inst. de Geociencias; Franco, Daniel Ribeiro, E-mail: imbernon@usp.br, E-mail: brotalain@free.fr, E-mail: vitor.pereira@ufrgs.br, E-mail: drfranco@on.br [Observatorio Nacional do Brasil (COGE/ON), Rio de Janeiro, RJ (Brazil). Coordenacao de Geofisica

    2011-06-15

    In order to provide new insights on mineralogical aspects of geochemical mapping/natural processes related to the chlorite formation (e.g. crystallochemistry and mechanisms of formation of these materials, which has been applied in different studies of environmental profiles), we investigated chlorite samples associated to the Pb-Zn-Ag sulfide ore from Canoas 1 deposit (Vale do Ribeira, state of Parana, Brazil). By means of Moessbauer (MS) and infrared (IV) spectroscopy, we addressed some issues as those related to the chloritization processes, as well as how Zn would be incorporated into its crystalline structure. Results carried out by ME and IV spectroscopy clearly pointed out for a chlorite occurrence, which in fact incorporates Zn into its structure and also alters the structural patterns for this mineral. Moreover, ME data sets indicated the presence of Fe which is located only in octahedral sites, in trans-configuration, and the Zn emplacement by the chloritization process also occurs in the brucite layer. (author)

  4. Moessbauer investigation of Au/Fe alloys with giant magnetoresistence properties

    Energy Technology Data Exchange (ETDEWEB)

    Albanese, G.; Deriu, A. E-mail: antonio.deriu@fis.unipr.it; Moya, J.; Angeli, E.; Bisero, D.; Da Re, A.; Ronconi, F.; Spizzo, F.; Vavassori, P.; Baricco, M.; Bosco, E

    2004-05-01

    Rapidly quenched ribbon samples and sputtered granular films of AuFe alloys with giant magnetoresistance behaviour were investigated by Moessbauer spectroscopy. The structural and magnetic characteristics of the two kinds of samples are discussed and compared.

  5. The stannides RE{sub 3}Au{sub 6}Sn{sub 5} (RE = La, Ce, Pr, Nd, Sm). Synthesis, structure, magnetic properties and {sup 119}Sn Moessbauer spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Fickenscher, Thomas; Rodewald, Ute C.; Niehaus, Oliver; Gerke, Birgit; Poettgen, Rainer [Muenster Univ. (Germany). Inst. fuer Anorganische und Analytische Chemie; Haverkamp, Sandra; Eckert, Hellmut [Muenster Univ. (Germany). Inst. fuer Physikalische Chemie

    2015-07-01

    The Ce{sub 3}Pd{sub 6}Sb{sub 5}-type rare earth stannides RE{sub 3}Au{sub 6}Sn{sub 5} (RE = La, Ce, Pr, Nd, Sm) were synthesized by arc-melting of the elements and subsequent annealing in open tantalum crucibles within sealed evacuated silica ampoules. The polycrystalline samples were studied by powder X-ray diffraction. The structures of three crystals were refined from single crystal X-ray diffractometer data: Pmmn, a = 1360.3(9), b = 455.9(2), c = 1023.6(4) pm, wR2 = 0.0275, 1069 F{sup 2} values, 48 variables for Ce{sub 3}Au{sub 6}Sn{sub 5}, a = 1352.4(4), b = 455.1(1), c = 1023.7(3) pm, wR2 = 0.0367, 1160 F{sup 2} values, 48 variables for Nd{sub 3}Au{sub 6}Sn{sub 5}, and a = 1339.8(2), b = 452.80(7), c = 1012.4(2) pm, wR2 = 0.1204, 1040 F{sup 2} values, 49 variables for Sm{sub 3}Au{sub 5.59(2)}Sn{sub 5.41(2)}. One of the gold sites of the samarium compound shows a significant degree of Au/Sn mixing. The RE{sub 3}Au{sub 6}Sn{sub 5} structures are composed of three-dimensional [Au{sub 6}Sn{sub 5}] polyanionic networks with the two crystallographically independent rare earth atoms in larger cages, i.e., RE1 rate at Au{sub 10}Sn{sub 6} and RE2 rate at Au{sub 8}Sn{sub 8}. The [Au{sub 6}Sn{sub 5}] network is stabilized by Au-Sn (266-320 pm), Au-Au (284-301 pm) as well as Sn-Sn (320 pm; distances given for the cerium compound) interactions. Temperature-dependent magnetic susceptibility measurements reveal an antiferromagnetic ordering only for Sm{sub 3}Au{sub 6}Sn{sub 5}, while the other compounds exhibit Curie-Weiss paramagnetism. {sup 119}Sn Moessbauer spectroscopy shows resonances in the typical range for intermetallic tin compounds where tin takes part in the polyanionic network [isomer shifts between 1.73(1) and 2.28(1) mm . s{sup -1}]. With the help of theoretical electric field gradient calculations using the WIEN2k code it was possible to resolve the spectroscopic contributions of all three crystallographically independent atomic tin sites in the {sup 119}Sn

  6. Moessbauer study of EUROFER and VVER steel reactor materials

    Energy Technology Data Exchange (ETDEWEB)

    Kuzmann, E., E-mail: kuzmann@ludens.elte.hu [Eoetvoes University, Laboratory of Nuclear Chemistry, Institute of Chemistry (Hungary); Horvath, A. [Hungarian Academy of Sciences, Centre for Energy Research (Hungary); Alves, L.; Silva, J. F.; Gomes, U.; Souza, C. [Universidade Federal do Rio Grande do Norte (University) (Brazil); Homonnay, Z. [Eoetvoes University, Laboratory of Nuclear Chemistry, Institute of Chemistry (Hungary)

    2013-04-15

    {sup 57}Fe Moessbauer spectroscopy and X-ray diffractometry were used to study EUROFER or VVER ferritic reactor steels mechanically alloyed with TaC or NbC. Significant changes were found in the Moessbauer spectra and in the corresponding hyperfine field distributions between the ball milled pure steel and that alloyed with TaC or NbC. Spectral differences were also found in the case of use of same carbides with different origin, too. The observed spectral changes as an effect of ball milling of the reactor material steels with carbides can be associated with change in short range order of the constituents of steel.

  7. Moessbauer study of function of magnesium in iron oxide catalysts

    Institute of Scientific and Technical Information of China (English)

    YangJie-Xin; MaoLian-Sheng; 等

    1997-01-01

    Moessbauer spectroscopy has been utilized for studying the action of Mg element in iron oxide catalysts used for the dehydrogenation of ethylbenzene to sytrene.The experimental results show that the presence of opportune amount of Mg can enhance the stability and dispersion of catalysts,i.e.Mg is an sueful structure promoter in this kind of catalysts.

  8. Moessbauer spectroscopic study of meteorites recovered on Antarctica

    Energy Technology Data Exchange (ETDEWEB)

    Endo, K. [Showa Coll. of Pharmaceutical Sci., Tokyo (Japan); Hirunuma, R. [Showa Coll. of Pharmaceutical Sci., Tokyo (Japan); Shinonaga, T. [Dept. of Chemistry, Tokyo Metropolitan Univ. (Japan); Ebihara, M. [Dept. of Chemistry, Tokyo Metropolitan Univ. (Japan); Nakahara, H. [Dept. of Chemistry, Tokyo Metropolitan Univ. (Japan)

    1994-11-01

    The chemical states of iron in sixteen Antarctic meteorites belonging to H-group chondrites were studied by means of Moessbauer spectroscopy. An Fe-Ni alloy, troilite, paramagnetic Fe(III), and two kinds of paramagnetic Fe(II) were observed in each meteorite. The Moessbauer parameters indicated that the Fe(II) components can be assigned to olivine and some pyroxenes. The relative area intensities of Fe(III) in the chondrites correlated positively with iodine content, which was determined by radiochemical neutron activation analysis, and those of two Fe(II)-species correlated negatively with the content. On the basis of the data on the halogen and the Moessbauer spectrocopy, the terrestrial contamination on Antarctic meteorites is discussed. (orig.)

  9. The history of the Moessbauer effect

    CERN Document Server

    Miglierini, M

    2003-01-01

    The background of the discovery of the Moessbauer effect and the development of Moessbauer spectrometry as an analytical technique are highlighted. The basic principles and instrumentation, application fields, and trends of future progress and outlined and discussed

  10. Spectroscopy of near-Earth asteroids

    DEFF Research Database (Denmark)

    Michelsen, René; Nathues, Andreas; Lagerkvist, Claes-Ingvar

    2006-01-01

    We present spectra and taxonomic classifications of 12 Near-Earth Asteroids (NEAs) and 2 inner Main Belt asteroids. The observations were carried out with the ESO 3.5 m NTT and the Danish 1.54 m telescope at La Silla, Chile. Eleven of the investigated NEAs belong to the S class while only one C......-type has been identified. Two NEAs were observed at phase angles larger than 60 degrees introducing significant phase reddening. In order to allow for comparisons between spectra of asteroids observed at different phase angles we make attempts to correct for this effect. However, it turned out...

  11. Spectroscopy of near-Earth asteroids

    DEFF Research Database (Denmark)

    Michelsen, René; Nathues, Andreas; Lagerkvist, Claes-Ingvar

    2006-01-01

    We present spectra and taxonomic classifications of 12 Near-Earth Asteroids (NEAs) and 2 inner Main Belt asteroids. The observations were carried out with the ESO 3.5 m NTT and the Danish 1.54 m telescope at La Silla, Chile. Eleven of the investigated NEAs belong to the S class while only one C......-type has been identified. Two NEAs were observed at phase angles larger than 60 degrees introducing significant phase reddening. In order to allow for comparisons between spectra of asteroids observed at different phase angles we make attempts to correct for this effect. However, it turned out...

  12. Mineralogy of the clay fraction of soils from the moray cusco archaeological site: a study by energy dispersive X-ray fluorescence, X-ray diffractometry and Moessbauer spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Ceron Loayza, Maria L., E-mail: malucelo@hotmail.com; Bravo Cabrejos, Jorge A.; Mejia Santillan, Mirian E. [Universidad Nacional Mayor de San Marcos, Laboratorio de Analisis de Suelos, Laboratorio de Espectroscopia Moessbauer, Facultad de Ciencias Fisicas (Peru)

    2011-11-15

    The purpose of this work is to report the advances in the elemental and structural characterization of the clay fraction of soils from the terraces of the Moray Archaeological site, located 38 km north of the city of Cusco, Cusco Region. One sample was collected from each of the twelve terraces of this site and its clay fraction was separated by sedimentation. Previously the pH of the raw samples was measured resulting that all of the samples were from alkaline to strongly alkaline. Energy dispersive X-ray fluorescence (EDXRF) was used for the elemental characterization, and X-ray diffractometry (XRD) and transmission Moessbauer spectroscopy (TMS), using the {gamma} 14.4 keV nuclear resonance transition in {sup 57}Fe, were used for the structural characterization of the clays and clay minerals present in each sample. The EDXRF analyses of all the samples show the presence of relatively high concentrations of sulfur in some of the samples and relatively high concentrations of calcium in all of the samples, which may be related to the high alkalinity of the samples. By XRD it is observed the presence of quartz, calcite, gypsum, cronstedtite, 2:1 phyllosilicates, and iron oxides. The mineralogical analysis of Fe by TMS shows that it is present in the form of hematite and occupying Fe{sup 2 + } and Fe{sup 3 + } sites in phyllosilicates, cronstedtite, and other minerals not yet identified.

  13. Aging effect in CaLaBa{l_brace}Cu{sub 1 - x}Fe{sub x}{r_brace}{sub 3}O{sub 7 - {delta}} with 0 {<=} x {<=} 0.07 studied by Moessbauer spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Bustamante, Angel, E-mail: angelbd1@gmail.com [Universidad Nacional Mayor de San Marcos, Laboratorio de Ceramicos y Nanomateriales, Facultad de Ciencias Fisicas (Peru); Santos Valladares, Luis De Los, E-mail: ld301@cam.ac.uk [University of Cambridge, Cavendish Laboratory (United Kingdom); Flores, Jesus [Universidad Nacional Mayor de San Marcos, Laboratorio de Ceramicos y Nanomateriales, Facultad de Ciencias Fisicas (Peru); Barnes, Crispin H. W. [University of Cambridge, Cavendish Laboratory (United Kingdom); Majima, Yutaka [Tokyo Institute of Technology, Materials and Structures Laboratory (Japan)

    2011-11-15

    In this work, we study the long-term aging effect caused by Fe atoms in the superconductor CaLaBa{l_brace}Cu{sub 1 - x}Fe{sub x}{r_brace}{sub 3}O{sub 7 - {delta}} with 0 {<=} x {<=} 0.07. XRD confirms that this system has a YBCO-like structure. The critical temperature (T{sub c}) is strongly affected by aging and depends on the amount of Fe in the structure. Room temperature Moessbauer spectroscopy reveals the presence of the typical species A, B-B Prime , C and new species E Prime and F. Interestingly; A, which corresponds to the Fe{sup 3 + } atom located in the Cu(1) of the chains with spin S{sub z} = 3/2, shows a drastic reduction which means migration to the species B, B Prime and C. Species B and B Prime correspond to the Fe{sup 3 + } in the Cu(2) site forming planar quasi-octahedral and planar square pyramidal, while the C specie is a square pyramidal with O(5) respectively (spin S{sub z} = 3/2 in all these cases). Aging causes loss of superconductivity in the samples with 5 and 7% of iron content.

  14. Cation distribution in Ba{sub 2}(Fe,W{sub 0.5}Mo{sub 0.5}){sub 2}O{sub 6} double-perovskites: A combined synchrotron and neutron diffraction, magnetization and Moessbauer spectroscopy study

    Energy Technology Data Exchange (ETDEWEB)

    Rammeh, N. [Laboratoire de Physique des Materiaux, Faculte des Sciences de Sfax, BP 1171, 3000 Sfax (Tunisia); Institute for Materials Science, University of Technology, D-64287 Darmstadt (Germany); Ehrenberg, H. [Institute for Materials Science, University of Technology, D-64287 Darmstadt (Germany); Ritter, C. [Institut Laue Langevin, BP 156, F-38042 Grenoble Cedex 9 (France); Fuess, H. [Institute for Materials Science, University of Technology, D-64287 Darmstadt (Germany); Cheikhrouhou, A. [Laboratoire de Physique des Materiaux, Faculte des Sciences de Sfax, BP 1171, 3000 Sfax (Tunisia)], E-mail: abdcheikhrouhou@yahoo.fr

    2009-03-20

    The crystallographic and magnetic structures of polycrystalline Ba{sub 2}(Fe,W){sub 2}O{sub 6} and Ba{sub 2}(Fe,W{sub 0.5}Mo{sub 0.5}){sub 2}O{sub 6} double-perovskites have been investigated by X-ray and neutron powder diffraction (NPD), magnetization and Moessbauer spectroscopy. The samples were synthesized by conventional solid-state reaction at temperatures about 1273 K. The compounds crystallize in the cubic structure with space group Fm3-barm. The magnetic structures were determined by neutron powder diffraction between 5 K and 310 K. Evidence for an antiferromagnetic behavior has been observed for Ba{sub 2}(Fe,W){sub 2}O{sub 6} with T{sub N} = 24.7 K and a two-phase separation for Ba{sub 2}(Fe,W{sub 0.5}Mo{sub 0.5}){sub 2}O{sub 6} into an antiferromagnetic structure of the W-type with T{sub N} = 24.7 K and the ferromagnetic Mo-type with T{sub C} = 270 K.

  15. Effect of particle size and alloying with different metals on {sup 57}Fe Moessbauer spectra

    Energy Technology Data Exchange (ETDEWEB)

    Nazir, Rabia; Mazhar, Muhammad, E-mail: mazhar42pk@yahoo.com [Quaid-i-Azam University, Department of Chemistry (Pakistan); Siddique, Muhammad [PINSTECH, Physics Division (Pakistan); Hussain, S. Tajammul [Quaid-i-Azam University, Department of Chemistry (Pakistan)

    2009-02-15

    Iron nanoparticles of various sizes have been synthesized using the chemical route which involves the preparation of iron bipyridine complexes in presence of different capping agents followed by thermal decomposition at 450 deg. C in inert atmosphere. The bimetallic nanoalloys of Fe with Mg and Pd have also been prepared by following the same route. The resulting nanoparticles have been characterized by EDX-RF, XRD, AFM and {sup 57}Fe Moessbauer spectroscopy. The appearance of quadrupole doublets in the Moessbauer spectra of Fe nanoparticles indicates the absence of magnetic interaction and variation in parameters is due to the varying particle size. The Moessbauer spectrum of Fe-Mg{sub 2} bimetallic nanoalloy shows two doublets indicating the presence of superparamagnetism. The two doublets can be attributed to change in s-electron density of iron resulting from its two neighboring magnesium atoms. Fe-Pd nanoalloy Moessbauer spectrum is characterized by having a superparamagnetic doublet and a ferromagnetic sextet.

  16. Optical Frequency Comb Spectroscopy of Rare Earth Atoms

    Science.gov (United States)

    Swiatlowski, Jerlyn; Palm, Christopher; Joshi, Trinity; Montcrieffe, Caitlin; Jackson Kimball, Derek

    2013-05-01

    We discuss progress in our experimental program to employ optical-frequency-comb-based spectroscopy to understand the complex spectra of rare-earth atoms. We plan to carry out systematic measurements of atomic transitions in rare-earth atoms to elucidate the energy level structure and term assignment and determine presently unknown atomic state parameters. This spectroscopic information is important in view of the increasing interest in rare-earth atoms for atomic frequency standards, in astrophysical investigations of chemically peculiar stars, and in tests of fundamental physics (tests of parity and time-reversal invariance, searches for time variation of fundamental constants, etc.). We are presently studying the use of hollow cathode lamps as atomic sources for two-photon frequency comb spectroscopy. Supported by the National Science Foundation under grant PHY-0958749.

  17. Moessbauer spectroscopic analysis of the BaNbFe based compound; Analise por espectroscopia Moessbauer do composto a base de BaNbFe

    Energy Technology Data Exchange (ETDEWEB)

    Silva, Manoel Ribeiro da; Araujo, Fabiana F. de; Gontijo, Marcelo R.F.; Polegato, Paulo H. [Universidade Federal de Itajuba (UNIFEI), MG (Brazil). Dept. de Fisica e Quimica], e-mail: mrsilva@unifei.edu.br

    2008-07-01

    This work presents the synthesis and the results resulting from the application of Moessbauer spectroscopy for the investigation of the compound containing BaNb{sub x}Fe{sub 2-x}O{sub 4}. The synthesis used the chemical compounds Fe{sub 2}, Nb{sub 2}O{sub 3} and BaCO{sub 3}. The Moessbauer spectroscopy shows that the central doublets are characteristically of Fe{sup 3+} in the paramagnetic mineral structures or Fe{sup 2+} oxides in the superparamagnetic state. The studied material is a strong candidate for the application studies of superparamagnetic materials.

  18. Spectroscopy of the earth's atmosphere and interstellar medium

    CERN Document Server

    Rao, KN

    1992-01-01

    Spectroscopy of the Earth's Atmosphere and Interstellar Medium focuses on the characteristics of the electromagnetic spectrum of the Earth's atmosphere in the far-infrared and microwave regions. It discusses the modes of observation in field measurements and reviews the two techniques used in the spectral region. Organized into six chapters, this volume begins with an overview of the effect of water-vapor absorption, followed by a discussion on the two frequently used method for deriving atmospheric parameters from high-resolution infrared atmospheric spectra, namely, the equivalent width

  19. LACAME 2006: Latin American conference on the applications of the Moessbauer effects. Program and Abstract Book

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    2006-07-01

    Theoretical and experimental papers are present in these proceedings on the following subjects: Moessbauer effects and spectroscopy, minerals, structural chemical analysis, crustal structure, ion oxides, hyperfine structure, geology, catalysts, transmission and absorption spectroscopies, materials, crystal and hyperfine structures, stereochemistry and geological materials.

  20. A Moessbauer effect study of the Soledade meteorite

    Energy Technology Data Exchange (ETDEWEB)

    Paduani, C. [Santa Catarina Univ., Florianopolis, SC (Brazil). Dept. de Fisica; Samudio Perez, C.A. [Universidade de Passo Fundo, RS (Brazil). Inst. de Ciencias Exatas; Ardisson, J.D. [Centro de Desenvolvimento da Tecnologia Nuclear (CDTN), Belo Horizonte, MG (Brazil)

    2005-09-15

    We performed a Moessbauer spectroscopy study of the iron meteorite Soledade. This meteorite, which consists of a metallic matrix, is an octahedrite with polycrystalline troilite, cohenite, schreibersite and rhabdites as major constituents. A chemical analysis indicates 6.78 % Ni, 0.46% Co, besides traces of Cu, Cr, Ga, Ge, As, Sb, W, Re, Ir and Au. No traces of silicates have been found and no oxygen was detected. Iron is appearing in the austenitic phase and alloyed with nickel. An analysis of the Moessbauer spectra at room temperature indicates that the Fe-Ni phase is homogeneously distributed in the matrix, although variations in the composition between different regions are observed. (author)

  1. Multi-Wavelength Spectroscopy of Super-Earth Atmospheres

    Science.gov (United States)

    Dragomir, Diana; Benneke, Björn; Crossfield, Ian; Lothringer, Joshua; Knutson, Heather

    2017-01-01

    The Kepler mission has revealed that super-Earths (planets with radii between 1 and 4 R_Earth) are the most common class of planets in the Galaxy, though none are known in our own Solar System. These planets can theoretically have a wide range of compositions which we are just beginning to explore observationally. While studies based on Kepler data have revolutionized many areas of exoplanet research, the relative faintness of most of the host stars in the Kepler field means that atmospheric characterization of these super-Earths with currently available instruments is extremely challenging. However, a handful of transiting super-Earths are within reach of existing facilities. We have pointed both the HST and Spitzer toward these systems in an effort to paint a thorough picture of their atmospheres. Our transmission spectroscopy observations explore the transition region between terrestrial planets and miniature gas giants, and contribute to distinguishing between low-density hydrogen-dominated atmospheres and compact high-metallicity atmospheres. Transmission spectroscopy over a wide wavelength range is also essential to understanding the properties and effects of clouds in these atmospheres. The results of this program will inform the direction to be taken by future multi-wavelength studies of these worlds, in particular those enabled when the HST joins forces with the upcoming JWST.

  2. Moessbauer optics of synchrotron radiation at an isotope interface

    CERN Document Server

    Belyakov, V A

    2000-01-01

    Coherent inelastic Moessbauer scattering (CIMS) of synchrotron radiation (SR) at an isotope interface (plane interface between two regions differing only in the concentration of the Moessbauer isotope) is investigated theoretically. Main attention is paid to the CIMS component resulting from SR quanta absorption by Moessbauer nuclei accompanied by creation or annihilation of the phonons in sample and following recoilless reemission of Moessbauer quanta.

  3. Early Pottery Making in Northern Coastal Peru. Part I: Moessbauer Study of Clays

    Energy Technology Data Exchange (ETDEWEB)

    Shimada, I. [Southern Illinois University (United States); Haeusler, W.; Hutzelmann, T.; Wagner, U. [Technische Universitaet Muenchen, Physik-Department E15 (Germany)

    2003-09-15

    We report on an investigation of several ancient clays which were used for pottery making in northern coastal Peru at a kiln site from the Formative period (ca. 2000-800 BC) in the Poma Canal and at a Middle Sican pottery workshop in use between ca. AD 950 and 1050 at Huaca Sialupe in the lower La Leche valley. Neutron activation analysis, {sup 57}Fe Moessbauer spectroscopy and X-ray diffraction were used for the characterisation of the clays. The changes that occur in iron-bearing compounds in the clays depending on the kiln atmosphere and on the maximum firing temperature were studied by Moessbauer spectroscopy and X-ray diffraction. Laboratory firing series under varying controlled conditions were performed to obtain a basic understanding of the different reactions taking place in the clays during firing. The results can be used as models in the interpretation of the Moessbauer spectra observed in ancient ceramics from the same context.

  4. Emission Spectroscopy of the Super-Earth 55 Cnc e

    Science.gov (United States)

    Dragomir, Diana; Bean, Jacob; Kreidberg, Laura; Stevenson, Kevin B.; Line, Michael R.

    2017-01-01

    Recent surveys have revealed an extraordinary and unexplained diversity of low-mass exoplanets. The main frontier for constraining the nature and origins of these planets is atmospheric characterization to reveal their detailed physical properties. Previous spectroscopic observations of small exoplanets have been focused on transmission measurements, but these studies are often limited by clouds. We are turning small exoplanet characterization in a new direction with multi-wavelength observations (Warm Spitzer and HST WFC3) of the dayside of 55 Cnc e, a quintessential super-Earth in a tight orbit and transiting a nearby star. We will present the first dayside emission spectrum of a super-Earth, which we use to distinguish between different atmospheric compositions and constrain the vertical temperature structure of the atmosphere. Our results for 55 Cnc e will guide JWST emission spectroscopy of a much larger sample of small close-in transiting exoplanets.

  5. Application of Mössbauer Spectroscopy in Earth Sciences

    Science.gov (United States)

    Vandenberghe, Robert E.; De Grave, Eddy

    Iron being the fourth most abundant element in the earth crust, 57Fe Mössbauer spectroscopy has become a suitable additional technique for the characterization of all kind of soil materials and minerals. However, for that purpose a good knowledge of the spectral behavior of the various minerals is indispensable. In this chapter a review of the most important soil materials and rock-forming minerals is presented. It starts with a description of the Mössbauer spectroscopic features of the iron oxides and hydroxides, which are essentially present in soils and sediments. Further, the Mössbauer spectra from sulfides, sulfates and carbonates are briefly considered. Finally, the Mössbauer features of the typical and most common silicate and phosphate minerals are reported. The chapter ends with some typical examples, illustrating the use and power of Mössbauer spectroscopy in the characterization of minerals.

  6. In Situ Resource Utilization (ISRU) on the Moon: Moessbauer Spectroscopy as a Process Monitor for Oxygen Production. Results from a Field Test on Mauna Kea Volcano, Hawaii

    Science.gov (United States)

    Morris, R.V.; Schroder, C.; Graff, T.G.; Sanders, G.B.; Lee, K.A.; Simon, T.M.; Larson, W.E.; Quinn, J.W.; Clark, L.D.; Caruso, J.J.

    2009-01-01

    Essential consumables like oxygen must to be produced from materials on the lunar surface to enable a sustained, long-term presence of humans on the Moon. The Outpost Precursor for ISRU and Modular Architecture (OPTIMA) field test on Mauna Kea, Hawaii, facilitated by the Pacific International Space Center for Exploration Systems (PISCES) of the University of Hawaii at Hilo, was designed to test the implementation of three hardware concepts to extract oxygen from the lunar regolith: Precursor ISRU Lunar Oxygen Testbed (PILOT) developed by Lockheed Martin in Littleton, CO; Regolith & Environmental Science and Oxygen & Lunar Volatiles Extraction (RESOLVE) developed at the NASA Kennedy Space Center in Cape Canaveral, FL; and ROxygen developed at the NASA Johnson Space Center in Houston, TX. The three concepts differ in design, but all rely on the same general principle: hydrogen reduction of metal cations (primarily Fe2+) bonded to oxygen to metal (e.g., Fe0) with the production of water. The hydrogen source is residual hydrogen in the fuel tanks of lunar landers. Electrolysis of the water produces oxygen and hydrogen (which is recycled). We used the miniaturized M ssbauer spectrometer MIMOS II to quantify the yield of this process on the basis of the quantity of Fe0 produced. Iron M ssbauer spectroscopy identifies iron-bearing phases, determines iron oxidation states, and quantifies the distribution of iron between mineral phases and oxidation states. The oxygen yield can be calculated by quantitative measurements of the distribution of Fe among oxidation states in the regolith before and after hydrogen reduction. A M ssbauer spectrometer can also be used as a prospecting tool to select the optimum feedstock for the oxygen production plants (e.g., high total Fe content and easily reduced phases). As a demonstration, a MIMOS II backscatter spectrometer (SPESI, Germany) was mounted on the Cratos rover (NASA Glenn Research Center in Cleveland, OH), which is one of

  7. Uses and perspectives of Moessbauer spectroscopic studies of iron minerals in coal

    Energy Technology Data Exchange (ETDEWEB)

    Gracia, M.; Marco, J.F.; Gancedo, J.R. [Instituto de Quimica Fisica ' Rocasolano' (Spain)

    1999-11-15

    The processes involved in the utilization of coal are affected by the minerals contained in it. Due to the presence of iron as a major constituent of coal mineral matter, and to the fact that the iron minerals, especially pyrite, and their transformation products play an important role in coal uses, {sup 57}Fe-Moessbauer spectroscopy appears as an attractive tool in coal research. Moessbauer studies related to the characterization of iron phases, coal oxidation and quantitative determination of pyritic sulphur are discussed in this work.

  8. Reducing firing of an early pottery making kiln at Batan Grande, Peru: A Moessbauer study

    Energy Technology Data Exchange (ETDEWEB)

    Wagner, U. [Technische Universitaet Muenchen, Physik-Department E15 (Germany); Gebhard, R. [Praehistorische Staatssammlung (Germany); Haeusler, W.; Hutzelmann, T. [Technische Universitaet Muenchen, Physik-Department E15 (Germany); Riederer, J. [Rathgen-Forschungslabor (Germany); Shimada, I. [Southern Illinois University (United States); Sosa, J.; Wagner, F.E. [Technische Universitaet Muenchen, Physik-Department E15 (Germany)

    1999-11-15

    Material from field firing experiments using a 2,700-year old Formative kiln at Batan Grande, Peru, was studied by X-ray diffraction and Moessbauer spectroscopy. The experiments explore the technology involved in producing the gray and black reduced ware for which Cupisnique and other Formative ceramics are justly known. During firing, the iron-bearing compounds in clays undergo characteristic changes which depend on kiln temperature and atmosphere. These changes can be observed in the Moessbauer spectra. By comparing spectra of an appropriate clay fired in field experiments and in the laboratory with the spectra of ancient ceramics, a description of Formative firing techniques in a reducing environment is attempted.

  9. Moessbauer Spectroscopic Study of a Mural Painting from Morgadal Grande, Mexico

    Energy Technology Data Exchange (ETDEWEB)

    Kuno, A.; Matsuo, M. [University of Tokyo, Graduate School of Arts and Sciences (Japan); Soto, A. Pascual [Universidad Nacional Autonoma de Mexico, Instituto de Investigaciones Esteticas (Mexico); Tsukamoto, K. [Escuela Nacional de Antropologia e Historia (Mexico)

    2004-12-15

    In this study, {sup 57}Fe Moessbauer spectroscopy has been applied to fragments of a mural painting excavated at Morgadal Grande, Mexico, to characterize the pigments used. A sextet attributable to hematite ({alpha}-Fe{sub 2}O{sub 3}) was clearly detected in the red fragments. The spectra of orange fragments showed a doublet attributable to paramagnetic high-spin Fe{sup 3+}, which presumably originates from goethite ({alpha}-FeOOH) exhibiting superparamagnetic relaxation due to its small particle size. The blue fragments contained little iron. The scattered X-ray Moessbauer spectra revealed that the thickness of the pigments was larger than 20 {mu}m.

  10. Moessbauer study of the orientation of the magnetic moments in Fe—based nanocrystalline alloys

    Institute of Scientific and Technical Information of China (English)

    HuBing-Yuan; ZhangGui-Lin; 等

    1997-01-01

    Magneto-impedance(MI) effect in Fe-based nanocrystalline Fe73 Cu1Nb1.5Mo2Si13.5B alloys has been observed by Moessbauer spectroscopy.The results show that the field dependence of the MI ratio is strongly influenced by the transverse magnetic structure in samples.

  11. Moessbauer spectra of iron--chromium sulphospinals with varying metal ratio

    Energy Technology Data Exchange (ETDEWEB)

    Lotgering, F.K.; van Diepen, A.M.; Olijhoek, J.F.

    1975-11-01

    Samples of the sulfospinel FeCr/sub 2/S/sub 4/ with varying Fe/Cr ratio around the nominal composition have been investigated by Moessbauer spectroscopy. The spectra with the narrowest lines, as well as a lambda-type peak in the specific heat-temperature curve at the low temperature transition previously described, were obtained for an overall composition with a small Fe deficit. The broadening often observed in Moessbauer spectra of FeCr/sub 2/S/sub 4/ samples is attributed to Fe/sup 2 +/ on octahedral sites in the spinel phase, resulting in an electric field gradient at the Fe/sup 2 +/ ions on the tetrahedral sites. The paramagnetic Moessbauer spectrum of Fe/sub 1.06/Cr/sub 1.94/S/sub 4/ is in accordance with this interpretation. (auth)

  12. Study on the ferromagnetic state in iron mixed-valence complexes, A[Fe{sup II}Fe{sup III}(dto){sub 3}] (A = (n-C{sub n}H{sub 2n + 1}){sub 4}N; dto = C{sub 2}S{sub 2}O{sub 2}) by means of Moessbauer spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Ono, Yuki; Okazawa, Atsushi, E-mail: cokazawa@mail.ecc.u-tokyo.ac.jp [University of Tokyo, Graduate School of Arts and Sciences (Japan); Enomoto, Masaya [Tokyo University of Science, Department of Chemistry, Faculty of Science Division I (Japan); Kojima, Norimichi, E-mail: cnori@mail.ecc.u-tokyo.ac.jp [University of Tokyo, Graduate School of Arts and Sciences (Japan)

    2012-03-15

    We have investigated the ferromagnetic states for (n-C{sub n}H{sub 2n + 1}){sub 4}N[Fe{sup II}Fe{sup III}(dto){sub 3}] (n = 3-6; dto C{sub 2}O{sub 2}S{sub 2}) by means of {sup 57}Fe Moessbauer spectroscopy. The major component of the spin configuration in the ferromagnetic states for n = 3 and 4 is the low-temperature phase (LTP) with the Fe{sup III} (S = 5/2) and Fe{sup II} (S = 0) states. The high-temperature phase (HTP) of n = 4 remains by more than 20%, which is consistent with two ferromagnetic transitions (T{sub C} = 7 and 13 K). Moreover, it was revealed that the Moessbauer spectra in the ferromagnetic states for n = 5 and 6 correspond to the HTP consisting of the Fe{sup II} (S = 2) and Fe{sup III} (S = 1/2) states.

  13. Automation of the Analysis of Moessbauer Spectra

    Energy Technology Data Exchange (ETDEWEB)

    Souza, Paulo A. de Jr.; Garg, R.; Garg, V. K. [Universidade Federal do Espirito Santo, Departamento de Fisica (Brazil)

    1998-12-15

    In the present report we propose the automation of least square fitting of Moessbauer spectra, the identification of the substance, its crystal structure and the access to the references with the help of a genetic algorith, Fuzzy logic, and the artificial neural network associated with a databank of Moessbauer parameters and references. This system could be useful for specialists and non-specialists, in industry as well as in research laboratories.

  14. Moessbauer Spectroscopy of Martian and Sverrefjell Carbonates

    Science.gov (United States)

    Agresti, David G.; Morris, Richard V.

    2011-01-01

    Mars, in its putative "warmer, wetter: early history, could have had a CO2 atmosphere much denser than its current value of Chocolate Pots in Yellowstone National Park (YNP) are shown; they are the same within error. For Comanche carbonate summed over 210-270 K, (CS, QS) = (1.23, 1.95) mm/s. The value of QS for Sverrefjell carbonate at 295 K, (CS, QS) = (1.25, 1.87) mm/s, is also plotted, and the plot shows that the QS for the Sverrefjell carbonate agrees within error with the Comanche data extrapolated to 295 K. This agreement is additional evidence that the Sverrefjell carbonates are Mossbauer analogues for the Comanche carbonates, and that both carbonates might have precipitated from solutions that became carbonate rich by passing through buried carbonate deposits.

  15. Transmission Moessbauer Analysis of Nanophased Oxides Formed on High Strength Steels

    Energy Technology Data Exchange (ETDEWEB)

    Balasubramanian, R. [James Madison University, Department of Physics (United States); Cook, D. C. [Old Dominion University, Department of Physics (United States); Townsend, H. [Homer Research Lab, Bethlehem Steel Corporation (United States)

    2002-06-15

    Nanophased oxides found in the corrosion coatings of atmospherically weathered steels have properties that are scientifically significant and industrially important. Moessbauer spectroscopy proves to be a very useful tool to accurately characterize the corrosion coatings. Samples of carbon steel were exposed in Campeche, along the Gulf of Mexico for up to one year and the development of corrosion products as a function of steel type and exposure time were studied using Moessbauer spectroscopy, micro-Raman spectrometry and X-ray diffraction. Both X-ray diffraction and transmission Moessbauer spectroscopic results indicated that lepidocrocite, maghemite and goethite were the dominant oxides. Transmission Moessbauer analysis at 77 K indicated that for up to three months of exposure, lepidocrocite and maghemite accounted for nearly 80% of the relative amount, with goethite contributing only 20% to the mixture. However, as the exposure time increased to 6 months, the relative contribution of goethite increased at the expense of decreasing amounts of maghemite. Monitoring the environment during the exposure time indicated that the average time of wetness decreased. The decrease in the relative contribution of maghemite to the total oxide concentration is related to the decreasing time of wetness, with increasing exposure time.

  16. Rare-earth magnetism in cuprates with T[sup prime-]structure. [GdPrCuO; GdNdCuO; GdSmCuO; GdEuCuO

    Energy Technology Data Exchange (ETDEWEB)

    Czjzek, G. (Kernforschungszentrum Karlsruhe, INFP and ITP, P.O. Box 3640, W-7500 Karlsruhe 1 (Germany)); Roth, G. (Kernforschungszentrum Karlsruhe, INFP and ITP, P.O. Box 3640, W-7500 Karlsruhe 1 (Germany)); Kroener, T. (Kernforschungszentrum Karlsruhe, INFP and ITP, P.O. Box 3640, W-7500 Karlsruhe 1 (Germany)); Adelmann, P. (Kernforschungszentrum Karlsruhe, INFP and ITP, P.O. Box 3640, W-7500 Karlsruhe 1 (Germany))

    1994-04-01

    Cuprates of composition (Gd[sub 1-x]R[sub x])[sub 2]CuO[sub 4], R=Pr, Nd, Sm, Eu, have been studied by [sup 155]Gd Moessbauer spectroscopy and by complementary experimental techniques. The results provide new evidence for the important influence of exchange interactions between Cu and rare-earth 4f-moments on rare-earth magnetism in these compounds. ((orig.))

  17. Thermal diffusion of {sup 57}Co into rhodium matrix as a second step in preparing Moessbauer sources

    Energy Technology Data Exchange (ETDEWEB)

    Cieszykowska, Izabela; ZoLtowska, MaLgorzata [Institute of Atomic Energy Polatom, Radioisotope Centre, 05-400 Otwock-Swierk (Poland); Zachariasz, Piotr [Institute of Atomic Energy Polatom, Moessbauer Spectroscopy Lab, 05-400 Otwock-Swierk (Poland); Piasecki, Andrzej; Janiak, Tomasz [Institute of Atomic Energy Polatom, Radioisotope Centre, 05-400 Otwock-Swierk (Poland); Mielcarski, MieczysLaw, E-mail: m.mielcarski@polatom.pl [Institute of Atomic Energy Polatom, Radioisotope Centre, 05-400 Otwock-Swierk (Poland)

    2011-09-15

    Thermal diffusion of {sup 57}Co into rhodium matrix was studied. The diffusion degree was evaluated by Moessbauer spectroscopy with the use of {alpha}-Fe absorber. The influence of different annealing conditions was investigated. For a set of sources examined, smooth and rounded Lorentzian lines were observed. The main spectra parameters are fairly acceptable with respect to the typical obtainable values for {alpha}-Fe absorbers in Moessbauer spectroscopy. The results obtained confirm that the deposited {sup 57}Co diffused almost completely into rhodium matrix without substantial loss of the activity deposited.

  18. Inelastic scattering in condensed matter with high intensity Moessbauer radiation

    Energy Technology Data Exchange (ETDEWEB)

    Yelon, W.B.; Schupp, G.

    1990-10-01

    We give a progress report for the work which has been carried out in the last three years with DOE support. A facility for high-intensity Moessbauer scattering is now fully operational at the University of Missouri Research Reactor (MURR) as well as facility at Purdue, using special isotopes produced at MURR. High precision, fundamental Moessbauer effect studies have been carried out using scattering to filter the unwanted radiation. These have led to a new Fourier transform method for describing Moessbauer effect (ME) lineshape and a direct method of fitting ME data to the convolution integral. These methods allow complete correction for source resonance self absorption (SRSA) and the accurate representation of interference effects that add an asymmetric component to the ME lines. We have begun applying these techniques to attenuated ME sources whose central peak has been attenuated by stationary resonant absorbers, to more precisely determine interference parameters and line-shape behavior in the resonance asymptotic region. This analysis is important to both the fundamental ME studies and to scattering studies for which a deconvolution is essential for extracting the correct recoilless fractions and interference parameters. A number of scattering studies have been successfully carried out including a study of the thermal diffuse scattering in Si, which led to an analysis of the resolution function for gamma-ray scattering. Also studied was the anharmonic motion in Na and the satellite reflection Debye-Waller factor in TaS{sub 2}, which indicate phason rather than phonon behavior. We have begun quasielastic diffusion studies in viscous liquids and current results are summarized. These advances, coupled to our improvements in MIcrofoil Conversion Electron spectroscopy lay the foundation for the proposed research outlined in this request for a three-year renewal of DOE support.

  19. Gamma scattering in condensed matter with high intensity Moessbauer radiation

    Energy Technology Data Exchange (ETDEWEB)

    1990-01-01

    We give a progress report for the work which has been carried out in the last three years with DOE support. A facility for high-intensity Moessbauer scattering is now fully operational at the University of Missouri Research Reactor (MURR) as well as a facility at Purdue, using special isotopes produced at MURR. High precision, fundamental Moessbauer effect studies have been carried out using scattering to filter the unwanted radiation. These have led to a new Fourier transform method for describing Moessbauer effect (ME) lineshape and a direct method of fitting ME data to the convolution integral. These methods allow complete correction for source resonance self absorption (SRSA) and the accurate representation of interference effects that add an asymmetric component to the ME lines. We have begun applying these techniques to attenuated ME sources whose central peak has been attenuated by stationary resonant absorbers, to more precisely determine interference parameters and line-shape behavior in the resonance asymptotic region. This analysis is important to both the fundamental ME studies and to scattering studies for which a deconvolution is essential for extracting the correct recoilless fractions and interference parameters. A number of scattering studies have been successfully carried out including a study of the thermal diffuse scattering in Si, which led to an analysis of the resolution function for gamma-ray scattering. Also studied was the anharmonic motion in Na and the satellite reflection Debye-Waller factor in TaS{sub 2}, which indicate phason rather than phonon behavior. We have begun quasielastic diffusion studies in viscous liquids and current results are summarized. These advances, coupled to our improvements in MIcrofoil Conversion Electron spectroscopy lay the foundation for the proposed research outlined in this request for a three-year renewal of DOE support.

  20. Moessbauer studies on impactites from Lonar impact crater

    Energy Technology Data Exchange (ETDEWEB)

    Verma, H. C., E-mail: hcverma@iitk.ac.in [I I T Kanpur, Department of Physics (India); Misra, S., E-mail: misrasaumitra@gmail.com [Indian Institute of Geomagnetism (India); Shyam Prasad, M., E-mail: shyam@nio.org [National Institute of Oceanography, Geological Oceanography Division (India); Bijlani, N.; Tripathi, A., E-mail: rpt2002@sify.com [J.N.V. University, Department of Physics (India); Newsom, Horton, E-mail: newsom@unm.edu [University of New Mexico, Institute of Meteoritics and Department of Earth and Planetary Sciences (United States)

    2008-09-15

    Iron mineralogy has been studied using Moessbauer spectroscopy on eight glassy impactite samples from different parts of the Lonar Crater Rim Region. Distinct changes are observed when compared to the host basaltic samples. Significant amount of Fe{sup 3+} phase is observed in the impactite samples whereas this phase is known to be almost absent in the basalt. Besides this we have a strong Fe{sup 2+} doublet showing up corresponding to the main iron-containing mineral. The Moessbauer results are very similar to those with glasses from Ries crater which is also believed to have formed by meteoritic impact but on nonbasaltic rock bed. Besides the glassy samples, we also study some spherules found in the crater region and some fine glassy particles on the surfaces of melt impact bombs. These contain a good amount of magnetically ordered phase, most likely nanosize hematite. Interestingly, part of it is strongly attracted by a magnet and part of it is not. But both parts show a significantly strong six-line component corresponding to hematite.

  1. Magnetic and Moessbauer Studies of Quaternary Argentine Loessic Soils and Paleosols

    Energy Technology Data Exchange (ETDEWEB)

    Mercader, R. C., E-mail: mercader@fisica.unlp.edu.ar; Sives, F. R. [Universidad Nacional de La Plata, Departamento de Fisica, IFLP, Facultad de Ciencias Exactas (Argentina); Imbellone, P. A. [Universidad Nacional de La Plata, Instituto de Geomorfologia y Suelos (Argentina); Vandenberghe, R. E. [Ghent University, NUMAT, Department of Subatomic and Radiation Physics (Belgium)

    2005-02-15

    This paper is a review of the current status about the remaining problems that are found in the investigation of the Quaternary Argentine soils and loessic sediments, and the way that Moessbauer studies can assist in solving them. There are two main types of investigations that make use of the magnetic response of the samples to correlate them with information gathered by other methods. On the one hand, there is the stratigraphic and chronological research, which is of importance from the geological and paleontological points of view. On the other hand, the paleoclimatic records, of significance toward a possible model of the past climate, are also studied because of their close relation to the sediments history. However, there is not yet a model that can tell the difference between the modifications due to the climatic conditions at the time when the soils were buried from processes that occurred after burial. Some examples are given that show that Moessbauer studies can be applied with a certain degree of success when cross-checked with magnetic measurements toward understanding the processes that occurred in alluvial B (paleosols) and C horizons (loess) from the eastern part of Buenos Aires Province. Although the application of Moessbauer studies to hydromorphic processes in soils is not straightforward, there are cases in which Moessbauer spectroscopy, if applied properly and correlated with other techniques, is able to characterize the type of iron oxides existing in the materials and thus assist theories about its origin and history.

  2. Moessbauer-spectroscopic studies on unordered oxidic solids; Moessbauer-Spektrokopische Untersuchungen ungeordneter oxidischer Festkoerper

    Energy Technology Data Exchange (ETDEWEB)

    Menzel, M.

    2004-07-01

    In this work he have performed Moessbauer spectroscopy measurements of unordered oxidic solids. Two different system have been investigated, mechanically activated Fe{sup 2+} containing spinels and glass systems. The Fe{sup 2+} containing spinels have been characterized before and after the mechanical treatment and the observed changes of the properties have been interpreted. Our special attention was focused on the changes of the magnetic properties and the mechanically induced redox processes of Fe{sub 2}GeO{sub 4}, FeV{sub 2}O{sub 4} and FeAl2O{sub 4}. The {sup 119}Sn containing glasses (similar to floatglasses) have been investigated in respect to different sodium and aluminium concentrations. In order to interprete the obtained spectra of Sn{sup 2+} a local bonding model has been suggested. The model allows statements about the local electron distribution of the investigated ions. Debye temperatures of different Sn-ions have been determined from temperature dependend measurements. These values have been compared with literature data from various Sn-Oxides. A temperature dependent extension of the local bonding modell shows an increasing roundness of the ion in respect to the electron distribution of the Sn{sup 2+} ion with increasing temperature.

  3. Moessbauer Studies in Chinese Archaeology: A Review

    Energy Technology Data Exchange (ETDEWEB)

    Hsia Yuanfu; Huang Hongbo [Nanjing University, Department of Physics (China)

    2003-09-15

    The Moessbauer effect has been applied to a wide variety of objects related to Chinese archaeology. Besides ceramic artifacts, materials like porcelain, glazes, bronzes, ancient coins, ancient mineral drugs, and even fossils were studied. This article reviews these applications with particular emphasis on the study of the famous terracotta warriors and horses of the Qin Dynasty.

  4. Moessbauer study of mixed crystalline (Eu sub 2 O sub 3) sub x (Fe sub 2 O sub 3) sub 1 sub - sub x (x=0.45)

    CERN Document Server

    Kim, J G; Kim, Y H; Kim, E C

    1998-01-01

    The crystallography and the temperature dependence of the Moessbauer parameters of mixed crystalline (Eu sub 2 O sub 3) sub x (Fe sub 2 O sub 3) sub 1 sub - sub x (x=0.45) were studied by the method of X-ray diffraction at room temperature and Moessbauer spectroscopy within the temperature range from liquid nitrogen temperature to 540 K. The X-ray diffraction pattern of the sample showed the coexistence of cubic and orthorhombic crystal phases. The Moessbauer spectrum of 540 K indicated a crystal phase which was in good agreement with the X-ray result and gave no indication, within the experimental error, of any other crystal phases. By analyzing the temperature dependence of the Moessbauer parameters by using the spin-wave theory and the Debye model, useful result were obtained for examining the changes in the physical properties in mixed crystalline system.

  5. A Moessbauer effect study of the Fe{sub 2+x}Mn{sub 1-x}Al Heusler alloys

    Energy Technology Data Exchange (ETDEWEB)

    Paduani, C., E-mail: paduani@fisica.ufsc.br [DF-UFSC (Brazil); Samudio Perez, C. A. [ICE-UPF (Brazil); Schaf, J. [IF-UFRGS (Brazil); Ardisson, J. D. [CDTN (Brazil); Takeuchi, A. Y. [CBPF (Brazil); Yoshida, M. I. [DQ-ICEX-UFMG (Brazil)

    2010-01-15

    In this work the Moessbauer spectroscopy has been used to study the magnetic properties of Fe{sub 2+x}Mn{sub 1-x}Al alloys with small deviations of composition from the stoichiometric 2:1:1. The Moessbauer parameters obtained for the L2{sub 1} phase indicate H{sub hf} fields of about 25 T and 30 T at 80 K for Fe atoms at X sites in the ordered X{sub 2}YZ structure of the L2{sub 1} full Heusler alloys.

  6. Moessbauer Study of a Celtic Pottery-Making Kiln in Lower Bavaria

    Energy Technology Data Exchange (ETDEWEB)

    Gebhard, R. [Archaeologische Staatssammlung (Germany); Guggenbichler, E.; Haeusler, W. [Technische Universitaet Muenchen, Physik Department E15 (Germany); Riederer, J. [Staatliche Museen Preussischer Kulturbesitz, Rathgen-Forschungslabor (Germany); Schmotz, K. [Kreisarchaeologie Deggendorf (Germany); Wagner, F. E.; Wagner, U. [Technische Universitaet Muenchen, Physik Department E15 (Germany)

    2004-06-15

    In 1995 a well preserved 3rd century BC Celtic kiln for pottery making was excavated at Schmiedorf in Lower Bavaria. The firing chamber and the flue plate of the kiln were preserved, whereas the dome was not found. We report on a study of material from this kiln by neutron activation analysis, thin-section microscopy, X-ray diffraction and Moessbauer spectroscopy, all performed with the aim to learn more about pottery-making procedures in Celtic times.

  7. Moessbauer study of Haltern 70 amphora sherds from Castro do Vieito, North of Portugal

    Energy Technology Data Exchange (ETDEWEB)

    Costa, B F O; Ramos Silva, M [CEMDRX, Department of Physics, University of Coimbra, P-3004-516, Coimbra (Portugal); Pereira, G [Science Museum of the University of Coimbra, P-3000-272, Coimbra Portugal (Portugal); Silva, A J M [Centro de Estudos Arqueologicos das Universidades de Coimbra e do Porto/CAM, Palacio de Sub-Ripas P-3004-395 Coimbra (Portugal); Carmo, S J C do, E-mail: benilde@ci.uc.p [GIAN, Department of Physics, University of Coimbra, P-3004-516, Coimbra (Portugal)

    2010-03-01

    Haltern 70 amphora sherds obtained from Castro do Vieito were studied by Moessbauer spectroscopy, X-ray diffraction and X-ray fluorescence. In all our samples non magnetic Fe{sup 3+} haematite species were found. In some samples, also Fe{sup 2+} was found. We conclude that the samples were fired under changing atmosphere, air being admitted at the end of the firing cycle following firing in a reducing atmosphere.

  8. Electron magnetic resonance and Moessbauer studies on iron doped SnO{sub 2} nanoparticles

    Energy Technology Data Exchange (ETDEWEB)

    Grecu, Maria Nicoleta, E-mail: mgrecu@infim.ro; Constantinescu, Serban Gr.; Ghica, Daniela; Tarabasanu-Mihaila, Doina; Diamandescu, Lucian [National Institute of Materials Physics (Romania)

    2012-03-15

    Iron doped (0.25-7.5% molar) hydrothermal nano-SnO{sub 2} was characterized by electron magnetic resonance (EMR) and Moessbauer spectroscopies. Only a small fraction of transition metal ions are in magnetic ordered state, contrary to the similar crystallographic compound TiO{sub 2}. Temperature dependences of spectra suggest that by increasing iron concentration, or annealing temperature, iron ions migrate to nanoparticles surfaces forming disordered iron oxides.

  9. {sup 57}Fe Moessbauer Spectroscopic Study on the Assembled Iron Complexes

    Energy Technology Data Exchange (ETDEWEB)

    Nakashima, S. [Hiroshima University, Natural Science Center for Basic Research and Development (N-BARD) (Japan); Asada, Y.; Okuda, T. [Hiroshima University, Department of Chemistry, Graduate School of Science (Japan)

    2004-12-15

    {sup 57}Fe Moessbauer spectroscopy was carried out to know the electronic states of the assembled iron complexes. The IS value revealed a high-spin Fe{sup II} state in the bipyridine and pyrazine iron complexes with NCS or NCSe. The dissociation behavior of ligand was investigated by TG, and the resultant change in the coordination sphere around iron atom was reflected in the change in QS value.

  10. Moessbauer studies of hemoglobin in erythrocytes exposed to neutron radiation

    Energy Technology Data Exchange (ETDEWEB)

    Niemiec, Katarzyna; Kaczmarska, Magdalena; Buczkowski, Mateusz [AGH University, Faculty of Physics and Computer Science, Department of Medical Physics and Biophysics (Poland); Fornal, Maria [Collegium Medicum, Jagiellonian University, Department of Internal Medicine and Gerontology (Poland); Pohorecki, Wladyslaw [AGH University, Faculty of Energy and Fuels (Poland); Matlak, Krzysztof; Korecki, Jozef [AGH University, Faculty of Physics and Computer Science, Department of Solid State Physics (Poland); Grodzicki, Tomasz [Collegium Medicum, Jagiellonian University, Department of Internal Medicine and Gerontology (Poland); Burda, Kvetoslava, E-mail: kvetoslava.burda@fis.agh.edu.pl [AGH University, Faculty of Physics and Computer Science, Department of Medical Physics and Biophysics (Poland)

    2012-03-15

    We studied radiation effects on the stability of various states of hemoglobin (Hb) in red blood cells (RBC) irradiated with a very low dose of neutron rays, 50 {mu}Gy. We investigated RBCs isolated from blood of healthy donors. Moessbauer spectroscopy was applied to monitor different forms of Hb. Our results show, for the first time, that oxyhemoglobin (OxyHb) and deoxyhemoglobin (DeoxyHb) are two Hb forms sensitive to such a low neutron radiation. Both Hbs change into a new Hb form (Hb{sub irr}). Additionally, OxyHb transfers into HbOH/H{sub 2}O, which under our experimental conditions is resistant to the action of neutron rays.

  11. The Nonanuclear [Mo(IV){l_brace}(CN)Fe(III)(3-ethoxy-saldptn){r_brace}{sub 8}]Cl{sub 4} Complex Compound Exhibits Multiple Spin Transitions Observed by Moessbauer Spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Renz, F., E-mail: Franz.Renz@uni-mainz.de; Kerep, P. [Johannes Gutenberg-University, Institut fuer Anorganische Chemie und Analytische Chemie (Germany)

    2004-12-15

    The pentadentate ligand 3-EO-{sup 5}LH{sub 2}= 3-ethoxy-saldptn N,N'-bis(3-ethoxy-1-hydroxy-2-benzyliden)-1,7-diamino-4-azaheptane has been prepared by a Schiff base condensation between 1,7-diamino-4-azaheptane and the corresponding 3-ethoxy-salicyaldehyde. 3-EO-{sup 5}LH{sub 2} is a sterical extention to {sup 5}LH{sub 2}. Its complexation with Fe(III) gave the high-spin (S=5/2) complex of [Fe(III)(3-EO-{sup 5}L)Cl]. This precursor was combined with [Mo(CN){sub 8}]{sup 4-} and a blue nonanuclear cluster [Mo(IV){l_brace}(CN)Fe(III)(3-EO-{sup 5}L){r_brace}{sub 8}]Cl{sub 4} resulted. This starshaped nonanuclear compound is a high-spin system at room temperature. On cooling to 10 K some of the eight iron(III) centers switched to the low-spin state as proven by Moessbauer spectra, i.e. multiple electronic transitions.

  12. Moessbauer Studies of Implanted Impurities in Solids

    CERN Multimedia

    2002-01-01

    Moessbauer studies were performed on implanted radioactive impurities in semiconductors and metals. Radioactive isotopes (from the ISOLDE facility) decaying to a Moessbauer isotope were utilized to investigate electronic and vibrational properties of impurities and impurity-defect structures. This information is inferred from the measured impurity hyperfine interactions and Debye-Waller factor. In semiconductors isoelectronic, shallow and deep level impurities have been implanted. Complex impurity defects have been produced by the implantation process (correlated damage) or by recoil effects from the nuclear decay in both semiconductors and metals. Annealing mechanisms of the defects have been studied. \\\\ \\\\ In silicon amorphised implanted layers have been recrystallized epitaxially by rapid-thermal-annealing techniques yielding highly supersaturated, electrically-active donor concentrations. Their dissolution and migration mechanisms have been investigated in detail. The electronic configuration of Sb donors...

  13. Moessbauer spectrometry applied to the study of laboratory samples made of iron gall ink

    Energy Technology Data Exchange (ETDEWEB)

    Burgaud, C. [Centre de Recherche pour la Conservation des Collections, MNHN, CNRS, MCC, 36 rue Geoffroy Saint Hilaire, CP 21, Paris (France); Universite de La Rochelle, LEMMA, Batiment Marie Curie, La Rochelle Cedex 01 (France); Rouchon, V. [Centre de Recherche pour la Conservation des Collections, MNHN, CNRS, MCC, 36 rue Geoffroy Saint Hilaire, CP 21, Paris (France); Refait, P. [Universite de La Rochelle, LEMMA, Batiment Marie Curie, La Rochelle Cedex 01 (France); Wattiaux, A. [Universite de Bordeaux 1, Institut de Chimie de la Matiere Condensee de Bordeaux, CNRS, Pessac Cedex (France)

    2008-07-15

    Iron gall inks consist of a mixture of vitriol, gall nut extracts and gum arabic. The association of the iron(II) sulphate present in vitriols, and the carboxyphenolic acids present in gall nut extracts leads to the formation of dark coloured iron-based precipitates. In order to evaluate the percentage of iron used in the formation of these precipitates, transmission Moessbauer spectroscopy (MS) measurements were performed on laboratory made inks at room temperature. These were completed by X-ray diffraction (XRD), and Raman spectroscopy measurements. The samples consisted of several solutions of iron(II) sulphate, gallic acid and gum arabic. After evaporation, the residues were analysed. Up to eight different Moessbauer signatures were detected, most of them correlated to iron sulphates. The Moessbauer signature of the iron gall precipitate was also isolated. It is not distinctly defined and may overlap with the signatures of iron(III) hydroxy-sulphates, such as jarosite or copiapite. Raman spectrometry then proved to be a useful complementary technique for the identification of the precipitate. (orig.)

  14. Moessbauer study of C18N/Fe Langmuir-Blodgett layers

    Energy Technology Data Exchange (ETDEWEB)

    Kuzmann, Erno [Institute of Chemistry, Eoetvoes Lorand University (Hungary); Telegdi, Judit [Institute of Nanochemistry and Catalysis, Chemical Research Center, HAS (Hungary); Nemeth, Zoltan, E-mail: hentes@chem.elte.hu; Vertes, Attila [Institute of Chemistry, Eoetvoes Lorand University (Hungary); Nyikos, Lajos [Institute of Nanochemistry and Catalysis, Chemical Research Center, HAS (Hungary)

    2012-03-15

    Langmuir-Blodgett (LB) films of octadecanoyl hydroxamic acid (C18N) complexed with Fe{sup 3 + } ions have been prepared at various subphase pH values. The LB films consisting of different number of layers were investigated by {sup 57}Fe conversion electron Moessbauer spectroscopy (CEM) at room temperature. The CEM detector contained a piece of {alpha}-iron, enriched with {sup 57}Fe, using as an internal standard. The Moessbauer pattern of the C18N/Fe LB films is a doublet with parameters {delta} = 0.35 mm/s and {Delta} = 0.74 mm/s. A gradual increase of the relative occurrence of the doublet compared to the sextet of the internal standard was observed with the increasing number of layers, indicating the nearly uniform distribution of Fe among the LB layers.

  15. Moessbauer effect study of fly and bottom ashes from an electric generating plant

    Energy Technology Data Exchange (ETDEWEB)

    Vandenberghe, R. E., E-mail: Robert.Vandenberghe@UGent.be; Resende, V. G. de; De Grave, E. [Ghent University, Department of Subatomic and Radiation Physics (Belgium)

    2009-06-15

    Samples of a fly ash and a bottom ash, each before and after ignition, have been investigated by X-ray diffraction and Moessbauer spectroscopy in order to explain the observed negative loss of ignition (LOI). It is shown that the ashes after ignition contain more maghemite resulting from newly formed magnetite. Moreover, the fly ash which contained already magnetite exhibited an increase of hematite after ignition. Both oxidation processes can be responsible for a weight gain which compensates the loss due to the burning of the remaining carbon. The magnetite and the alpha-iron formed after ignition is originated by an unidentified compound represented by a Fe{sup 2+} doublet in the Moessbauer spectrum.

  16. Moessbauer study of glasses in meteorites: the D'Orbigny angrite and Cachari eucrite

    Energy Technology Data Exchange (ETDEWEB)

    Abdu, Y. A.; Souza Azevedo, I. [Centro Brasileiro de Pesquisas Fisicas (Brazil); Stewart, S. J. [Universidad Nacional de La Plata, IFLP, CONICET, Depto. De Fisica, Facultad de Cs. Exactas (Argentina); Lopez, A. [Centro Brasileiro de Pesquisas Fisicas (Brazil); Varela, M. E. [CONICET-UNS, Depto. de Geologia (Argentina); Kurat, G. [Naturhistorisches Museum (Austria); Scorzelli, R. B., E-mail: scorza@cbpf.br [Centro Brasileiro de Pesquisas Fisicas (Brazil)

    2005-11-15

    Moessbauer spectroscopy measurements at room temperature (RT) and at liquid helium temperature (4.2 K) were carried out on bulk and glass samples from the D'Orbigny (angrite) and Cachari (eucrite) meteorites. The RT Moessbauer spectrum of the bulk sample of D'Orbigny shows the presence of Fe{sup 2+} in olivine and pyroxene and that of bulk Cachari contains only pyroxene. Very small amounts of Fe{sup 3+} are also present in the bulk samples, but are attributed to surface contamination. The RT spectra of the D'Orbigny and Cachari glasses are fitted with three doublets, which are assigned to Fe{sup 2+} at three different octahedral positions. No Fe{sup 3+} was detected in the glass samples. The spectra of the glasses measured at 4.2 K show the presence of relaxation effects. The results suggest a certain degree of structural ordering in these glasses.

  17. Moessbauer Study of Ceramic Finds from the Galeria de las Ofrendas, Chavin de Huantar

    Energy Technology Data Exchange (ETDEWEB)

    Lumbreras, L. G. [Museo Nacional de Antropologia (Peru); Gebhard, R. [Archaeologische Staatssammlung Muenchen (Germany); Haeusler, W. [Technische Universitaet Muenchen, Physik-Department E15 (Germany); Kauffmann-Doig, F. [Universidad Peruana de Ciencias Aplicadas (UPC) (Peru); Riederer, J. [Rathgen-Forschungslabor (Germany); Sieben, G.; Wagner, U. [Technische Universitaet Muenchen, Physik-Department E15 (Germany)

    2003-09-15

    Ceramic finds from the Galeria de las Ofrendas at Chavin de Huantar and surface finds from the settlement of Chavin were characterised by combining the results of archaeological typology with archaeometric studies using neutron activation analysis, Moessbauer spectroscopy, X-ray diffraction and thin-section microscopy. Sherds from the pyramid Tello are included in the study as representative of local material. The analyses show that the vessels were made from different raw materials and that different firing procedures were used in their production. Sherds of certain styles largely exhibit similar types of Moessbauer patterns and in many instances also have similar element compositions. This supports the archaeological notion that the vessels were brought to Chavin from the provinces, perhaps on the occasion of a festivity.

  18. Moessbauer study of FINEMET type nanocrystalline ribbons irradiated with swift heavy ions

    Energy Technology Data Exchange (ETDEWEB)

    Kuzmann, Erno, E-mail: kuzmann@ludens.elte.hu; Stichleutner, Sandor; Sapi, Andras [Institute of Chemistry, Eoetvoes University (Hungary); Varga, Lajos Karoly [Research Institute for Solid State Physics and Optics, HAS (Hungary); Havancsak, Karoly [Eoetvoes University, Department of Materials Physics (Hungary); Skuratov, Vlamidir [Joint Institute for Nuclear Research (Russian Federation); Homonnay, Zoltan; Vertes, Attila [Institute of Chemistry, Eoetvoes University (Hungary)

    2012-03-15

    As-quenched and stress field annealed FINEMET ribbons were irradiated with 246 MeV energy Kr, 470 MeV energy Xe and 720 MeV energy Bi ions and investigated by {sup 57}Fe Moessbauer spectroscopy and XRD methods. The change in relative areas of the 2nd and 5th lines in the Moessbauer spectra indicated significant changes in the magnetic anisotropy of both as-quenched and stress annealed FINEMET due to irradiation with swift heavy ions. Differences were observed between the effect of irradiations with various ions having different energy and fluence. The effect of irradiation on the magnetic orientation in FINEMET was explained in terms of radiation induced defects. The swift heavy ion irradiation can be applied to produce FINEMET ribbons with more favorable soft magnetic properties for technological applications.

  19. Moessbauer study of peroxynitrito complex formation with Fe{sup III}-chelates

    Energy Technology Data Exchange (ETDEWEB)

    Homonnay, Zoltan, E-mail: homonnay@ludens.elte.hu; Buszlai, Peter; Nador, Judit [Eoetvoes University, Institute of Chemistry (Hungary); Sharma, Virender K. [Florida Institute of Technology (United States); Kuzmann, Erno; Vertes, Attila [Eoetvoes University, Institute of Chemistry (Hungary)

    2012-03-15

    The reaction of the {mu}-oxo-diiron(III)-L complex (L = EDTA, ethylene diamine tetraacetate, HEDTA, hydroxyethyl ethylene diamine triacetate, and CyDTA, cyclohexane diamine tetraacetate) with peroxynitrite in alkaline solution was studied by Moessbauer spectroscopy using rapid-freezing technique. These complexes yield an (L)Fe{sup III}({eta}{sup 2}-O{sub 2}){sup 3-} complex ion when they react with hydrogen peroxide and the formation of the peroxide adduct results in a deep purple coloration of the solution. The same color appears when the reaction occurs with peroxinitrite. Although spectrophotometry indicated some difference between the molar extinction coefficients of the peroxo and the peroxinitrito adducts, the Moessbauer parameters proved to be the same within experimental error. It is concluded that the peroxynitrite ion decomposes when reacting with Fe{sup III}(L) and the peroxo adduct forms.

  20. Effect of nanocrystallization on the electrical conductivity enhancement and Moessbauer hyperfine parameters of iron based glasses

    Energy Technology Data Exchange (ETDEWEB)

    El-Desoky, M.M., E-mail: mmdesoky@gmail.com [Department of Physics, Faculty of Education, Suez Canal University, Al-Arish 45511, North Sinaa (Egypt); Ibrahim, F.A. [Department of Physics, Faculty of Education, Suez Canal University, Al-Arish 45511, North Sinaa (Egypt); Mostafa, A.G.; Hassaan, M.Y. [Department of Physics, Faculty of Science, Al-Azhar University, Nasr City 11884, Cairo (Egypt)

    2010-09-15

    Selected glasses of Fe{sub 2}O{sub 3}-PbO{sub 2}-Bi{sub 2}O{sub 3} system have been transformed into nanomaterials by annealing at temperature close to crystallization temperature (T{sub c}) for 1 h. The effects of the annealing of the present samples on its structural and electrical properties were studied by Moessbauer spectroscopy, transmission electron micrograph (TEM), differential scanning calorimeter (DSC) and dc conductivity ({sigma}). Moessbauer spectroscopy was used in order to determine the states of iron and its hyperfine structure. The effect of nanocrystalization on the Moessbauer hyperfine parameters did not exhibit significant modifications in present glasses. However, in case of glass ceramic nanocrystals show a distinct decrease in the quadrupole splitting ({Delta}) is observed, reflecting an evident decrease in the distortion of structural units like FeO{sub 4} units. In general, the Moessbauer parameters of the nano-crystalline phase exhibit tendency to increase with PbO{sub 2} content. TEM of as-quenched glasses confirm the homogeneous and essentially featureless morphology. TEM of the corresponding glass ceramic nanocrystals indicates nanocrystals embedded in the glassy matrix with average particle size of about 32 nm. The crystallization temperature (T{sub c}) was observed to decrease with PbO{sub 2} content. The glass ceramic nanocrystals obtained by annealing at T{sub c} exhibit improvement of electrical conductivity up to four orders of magnitude than the starting glasses. This considerable improvement of electrical conductivity after nanocrystallization is attributed to formation of defective, well-conducting phases 'easy conduction paths' along the glass-crystallites interfaces.

  1. Hyper-Raman spectroscopy of Earth related materials

    Science.gov (United States)

    Hellwig, H.

    2004-12-01

    Raman and infrared spectroscopy proved extremely successful in obtaining structural information and thermodynamic data on samples under high pressure conditions in a diamond anvil cell [1,2]. With substantial advances in CCD detector technology and the possibility to focus visible laser light down to several microns, Raman spectroscopy can nowadays be regarded one of the standard techniques for diamond anvil cell investigations. Nevertheless, Raman scattering suffers from often strong fluorescence and the strong Raman signal of the diamonds. Infrared spectroscopy is limited by the sample size and the diffraction limit of mid- or far-infrared radiation. With increasing pressure, diamonds also show strong infrared activity, which can interfere with the signal from the sample. Detectors in the mid- and far-infrared are inherently noisy, often leading to low signal-to-noise ratios for infrared measurements. With new techniques and instrumentation available, such as low noise CCD cameras and stable diode-pumped solid state laser systems, more demanding techniques become feasible as well. Especially hyper-Raman scattering, a nonlinear optical variant of infrared spectroscopy, can be used on a more routine basis for the first time. Pioneering work in the 70s and 80s have explored some of the capabilities of Hyper-Raman spectroscopy [3]. Unlike infrared spectroscopy, Hyper-Raman is not limited by the diffraction limit of mid- or far-infrared radiation, typically restricting the lower frequency limit to several hundred wave numbers. The major advantages of hyper-Raman are essentially background free spectra and the use of wavelengths in the near-infrared and visible, making possible micro focusing and taking advantage of high efficiencies, low noise, and smooth wavelength dependencies of CCD detectors. Hyper-Raman does not suffer from saturation caused by strong absorption in the infrared and is therefore less sensitive to surface effects. For centrosymmetric materials

  2. Identifying meteorite source regions through near-Earth object spectroscopy

    Science.gov (United States)

    Thomas, Cristina A.; Binzel, Richard P.

    2010-02-01

    By virtue of their landing on Earth, meteorites reside in near-Earth object (NEO) orbits prior to their arrival. Thus the population of observable NEOs, in principle, gives important representation of meteorite source bodies. By linking meteorites to NEOs, and linking NEOs to their most likely main-belt source locations, we seek to gain insight into the original Solar System formation locations for different meteorite classes. To forge possible links between meteorites and NEOs, we have developed a three dimensional method for quantitative comparisons between laboratory measurements of meteorites and telescopic measurements of near-Earth objects. We utilize meteorite spectra from the Reflectance Experiment Laboratory (RELAB) database and NEO data from the SpeX instrument on the NASA Infrared Telescope Facility (IRTF). Using the Modified Gaussian Model (MGM) as a mathematical tool, we treat asteroid and meteorite spectra identically in the calculation of 1-μm and 2-μm Geometric Band Centers and their Band Area Ratios (BARs). Using these identical numerical parameters we quantitatively compare the spectral properties of S-, Sq-, Q- and V-type NEOs with the spectral properties of the meteorites in four classes: H, L, LL and HED. For each NEO spectrum, we assign a set of probabilities for it being related to each of these four meteorite classes. Our NEO-meteorite correlation probabilities are then convolved with NEO-source region probabilities to yield a final set of meteorite-source region correlations. While the ν6 resonance dominates the delivery for all four meteorite classes, an excess (significant at the 2.1-sigma level) source region signature is found for the H chondrites through the 3:1 mean motion resonance. This results suggest an H chondrite source with a higher than average delivery preference through the 3:1 resonance. A 3:1 resonance H chondrite source region is consistent with the short cosmic ray exposure ages known for H chondrites.

  3. Moessbauer study of spin structure transformation from an incommensurate to a commensurate state

    Energy Technology Data Exchange (ETDEWEB)

    Choi, Kang Ryong; Park, Seung-Iel; Kim, Sam Jin; Kim, Chul Sung, E-mail: cskim@phys.kookmin.ac.kr [Kookmin University, Departmentt of Physics (Korea, Republic of)

    2009-01-15

    We present crystallographic and magnetic properties of NiCr{sub 1.98}{sup 57}Fe{sub 0.02}O{sub 4} by using X-ray diffractometry (XRD), vibrating sample magnetometry (VSM), and Moessbauer spectroscopy. The lattice constants a{sub 0} were determined to be 8.318 A. The ferrimagnetic Neel temperature (T{sub N}) for NiCr{sub 1.98}{sup 57}Fe{sub 0.02}O{sub 4} is determined to be 90 K. The Moessbauer absorption spectra for all chromites at 4.2 K show two well developed sextets superposed with small difference of hyperfine fields (H{sub hf}) caused by Cr{sup 3+} ions in two different magnetic sites. The values of the isomer shifts show that the charge states of Fe are Fe{sup 3+} for all temperature range. Ni-chromites Moessbauer spectra below T{sub N} present aline broadening due to a Jahn-Teller distortion and show that spin structure behavior of Cr ions change from an incommensurate to a commensurate state.

  4. The stabilization of the highest oxidation states of transition metals under oxygen pressures: TlNiO sub 3 , a new Ni(III) perovskite - comparison of the electronic properties with those of TNiO sub 3 (T = rare earth and Y)

    CERN Document Server

    Kim, S J; Presniakov, I

    2002-01-01

    The crystal structure and the magnetic properties of TlNiO sub 3 have been characterized and compared with those of TNiO sub 3 (T = rare earth and Y). The electronic structure of Ni(III) has been investigated by Moessbauer spectroscopy. Through these analyses, the effects of the A-site ion on structural distortion, magnetic behaviour and electronic structure of Ni(III) in a perovskite have been discussed.

  5. XRD and Moessbauer characterization of iron-doped SnO{sub 2} powders obtained by ball-milling

    Energy Technology Data Exchange (ETDEWEB)

    Brito, A.D.B. de; Alves, H.W.L.; Raposo, M.T. [Universidade Federal de Sao Joao del-Rei (UFSJ), MG (Brazil); Ardisson, J.D. [Centro de Desenvolvimento da Tecnologia Nuclear (CDTN/CNEN-MG), Belo Horizonte, MG (Brazil)

    2012-07-01

    Full text: Rutile SnO{sub 2} (or cassiterite) is a semiconductor oxide, with many industrial applications, mainly as spin source for spintronics because of the relevant electronic and magnetic properties changes when doped with transition elements (TE) like Fe, Co, Ni and Co. Therefore, it is meaningful for the materials science research to study the properties of SnO{sub 2} nanomaterials doped by a TE ion. In this work, mechanical alloying process has been used to produce SnO{sub 2} doped with iron. The samples were characterized by X-Ray and Moessbauer spectroscopy. The crystalline alloy were obtained by milling in a planetary ball mill with a zirconia milling assembly for up to 24 hours in air, at room temperature. The mill rotation speed was 250 rpm and two different powder-to-ball weight ratios, 1:20 and 1:10, were used. X-ray diffraction analyses of SnO{sub 2} powders indicate only the formation of the cassiterite phase. X-Ray diffraction results of SnO{sub 2} doped with 10% of iron show some peaks quite wider when compared with diffraction peaks of the undoped samples, suggesting the absorption of iron probably in a new phase with tin. However, this phase cannot be identified by X-Ray diffraction. Moessbauer spectroscopy analyses (table below) indicate the presence of 85% of {alpha}-Fe and two new phases, both related to Fe-Sn phase magnetically disordered. On the other hand, {sup 119}Sn-Moessbauer spectroscopy measurements show the presence of tetrahedral tin (IV), chemical environment of the tin species. Based on the obtained results, thermal annealing and new measurements with both XRD and Moessbauer spectroscopies will be performed and compared with them. (author)

  6. A Moessbauer investigation of complexes of tin tetrahalides with ambidentate Lewis bases containing nitrogen, sulphur and oxygen

    Energy Technology Data Exchange (ETDEWEB)

    Teles, W.M. (Dept. de Quimica, ICEx, Univ. Federal de Minas Gerais, Belo Horizonte (Brazil)); Allain, L.R. (Dept. de Quimica, ICEx, Univ. Federal de Minas Gerais, Belo Horizonte (Brazil)); Filgueiras, C.A.L. (Dept. de Quimica, ICEx, Univ. Federal de Minas Gerais, Belo Horizonte (Brazil)); Abras, A. (Dept. de Fisica, ICEx, Univ. Federal de Minas Gerais, Belo Horizonte (Brazil))

    1994-02-01

    A series of 1 : 1 complexes was prepared with SnX[sub 4] (X = Cl, Br, I) and the Lewis bases 2-mercaptobenzothiazole, 2-mercapto-1-methylimidazole, 2-aminothiazole, 2-acetylpyridine, and 2,2'-bis(pyridyl)ketone. The latter two ligands yielded bidentate, N, O-bonded hexacoordinate complexes, whereas the other ligands produced monodentate, N-bonded pentacoordinate species, as suggested by Moessbauer parameters, which correlate quite well with the IR spectroscopy data. (orig.)

  7. Moessbauer effect and magnetization studies of Nd{sub 16}Fe{sub 76-x}Ru {sub x}B{sub 8} alloys

    Energy Technology Data Exchange (ETDEWEB)

    Valcanover, J.A. [DF-UFSC, Florianopolis, CEP 88040-900, SC (Brazil); Paduani, C. [DF-UFSC, Florianopolis, CEP 88040-900, SC (Brazil)]. E-mail: paduani@fisica.ufsc.br; Ardisson, J.D. [CDTN, Belo Horizonte, CEP 30123-970, MG (Brazil); Samudio Perez, C.A. [FEA-UPF, Passo Fundo, CEP 99001-970, RS (Brazil); Yoshida, M.I. [DQ-UFMG, Belo Horizonte, CEP 31270-901, MG (Brazil)

    2005-05-15

    The intrinsic magnetic properties of Nd{sub 16}Fe{sub 76-x}Ru {sub x}B{sub 8} alloys are investigated by means of Moessbauer spectroscopy and magnetization measurements. The Moessbauer parameters derived from fitting the six sextets assigned to the six different iron sites provide information about preferential site occupation of solute atoms. The cell volume decreases with the Ru substitution for Fe and the shrinkage of the lattice is greater in the c direction than in the a direction of the tetragonal unit cell. The decrease of the spectral area for the subpatterns corresponding to k{sub 1} and k{sub 2} sites with the substitution indicates that the ruthenium atoms enter preferentially in these sites, whereas the Fe atoms prefer the j-sites. The behavior of the Moessbauer parameters with changes in composition indicates that the ruthenium interactions have long range order character in this compound.

  8. Characterization of Ag-Ge-Se bulk glasses by means of Moessbauer effect on {sup 57}Fe and {sup 119}Sn atomic nuclei

    Energy Technology Data Exchange (ETDEWEB)

    Arcondo, B; Urena, M A; Garrido, J M Conde; Rocca, J A; Fontana, M, E-mail: barcond@fi.uba.a [Laboratorio de Solidos Amorfos, INTECIN, Facultad de IngenierIa, Universidad de Buenos Aires-CONICET (Argentina)

    2010-03-01

    In this work, the structure of Fe and Sn doped Ag{sub x}(Ge{sub 0.25}Se{sub 0.75}){sub 100-x} (x=0 to 25 at.%) intrinsically inhomogeneous glasses is analyzed employing {sup 119m}Sn and {sup 57}Fe Moessbauer spectroscopy, X-ray diffractometry and scanning electron microscopy. {sup 119m}Sn enters in the glass as a substitutional impurity for Ge whereas {sup 57}Fe enters as an interstitial impurity. Moessbauer spectra obtained with {sup 119m}SnO{sub 3}Ca source, from samples containing about 1% {sup 119}Sn for Ge, reveal that the local order of Ge in both amorphous phases is basically the same whereas Moessbauer spectra obtained with {sup 57}Fe(Rh) source, from samples containing about 0.5% {sup 57}Fe, evidence the differences between both phases.

  9. Moessbauer of phase separation in FeNi multilayers under ion bombardment

    Energy Technology Data Exchange (ETDEWEB)

    Amaral, L.; Paesano, A.; Brueckman, M.E. [Rio Grande do Sul Univ., Porto Alegre, RS (Brazil). Inst. de Fisica; Scorzelli, R.B.; Dominguez, A.B. [Centro Brasileiro de Pesquisas Fisicas (CBPF), Rio de Janeiro, RJ (Brazil); Shinjo, T.; Ono, T.; Hosoito, N. [Kyoto Univ. (Japan). Inst. for Chemical Research

    1997-01-01

    We investigated the effect of noble gas irradiation (He, Ne, Ar and Xe) on the Fe-Ni multilayers with a very thin modulation and nominal composition in the invar region Fe{sub 0.63} Ni{sub 0.37}. The evaluation of the formation/stability of the Fe-Ni phases formed under irradiation with different ions and doses was followed by conversion electron Moessbauer spectroscopy (CEMS). (author). 21 refs., 4 figs., 2 tabs.; e-mail: scorza at novell.cat.cbpf.br.

  10. {sup 57}Fe Moessbauer Studies in Mo-Fe Supported Catalysts

    Energy Technology Data Exchange (ETDEWEB)

    Castelao-Dias, M. [University of Coimbra, Department of Chemical Engineering (Portugal); Costa, B. F. O. [University of Coimbra, Department of Physics (Portugal); Quinta-Ferreira, R. M. [University of Coimbra, Department of Chemical Engineering (Portugal)

    2001-09-15

    Industrially, the Mo-Fe catalysts used in the selective oxidation of methanol to formaldehyde can rapidly deactivate. The use of support materials may reduce the high temperatures in the catalytic bed and/or increase thermal and mechanical resistance. However, during the preparation of these catalysts, or even during reaction conditions, the active species may react with the support material losing their catalytic activity. In this work silica, silicium carbide and titania were studied as supported catalysts by Moessbauer spectroscopy which proved to be a useful technique in the choice of supported materials.

  11. Moessbauer characterization of joints of steel pieces in transient liquid phase bonding experiences

    Energy Technology Data Exchange (ETDEWEB)

    Di Luozzo, N.; Martinez Stenger, P. F.; Canal, J. P.; Fontana, M. R.; Arcondo, B., E-mail: barcond@fi.uba.ar [INTECIN (UBA-CONICET), Laboratorio de Solidos Amorfos, Facultad de Ingenieria (Argentina)

    2011-11-15

    Joining of seamless, low carbon, steel tubes were performed by means of Transient Liquid Phase Bonding process employing a foil of Fe-Si-B metallic glass as filler material. The influence of the main parameters of the process was evaluated: temperature, holding time, pressure and post weld heat treatment. Powder samples were obtained from the joint of tubes and characterized employing Moessbauer Spectroscopy in transmission geometry. The sampling was performed both in tubes successfully welded and in those which show joint defects. The results obtained are correlated with the obtained microstructure and the diffusion of Si and B during the process.

  12. Early Pottery Making in Northern Coastal Peru. Part III: Moessbauer Study of Sican Pottery

    Energy Technology Data Exchange (ETDEWEB)

    Shimada, I. [Southern Illinois University (United States); Haeusler, W.; Hutzelmann, T. [Technische Universitaet Muenchen, Physik-Department E15 (Germany); Riederer, J. [Rathgen-Forschungslabor, Staatliche Museen Preussischer Kulturbesitz (Germany); Wagner, U. [Technische Universitaet Muenchen, Physik-Department E15 (Germany)

    2003-09-15

    Sican blackware from a 1000-year old elite tomb at Huaca Loro was characterised by neutron activation analysis, optical thin-section microscopy, X-ray diffraction and Moessbauer spectroscopy. A number of blackware fragments from the later site of Puerto Pobre (ca. AD 1460-1550) were included in the analysis for comparison and found to be of different origin. The black surface of the specimens from Huaca Loro is mostly due to carbon deposition during firing in a reducing environment. Part of the pottery was merely dried at temperatures below 400 deg. C, perhaps because it was made in haste for funeral use.

  13. Moessbauer studies of frataxin role in iron-sulfur cluster assembly and dysfunction-related disease

    Energy Technology Data Exchange (ETDEWEB)

    Garcia-Serres, Ricardo [Universite Joseph Fourier (France); Clemancey, Martin [CNRS, UMR5249 (France); Oddou, Jean-Louis [Universite Joseph Fourier (France); Pastore, Annalisa [Medical Research Council National Institute for Medical Research (United Kingdom); Lesuisse, Emmanuel [Laboratoire Mitochondries, Metaux et Stress oxydant, Institut Jacques Monod, CNRS-Universite Paris (France); Latour, Jean-Marc, E-mail: jean-marc.latour@cea.fr [CEA, iRTSV, LCBM (France)

    2012-03-15

    Friedreich ataxia is a disease that is associated with defects in the gene coding for a small protein frataxin. Several different roles have been proposed for the protein, including iron chaperoning and iron storage. Moessbauer spectroscopy was used to probe these hypotheses. Iron accumulation in mutant mitochondria unable to assemble iron sulfur clusters proved to be insensitive to overexpression of frataxin, ruling out its potential involvement as an iron storage protein similar to ferritin. Rather, it was found that frataxin negatively regulates iron sulfur cluster assembly.

  14. Determination of Coordination Configuration of Rare Earth Ionswith Aminoacids in Solutions with Cooperative Vibronic Spectroscopy

    Institute of Scientific and Technical Information of China (English)

    2000-01-01

    The use of cooperative vibronic spectroscopy to measure coordination numbers of the ligands surrounding rare earth ions in solutions was proposed and demonstrated. It is shown that the time-resolved cooperative vibronic spectroscopy is a very useful technique for the determination of the ligand type and ligand number for different coordination groups. Coordination configuration of arginine with Tb3+ in solutions with different pH values was studied. It demonstrates that the carboxyl of arginine can replace H2O to coordinate with Tb3+ and the coordination number of carboxyl increases with the increase of pH value of the solutions.

  15. Moessbauer backscatter spectrometer with full data processing capability

    Energy Technology Data Exchange (ETDEWEB)

    O' Connell, T.; Hartzell, R.; Liebermann, M.

    1976-01-01

    The design and operation of a Moessbauer backscatter spectrometer with full data processing capability is described, and the investigation of the applicability of this technique to a variety of practical metallurgical problems is discussed. (WHK)

  16. Moessbauer spectroscopic investigation of low rank coal lithotypes

    Energy Technology Data Exchange (ETDEWEB)

    Kostova, I.; Markova, K.; Kuntchev, K. [Bulgarian Academy of Sciences, Sofia (Bulgaria). Inst. of Applied Mineralogy

    1997-12-31

    Low rank coal lithotypes - xylain, humovitrain, semifusain, fusain and liptain sampled from the Maritsa Iztok coal basin (Bulgaria) have been examined by Moessbauer spectroscopy with no pre-concentration procedures. The results are used to identify three iron species in coal lithotypes and show that covalent iron (Fe{sup II}) related to pyrite, is the main iron species in xylain, while in humovitrain ferric iron is dominant. The total quantity of iron species in semifusain, fusain and liptain is about the same but their distribution is different. Ferric iron dominates in all the three lithotypes. Ferrous iron, although present in smaller quantities, has a higher content in fusain than in semifusain. The results illustrate the type of oxidation processes which formed the coal lithotypes. A transformation of Fe{sup 2+} to Fe{sup 3+} has occurred as a result of differing oxidation processes. The intensity of that transformation increases during the destructive microbial oxidation and decreases during thermal oxidation and direct oxidation processes. The opposite transformation of ferric to ferrous iron has been achieved during both thermal oxidation and direct oxidation processes. 9 refs., 2 figs., 2 tabs.

  17. High-pressure Moessbauer study of perovskite iron oxides

    CERN Document Server

    Kawakami, T; Sasaki, T; Kuzushita, K; Morimoto, S; Endo, S; Kawasaki, S; Takano, M

    2002-01-01

    The perovskite oxides CaFeO sub 3 and La sub 1 sub / sub 3 Sr sub 2 sub / sub 3 FeO sub 3 have been investigated by high-pressure sup 5 sup 7 Fe Moessbauer spectroscopy. The critical temperatures of the charge disproportionation (CD) and the magnetic order (MO) have been determined as a function of pressure. In CaFeO sub 3 the CD (2Fe sup 4 sup + -> Fe sup 3 sup + + Fe sup 5 sup +) occurs at an almost constant temperature of 290 K in the pressure range of 0-17 GPa. Above 20 GPa, the CD is suppressed. The MO temperature of 125 K at an ambient pressure rises to 300 K at 34 GPa. In La sub 1 sub / sub 3 Sr sub 2 sub / sub 3 FeO sub 3 the CD (3Fe sup 1 sup 1 sup / sup 3 sup + -> 2Fe sup 3 sup + + Fe sup 5 sup +) and the MO occur at the same temperature up to 21 GPa, which decreases from 207 to 165 K with increasing pressure. Above 25 GPa, however, the MO temperature rises above 400 K.

  18. The EnMAP Spaceborne Imaging Spectroscopy Mission for Earth Observation

    Directory of Open Access Journals (Sweden)

    Luis Guanter

    2015-07-01

    Full Text Available Imaging spectroscopy, also known as hyperspectral remote sensing, is based on the characterization of Earth surface materials and processes through spectrally-resolved measurements of the light interacting with matter. The potential of imaging spectroscopy for Earth remote sensing has been demonstrated since the 1980s. However, most of the developments and applications in imaging spectroscopy have largely relied on airborne spectrometers, as the amount and quality of space-based imaging spectroscopy data remain relatively low to date. The upcoming Environmental Mapping and Analysis Program (EnMAP German imaging spectroscopy mission is intended to fill this gap. An overview of the main characteristics and current status of the mission is provided in this contribution. The core payload of EnMAP consists of a dual-spectrometer instrument measuring in the optical spectral range between 420 and 2450 nm with a spectral sampling distance varying between 5 and 12 nm and a reference signal-to-noise ratio of 400:1 in the visible and near-infrared and 180:1 in the shortwave-infrared parts of the spectrum. EnMAP images will cover a 30 km-wide area in the across-track direction with a ground sampling distance of 30 m. An across-track tilted observation capability will enable a target revisit time of up to four days at the Equator and better at high latitudes. EnMAP will contribute to the development and exploitation of spaceborne imaging spectroscopy applications by making high-quality data freely available to scientific users worldwide.

  19. Effects of alkaline earth metal ion complexation on amino acid zwitterion stability: Results from infrared action spectroscopy

    NARCIS (Netherlands)

    Bush, M. F.; Oomens, J.; Saykally, R. J.; Williams, E. R.

    2008-01-01

    The structures of isolated alkaline earth metal cationized amino acids are investigated using infrared multiple photon dissociation (IRMPD) spectroscopy and theory. These results indicate that arginine, glutamine, proline, serine, and valine all adopt zwitterionic structures when complexed with diva

  20. Neutron diffraction and Moessbauer study on FeGa{sub x}Cr{sub 2-x}S{sub 4}

    Energy Technology Data Exchange (ETDEWEB)

    Kim, Sam Jin; Son, Bae Soon; Shim, In-Bo [Kookmin University, Department of Physics (Korea, Republic of); Lee, Bo Wha [Hankuk University of Foreign Studies, Department of Physics (Korea, Republic of); Kim, Chul Sung, E-mail: cskim@phys.kookmin.ac.kr [Kookmin University, Department of Physics (Korea, Republic of)

    2006-02-15

    Ga doped sulphur spinel FeGa{sub x}Cr{sub 2-x}S{sub 4} (x = 0.1 and 0.3) have been studied with X-ray, neutron diffraction, and Moessbauer spectroscopy. Rietveld refinement of X-ray, neutron diffraction, and Moessbauer spectroscopy lead to the conclusion that the samples are in inverse spinel type, where most Ga ions are present at octahedral site (B). The neutron diffractions on FeGa{sub x}Cr{sub 2-x}S{sub 4} (x = 0.1) above 10 K show long range interaction behaviors and reveal a ferrimagnetic ordering, with the magnetic moment of Fe{sup 2+}(-3.45 {mu}{sub B}) aligned antiparallel to Cr{sup 3+} (+2.89 {mu}{sub B}) at 10 K. Fe ions migrate from the tetrahedral (A) site to the octahedral (B) site with an increase in Ga substitutions. The electric quadrupole splittings of the A and B sites in Moessbauer spectra give direct evidence that Ga ions stimulate an asymmetric charge distribution of Fe ions in the A site.

  1. Moessbauer comparative study of Fe-Si (3.5 wt%) alloys produced by melting and by mechanical alloying

    Energy Technology Data Exchange (ETDEWEB)

    Sanchez Sthepa, H.; Fajardo, M.; Perez Alcazar, G.A. [Universidad del Valle, A.A, Departamento de Materiales (Colombia)

    1999-11-15

    Moessbauer spectroscopy and X-ray diffraction measurements were done on Fe-Si (3.5 wt%) alloys produced by melting and by mechanical alloying during 15, 30, 50 and 75 milling hours from over 99% purity powders. The Moessbauer spectra were fitted using hyperfine field distribution and it was obtained for all the samples in three ferromagnetic sites with fields of 27, 30 and 33 T for the mechanical alloyed samples and 26.8, 30.13 and 32.83 T for the commercial sample. These three sites are attributed to the pure Fe, Fe with one Si in the next near neighbor (nnn) and Fe with two Si in the nnn. As the milling time increases, the mean field increases too. X-ray diffraction measurement shows that all the samples are BCC, with a lattice parameter that increases with the milling time. These lattice parameters are bigger than that of the commercial alloy.

  2. Moessbauer spectroscopic evidence on the heme binding to the proximal histidine in unfolded carbonmonoxy myoglobin by guanidine hydrochloride

    Energy Technology Data Exchange (ETDEWEB)

    Harami, Taikan, E-mail: harami.taikan@jaea.go.jp [Japan Atomic Energy Agency (Japan); Kitao, Shinji; Kobayashi, Yasuhiro [Kyoto University, Research Reactor Institute (Japan); Mitsui, Takaya [Japan Atomic Energy Agency (Japan)

    2008-01-15

    The unfolded heme structure in myoglobin is controversial because of no chance of direct X-ray structure analyses. The unfolding of carbonmonoxy myoglobin (MbCO) by guanidine hydrochloride (GdnHCl) was studied by the Moessbauer spectroscopy. The spectra show the presence of a sort of spectrum in the unfolded MbCO, independent on the concentration of GdnHCl from 1 to 6 M and the increase of the fraction of unfolded MbCO, depending on the GdnHCl concentration. The isomer shift of the iron of heme in the unfolded MbCO was identified to be different from that of the native MbCO as the globin structure in Mb collapses under the unfolded conditions. This result and the existing related Moessbauer data proved that the heme in the unfolded MbCO may remain coordinated to the proximal histidine.

  3. Moessbauer studies of iron ore from East Awinat mountains in Libya

    Energy Technology Data Exchange (ETDEWEB)

    Ellid, M.S. [Tajoura Nucl. Res. Center, Tripoli (Libyan Arab Jamahiriya). Dept. of Phys. and Mater. Sci.; Fallagh, F. [Tajoura Nucl. Res. Center, Tripoli (Libyan Arab Jamahiriya). Dept. of Phys. and Mater. Sci.

    1994-11-01

    In this paper, we report studies of local and imported iron ores using the techniques of Moessbauer spectroscopy, X-ray diffraction, and chemical analysis. Results from Moessbauer spectroscopy and X-ray diffraction of the two ores indicate that the raw materials consist mainly of hematite with a magnetic field of 517 kOe. The d-spacings are consistent with {alpha}-Fe{sub 2}O{sub 3}. A series of reduction processes in an H{sub 2} environment at 410 C for the local ore was performed in order to understand the kinetics of reduction. The reduction was complete after 5 h and the spectra reveal only an {alpha}-Fe phase with a hyperfine magnetic field of 330 kOe. On the other hand, the reduced pellets, from Misratah`s Iron and Steel Factory (imported iron ore), reveal the presence of an additional phase. This phase was identified as {theta}-carbide with a magnetic field of 208 kOe and an isomer shift of 0.22 mm/s. (orig.)

  4. Spectral Analysis of Rare Earth Elements using Laser-Induced Breakdown Spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Martin, Madhavi Z [ORNL; Fox, Dr. Richard V [Idaho National Laboratory (INL); Miziolek, Andrzej W [United States Army Research Laboratory; DeLucia, Frank C [United States Army Research Laboratory; Andre, Nicolas O [ORNL

    2015-01-01

    There is growing interest in rapid analysis of rare earth elements (REEs) both due to the need to find new natural sources to satisfy increased demand in their use in various electronic devices, as well as the fact that they are used to estimate actinide masses for nuclear safeguards and nonproliferation. Laser-Induced Breakdown Spectroscopy (LIBS) appears to be a particularly well-suited spectroscopy-based technology to rapidly and accurately analyze the REEs in various matrices at low concentration levels (parts-per-million). Although LIBS spectra of REEs have been reported for a number of years, further work is still necessary in order to be able to quantify the concentrations of various REEs in real-world complex samples. LIBS offers advantages over conventional solution-based radiochemistry in terms of cost, analytical turnaround, waste generation, personnel dose, and contamination risk. Rare earth elements of commercial interest are found in the following three matrix groups: 1) raw ores and unrefined materials, 2) as components in refined products such as magnets, lighting phosphors, consumer electronics (which are mostly magnets and phosphors), catalysts, batteries, etc., and 3) waste/recyclable materials (aka e-waste). LIBS spectra for REEs such as Gd, Nd, and Sm found in rare earth magnets are presented.

  5. Spectral Analysis of Rare Earth Elements using Laser-Induced Breakdown Spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Martin, Madhavi Z [ORNL; Fox, Dr. Richard V [Idaho National Laboratory (INL); Miziolek, Andrzej W [United States Army Research Laboratory; DeLucia, Frank C [United States Army Research Laboratory; Andre, Nicolas O [ORNL

    2015-01-01

    There is growing interest in rapid analysis of rare earth elements (REEs) both due to the need to find new natural sources to satisfy increased demand in their use in various electronic devices, as well as the fact that they are used to estimate actinide masses for nuclear safeguards and nonproliferation. Laser-Induced Breakdown Spectroscopy (LIBS) appears to be a particularly well-suited spectroscopy-based technology to rapidly and accurately analyze the REEs in various matrices at low concentration levels (parts-per-million). Although LIBS spectra of REEs have been reported for a number of years, further work is still necessary in order to be able to quantify the concentrations of various REEs in realworld complex samples. LIBS offers advantages over conventional solution-based radiochemistry in terms of cost, analytical turnaround, waste generation, personnel dose, and contamination risk. Rare earth elements of commercial interest are found in the following three matrix groups: 1) raw ores and unrefined materials, 2) as components in refined products such as magnets, lighting phosphors, consumer electronics (which are mostly magnets and phosphors), catalysts, batteries, etc., and 3) waste/recyclable materials (aka e-waste). LIBS spectra for REEs such as Gd, Nd, and Sm found in rare earth magnets are presented.

  6. Spectral Analysis of Rare Earth Elements using Laser-Induced Breakdown Spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Madhavi Z. Martin; Robert V. Fox; Andrzej W. Miziolek; Frank C. DeLucia, Jr.; Nicolas Andre

    2001-05-01

    There is growing interest in rapid analysis of rare earth elements (REEs) both due to the need to find new natural sources to satisfy increased demand in their use in various electronic devices, as well as the fact that they are used to estimate actinide masses for nuclear safeguards and nonproliferation. Laser-Induced Breakdown Spectroscopy (LIBS) appears to be a particularly well-suited spectroscopy-based technology to rapidly and accurately analyze the REEs in various matrices at low concentration levels (parts-per-million). Although LIBS spectra of REEs have been reported for a number of years, further work is still necessary in order to be able to quantify the concentrations of various REEs in realworld complex samples. LIBS offers advantages over conventional solution-based radiochemistry in terms of cost, analytical turnaround, waste generation, personnel dose, and contamination risk. Rare earth elements of commercial interest are found in the following three matrix groups: 1) raw ores and unrefined materials, 2) as components in refined products such as magnets, lighting phosphors, consumer electronics (which are mostly magnets and phosphors), catalysts, batteries, etc., and 3) waste/recyclable materials (aka e-waste). LIBS spectra for REEs such as Gd, Nd, and Sm found in rare earth magnets are presented.

  7. The Mission Accessible Near-Earth Objects Survey (MANOS): spectroscopy results

    Science.gov (United States)

    Thomas, Cristina A.; Moskovitz, Nicholas; Hinkle, Mary L.; Mommert, Michael; Polishook, David; Thirouin, Audrey; Binzel, Richard; Christensen, Eric J.; DeMeo, Francesca E.; Person, Michael J.; Trilling, David E.; Willman, Mark; Burt, Brian

    2016-10-01

    The Mission Accessible Near-Earth Object Survey (MANOS) is an ongoing physical characterization survey to build a large, uniform catalog of physical properties including lightcurves and visible wavelength spectroscopy. We will use this catalog to investigate the global properties of the small NEO population and identify individual objects that can be targets of interest for future exploration. To accomplish our goals, MANOS uses a wide variety of telescopes (1-8m) in both the northern and southern hemispheres. We focus on targets that have been recently discovered and operate on a regular cadence of remote and queue observations to enable rapid characterization of small NEOs. Targets for MANOS are selected based on three criteria: mission accessibility, size, and observability. With our resources, we observe 5-10 newly discovered sub-km NEOs per month. MANOS has been operating for three years and we have observed over 500 near-Earth objects in that time.We will present results from the spectroscopy component of the MANOS program. Visible wavelength spectra are obtained using DeVeny on the Discovery Channel Telescope (DCT), Goodman on the Southern Astrophysical Research (SOAR) telescope, and GMOS on Gemini North and South. Over 300 NEO spectra have been obtained during our program. We will present preliminary results from our spectral sample. We will discuss the compositional diversity of the small NEO population and how the observed NEOs compare to the meteorite population.MANOS is funded by the NASA Near-Earth Object Observations program.

  8. Moessbauer spectra of tin in float glass

    Energy Technology Data Exchange (ETDEWEB)

    Johnson, J.A. [Liverpool John Moores Univ. (United Kingdom). Sch. of the Built Environ.; Johnson, C.E. [Liverpool Univ. (United Kingdom). Dept. of Physics; Williams, K.F.E. [Liverpool Univ. (United Kingdom). Dept. of Physics; Holland, D. [Warwick Univ., Coventry (United Kingdom). Dept. of Physics; Karim, M.M. [Warwick Univ., Coventry (United Kingdom). Dept. of Physics

    1995-03-01

    Tin is not a major constituent of window glass, but is found at high concentrations in the lower surface of float glass which has been in contact with the molten tin bath. It does not extend far into the surface, but causes the physical and chemical behaviour to differ from that of the upper surface. It is important, therefore, to understand the structural role of tin in silicate glasses and thus its effect on various properties. Moessbauer spectra were taken of three series of glassy materials, namely binary glasses (SnO and SiO{sub 2}) in varying proportions, re-melted float glass containing tin, and float glass from a production plant. The binary glasses contained between 20 and 70% tin which was found to be mainly Sn{sup 2+}, with very small amounts of Sn{sup 4+} in some of them. The spectra showed a small decrease in isomer shift with increase in tine content, which is ascribed to the change in molar volume. The re-melted samples were float glass which was mixed with stannous oxalate in appropriate conditions to try and maintain tin in the 2+ state, and contained up to 15% tin by weight. The spectra show both Sn{sup 4+} and Sn{sup 2+} with rather more in the 4+ oxidation state. The change in the spectra as a function of temperature revealed a large difference in the f-factor (and hence the chemical binding) of the two states. A series of spectra was taken between 17.5 and 900 K for the sample containing 15% tin. From the absorption as a function of temperature the f-factor was determined for both oxidation states, and hence enabled the relative amounts of Sn{sup 4+} and Sn{sup 2+} present in each sample to be estimated. Measurements of the shift as a function of temperature were also made. The float samples were surface material produced by grinding away all but 0.1 mm of the lower surface of industrially produced float glass. The Moessbauer spectra showed them to be predominantly Sn{sup 2+}, as expected from the reducing atmosphere in the float plant.

  9. Hubble Space Telescope Near-IR Transmission Spectroscopy of the Super-Earth HD 97658b

    CERN Document Server

    Knutson, Heather A; Kreidberg, Laura; Kempton, Eliza M -R; McCullough, P R; Fortney, Jonathan J; Bean, Jacob L; Gillon, Michael; Homeier, Derek; Howard, Andrew W

    2014-01-01

    Recent results from the Kepler mission indicate that super-Earths (planets with masses between 1-10 times that of the Earth) are the most common kind of planet around nearby Sun-like stars. These planets have no direct solar system analogue, and are currently one of the least well-understood classes of extrasolar planets. Many super-Earths have average densities that are consistent with a broad range of bulk compositions, including both water-dominated worlds and rocky planets covered by a thick hydrogen and helium atmosphere. Measurements of the transmission spectra of these planets offer the opportunity to resolve this degeneracy by directly constraining the scale heights and corresponding mean molecular weights of their atmospheres. We present Hubble Space Telescope near-infrared spectroscopy of two transits of the newly discovered transiting super-Earth HD 97658b. We use the Wide Field Camera 3's scanning mode to measure the wavelength-dependent transit depth in thirty individual bandpasses. Our averaged ...

  10. Infrared spectroscopy of rare-earth-doped CaFe2As2

    Science.gov (United States)

    Xing, Zhen; Huffman, T. J.; Xu, Peng; Qazilbash, M. M.; Saha, S. R.; Drye, Tyler; Paglione, J.

    2014-03-01

    Recently, rare-earth doping in CaFe2As2 has been used to tune its electronic, magnetic, and structural properties. The substitution of rare-earth ions at the alkaline-earth sites leads to the suppression of the spin-density wave (SDW) phase transition in CaFe2As2. For example, Pr substitution results in a paramagnetic metal in the tetragonal phase that is susceptible to a low temperature structural transition to a collapsed tetragonal phase. However, La-doped CaFe2As2 remains in the uncollapsed tetragonal structure down to the lowest measured temperatures. Both the uncollapsed and collapsed tetragonal structures exhibit superconductivity with maximum Tc reaching 47 K, the highest observed in inter-metallics albeit with a small superconducting volume fraction. In this work, we perform ab-plane infrared spectroscopy of rare-earth-doped CaFe2As2 at different cryogenic temperatures. Our aim is to ascertain the contributions of electron doping and chemical pressure to the charge and lattice dynamics of this iron-arsenide system.

  11. The Effects of Refraction on Transit Transmission Spectroscopy: Application to Earth-like Exoplanets

    CERN Document Server

    Misra, Amit; Crisp, Dave

    2014-01-01

    We quantify the effects of refraction in transit transmission spectroscopy on spectral absorption features and on temporal variations that could be used to obtain altitude-dependent spectra for planets orbiting stars of different stellar types. We validate our model against altitude-dependent transmission spectra of the Earth from ATMOS and against lunar eclipse spectra from Palle et al. (2009). We perform detectability studies to show the potential effects of refraction on hypothetical observations of Earth analogs with the James Webb Space Telescope (JWST) Near-Infrared Spectrograph (NIRSPEC). Due to refraction, there will be a maximum tangent pressure level that can be probed during transit for each given planet-star system. We show that because of refraction, for an Earth-analog planet orbiting in the habitable zone of a Sun-like star only the top 0.3 bars of the atmosphere can be probed, leading to a decrease in the signal to noise ratio (SNR) of absorption features by 60%, while for an Earth-analog plan...

  12. Decay spectroscopy of neutron-rich rare-earth isotopes and collectivity around double midshell

    Energy Technology Data Exchange (ETDEWEB)

    Watanabe, Hiroshi, E-mail: hiroshi@ribf.riken.jp [IRCNPC, School of Physics and Nuclear Energy Engineering, Beihang University, Beijing 100191 (China); RIKEN Nishina Center, 2-1 Hirosawa, Wako, Saitama 351-0198 (Japan)

    2015-10-15

    Neutron-rich rare-earth isotopes with A ≈ 170, which locate near the middle of the major shells for both proton and neutron between the doubly magic nuclei {sup 132}Sn and {sup 208}Pb, have been investigated by means of decay spectroscopy techniques at the RIBF facility at RIKEN. The nuclei of interest were produced by in-flight fission of a high-intensity {sup 238}U beam at 345 MeV/u. In this contribution, scientific motivations, the details of experimental procedures, and some prospects of the data analysis are reported.

  13. Laser spectroscopy of rare earth ions in lead borate glasses and transparent glass-ceramics

    Science.gov (United States)

    Pisarski, W. A.; Grobelny, Ł.; Pisarska, J.; Lisiecki, R.; Dominiak-Dzik, G.; Ryba-Romanowski, W.

    2010-03-01

    Rare earth doped lead borate glasses and transparent glass-ceramics have been studied using optical spectroscopy. Based on the absorption, emission and its decay and the Judd-Ofelt calculations, several radiative and laser parameters for Ln 3+ ( Ln = Pr, Nd, Eu, Dy, Er, Tm) were evaluated. The large values of luminescence lifetime, quantum efficiency of excited state and room temperature peak stimulated emission cross-section suggest efficient laser transitions of Ln 3+ ions in lead borate glasses. The obtained results indicate that lead borate glasses and glass-ceramics containing Ln 3+ ions are promising host matrices for solid-state laser applications.

  14. Doppler spectroscopy as a path to the detection of Earth-like planets.

    Science.gov (United States)

    Mayor, Michel; Lovis, Christophe; Santos, Nuno C

    2014-09-18

    Doppler spectroscopy was the first technique used to reveal the existence of extrasolar planetary systems hosted by solar-type stars. Radial-velocity surveys led to the detection of a rich population of super-Earths and Neptune-type planets. The numerous detected systems revealed a remarkable diversity. Combining Doppler measurements with photometric observations of planets transiting their host stars further provides access to the planet bulk density, a first step towards comparative exoplanetology. The development of new high-precision spectrographs and space-based facilities will ultimately lead us to characterize rocky planets in the habitable zone of our close stellar neighbours.

  15. The effects of refraction on transit transmission spectroscopy: application to Earth-like exoplanets

    Energy Technology Data Exchange (ETDEWEB)

    Misra, Amit; Meadows, Victoria [Astronomy Department, University of Washington, Box 351580, Seattle, WA 98195 (United States); Crisp, Dave, E-mail: amit0@astro.washington.edu [NAI Virtual Planetary Laboratory, Seattle, WA (United States)

    2014-09-01

    We quantify the effects of refraction in transit transmission spectroscopy on spectral absorption features and on temporal variations that could be used to obtain altitude-dependent spectra for planets orbiting stars of different stellar types. We validate our model against altitude-dependent transmission spectra of the Earth from ATMOS and against lunar eclipse spectra from Pallé et al. We perform detectability studies to show the potential effects of refraction on hypothetical observations of Earth analogs with the James Webb Space Telescope NIRSPEC. Due to refraction, there will be a maximum tangent pressure level that can be probed during transit for each given planet-star system. We show that because of refraction, for an Earth-analog planet orbiting in the habitable zone of a Sun-like star only the top 0.3 bars of the atmosphere can be probed, leading to a decrease in the signal-to-noise ratio (S/N) of absorption features by 60%, while for an Earth-analog planet orbiting in the habitable zone of an M5V star it is possible to probe almost the entire atmosphere with minimal decreases in S/N. We also show that refraction can result in temporal variations in the transit transmission spectrum which may provide a way to obtain altitude-dependent spectra of exoplanet atmospheres. Additionally, the variations prior to ingress and subsequent to egress provide a way to probe pressures greater than the maximum tangent pressure that can be probed during transit. Therefore, probing the maximum range of atmospheric altitudes, and in particular the near-surface environment of an Earth-analog exoplanet, will require looking at out-of-transit refracted light in addition to the in-transit spectrum.

  16. Structure and spectroscopy of rare earth – Doped lead phosphate glasses

    Energy Technology Data Exchange (ETDEWEB)

    Pisarski, Wojciech A., E-mail: wojciech.pisarski@us.edu.pl [University of Silesia, Institute of Chemistry, Szkolna 9, 40-007 Katowice (Poland); Żur, Lidia [University of Silesia, Institute of Chemistry, Szkolna 9, 40-007 Katowice (Poland); Goryczka, Tomasz [University of Silesia, Institute of Materials Science, Bankowa 12, 40-007 Katowice (Poland); Sołtys, Marta; Pisarska, Joanna [University of Silesia, Institute of Chemistry, Szkolna 9, 40-007 Katowice (Poland)

    2014-02-25

    Highlights: • Lead phosphate glasses doped with rare earth ions were prepared. • The local structure was examined using X-ray diffraction and spectroscopic methods. • Different structural phosphate groups are present in lead phosphate glasses. • The electron–phonon coupling strength and phonon energy of the glass host was determined. • Several observed emission bands are due to 4f–4f electronic transitions of rare earth ions. -- Abstract: Lead–gallium phosphate glasses doped with rare the earth ions (Eu{sup 3+}, Dy{sup 3+}, Tb{sup 3+}, Er{sup 3+}) were synthesized. The structure of obtained glasses was examined by means of use: X-ray diffraction (XRD), nuclear magnetic resonance ({sup 207}Pb and {sup 31}P NMR), fourier transform infrared (FT-IR) and Raman spectroscopy. In contrast to fully amorphous Ln-doped samples (Ln = Eu, Dy, Tb), in Er-doped sample the GaPO{sub 4} crystalline phase was identified. It was found from the NMR, FT-IR and Raman spectroscopic techniques that, different structural phosphate groups were present in lead phosphate glasses. Based on absorption measurements, the UV–VIS cut-off wavelength for lead phosphate glass was determined and its value is close to 305 nm. Excitation and emission spectra of rare earths were also detected. From excitation spectra of Eu{sup 3+} the electron–phonon coupling strength and phonon energy of the glass host were determined. Due to 4f{sup 6}–4f{sup 6} (Eu{sup 3+}), 4f{sup 8}–4f{sup 8} (Tb{sup 3+}), 4f{sup 9}–4f{sup 9} (Dy{sup 3+}) and 4f{sup 11}–4f{sup 11} (Er{sup 3+}) electronic transitions of trivalent rare earth ions several luminescence bands were stated.

  17. Hubble space telescope near-ir transmission spectroscopy of the super-Earth HD 97658B

    Energy Technology Data Exchange (ETDEWEB)

    Knutson, Heather A. [Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125 (United States); Dragomir, Diana [Las Cumbres Observatory Global Telescope Network, Goleta, CA 93117 (United States); Kreidberg, Laura; Bean, Jacob L. [Department of Astronomy and Astrophysics, University of Chicago, Chicago, IL 60637 (United States); Kempton, Eliza M.-R. [Department of Physics, Grinnell College, Grinnell, IA 50112 (United States); McCullough, P. R. [Space Telescope Science Institute, Baltimore, MD 21218 (United States); Fortney, Jonathan J. [Department of Astronomy and Astrophysics, University of California, Santa Cruz, CA 95064 (United States); Gillon, Michael [Institut d' Astrophysique et de Géophysique, Universiteé de Liége, Liége 1 (Belgium); Homeier, Derek [Centre de Recherche Astrophysique de Lyon, F-69364 Lyon (France); Howard, Andrew W., E-mail: hknutson@caltech.edu [Institute for Astronomy, University of Hawaii at Manoa, Honolulu, HI 96822 (United States)

    2014-10-20

    Recent results from the Kepler mission indicate that super-Earths (planets with masses between 1-10 times that of the Earth) are the most common kind of planet around nearby Sun-like stars. These planets have no direct solar system analogue, and are currently one of the least well-understood classes of extrasolar planets. Many super-Earths have average densities that are consistent with a broad range of bulk compositions, including both water-dominated worlds and rocky planets covered by a thick hydrogen and helium atmosphere. Measurements of the transmission spectra of these planets offer the opportunity to resolve this degeneracy by directly constraining the scale heights and corresponding mean molecular weights of their atmospheres. We present Hubble Space Telescope near-infrared spectroscopy of two transits of the newly discovered transiting super-Earth HD 97658b. We use the Wide Field Camera 3's (WFC3) scanning mode to measure the wavelength-dependent transit depth in 30 individual bandpasses. Our averaged differential transmission spectrum has a median 1σ uncertainty of 23 ppm in individual bins, making this the most precise observation of an exoplanetary transmission spectrum obtained with WFC3 to date. Our data are inconsistent with a cloud-free solar metallicity atmosphere at the 10σ level. They are consistent at the 0.4σ level with a flat line model, as well as effectively flat models corresponding to a metal-rich atmosphere or a solar metallicity atmosphere with a cloud or haze layer located at pressures of 10 mbar or higher.

  18. Luminescence spectroscopy of rare earth-doped oxychloride lead borate glasses

    Energy Technology Data Exchange (ETDEWEB)

    Pisarski, Wojciech A., E-mail: Wojciech.Pisarski@us.edu.p [University of Silesia, Institute of Chemistry, Szkolna 9, 40-007 Katowice (Poland); Pisarska, Joanna [University of Silesia, Institute of Chemistry, Szkolna 9, 40-007 Katowice (Poland); Lisiecki, RadosLaw [Institute of Low Temperature and Structure Research, Polish Academy of Sciences, Okolna 2, 50-422 WrocLaw (Poland); Grobelny, Lukasz [University of Silesia, Institute of Chemistry, Szkolna 9, 40-007 Katowice (Poland); Dominiak-Dzik, Grazyna; Ryba-Romanowski, Witold [Institute of Low Temperature and Structure Research, Polish Academy of Sciences, Okolna 2, 50-422 WrocLaw (Poland)

    2011-04-15

    Ln-doped oxychloride lead borate glasses were studied using luminescence spectroscopy. Rare earth ions were limited to trivalent Pr{sup 3+}, Tm{sup 3+}, Eu{sup 3+} and Er{sup 3+}. Luminescence spectra were registered, which correspond to {sup 3}P{sub 0}-{sup 3}H{sub 4} and {sup 1}D{sub 2}-{sup 3}H{sub 4} transitions of Pr{sup 3+}, {sup 1}G{sub 4}-{sup 3}H{sub 5} and {sup 1}G{sub 4}-{sup 3}F{sub 4} transitions of Tm{sup 3+}, {sup 5}D{sub 0}-{sup 7}F{sub J} (J=0, 1, 2, 3, 4) transitions of Eu{sup 3+} and {sup 4}S{sub 3/2},{sup 2}H{sub 11/2}-{sup 4}I{sub 15/2} and {sup 4}I{sub 13/2}-{sup 4}I{sub 15/2} transitions of Er{sup 3+}. Luminescence decays from the excited states of Ln{sup 3+} ions were analyzed in detail. The experimental results indicate that relatively high phonon energy of the host gives important contribution to the excited state relaxation of rare earth ions. - Research Highlights: {yields}Lead borate glasses modified by PbCl{sub 2} were synthesized. {yields}Luminescence of Pr{sup 3+}, Tm{sup 3+}, Eu{sup 3+} and Er{sup 3+} ions in multicomponent oxychloride glasses was registered. {yields}From decay curves luminescence lifetimes for the excited states of rare earth ions were determined. {yields}The relatively high phonon energy of the host gives important contribution to the excited state relaxation of rare earth ions.

  19. TWINKLE - A Low Earth Orbit Visible and Infrared Exoplanet Spectroscopy Observatory

    Science.gov (United States)

    Tessenyi, Marcell; Savini, Giorgio; Tinetti, Giovanna; Tennyson, Jonathan; Dhesi, Mekhi; Joshua, Max

    2016-10-01

    Twinkle is a space mission designed for visible and near-IR spectroscopic observations of extrasolar planets. Twinkle's highly stable instrument will allow the photometric and spectroscopic observation of a wide range of planetary classes around different types of stars, with a focus on bright sources close to the ecliptic. The planets will be observed through transit and eclipse photometry and spectroscopy, as well as phase curves, eclipse mapping and multiple narrow-band time-series. The targets observed by Twinkle will be composed of known exoplanets mainly discovered by existing and upcoming ground surveys in our galaxy and will also feature new discoveries by space observatories (K2, GAIA, Cheops, TESS).Twinkle is a small satellite with a payload designed to perform high-quality astrophysical observations while adapting to the design of an existing Low Earth Orbit commercial satellite platform. The SSTL-300 bus, to be launched into a low-Earth sun-synchronous polar orbit by 2019, will carry a half-meter class telescope with two instruments (visible and near-IR spectrographs - between 0.4 and 4.5µm - with resolving power R~300 at the lower end of the wavelength scale) using mostly flight proven spacecraft systems designed by Surrey Satellite Technology Ltd and a combination of high TRL instrumentation and a few lower TRL elements built by a consortium of UK institutes.The Twinkle design will enable the observation of the chemical composition and weather of at least 100 exoplanets in the Milky Way, including super-Earths (rocky planets 1-10 times the mass of Earth), Neptunes, sub-Neptunes and gas giants like Jupiter. It will also allow the follow-up photometric observations of 1000+ exoplanets in the visible and infrared, as well as observations of Solar system objects, bright stars and disks.

  20. TWINKLE - A Low Earth Orbit Visible and Infrared Exoplanet Spectroscopy Observatory

    Science.gov (United States)

    Tessenyi, M.; Savini, G.; Tinetti, G.; Tennyson, J.; Dhesi, M.; Joshua, M.

    2017-07-01

    Twinkle is a space mission designed for visible and near-IR spectroscopic observations of extrasolar planets. Twinkle's highly stable instrument will allow the photometric and spectroscopic observation of a wide range of planetary classes around different types of stars, with a focus on bright sources close to the ecliptic. The planets will be observed through transit and eclipse photometry and spectroscopy, as well as phase curves, eclipse mapping and multiple narrow-band time-series. The targets observed by Twinkle will be composed of known exoplanets mainly discovered by existing and upcoming ground surveys in our galaxy and will also feature new discoveries by space observatories (K2, GAIA, Cheops, TESS). Twinkle is a small satellite with a payload designed to perform high-quality astrophysical observations while adapting to the design of an existing Low Earth Orbit commercial satellite platform. The SSTL-300 bus, to be launched into a low-Earth sun-synchronous polar orbit by 2019, will carry a half-meter class telescope with two instruments (visible and near-IR spectrographs - between 0.4 and 4.5μm - with resolving power R˜300 at the lower end of the wavelength scale) using mostly flight proven spacecraft systems designed by Surrey Satellite Technology Ltd and a combination of high TRL instrumentation and a few lower TRL elements built by a consortium of UK institutes. The Twinkle design will enable the observation of the chemical composition and weather of at least 100 exoplanets in the Milky Way, including super-Earths (rocky planets 1-10 times the mass of Earth), Neptunes, sub-Neptunes and gas giants like Jupiter. It will also allow the follow-up photometric observations of 1000+ exoplanets in the visible and infrared, as well as observations of Solar system objects, bright stars and disks.

  1. Diagnostic Comparisons of Near-Earth Object Identification using Slit Spectroscopy and Slitless Grating Methods

    Science.gov (United States)

    Ryan, E.; Ryan, W.

    2014-09-01

    Space object identification and characterization is an important component of Space Situational Awareness (SSA). Through an Air Force collaboration that has provided a visible wavelength, low-resolution spectrometer, researchers at the Magdalena Ridge Observatory 2.4-meter telescope (located in New Mexico) have been investigating the advantages and disadvantages of using slit spectroscopy versus slitless grating methods to characterize artificial Earth-orbiting objects. The objective is to develop a method that returns useful diagnostic information with a minimal investment in observational monitoring time. However, spectral measurements are a desirable component of characterization studies of natural objects in near-Earth orbit as well. Therefore, in 2012, we began to extend this instrumentation beyond its SSA applications to the study of Near-Earth asteroids (NEAs). The typical lifetimes of NEAs are up to three orders of magnitude shorter than the typical timescales associated with the main asteroid belt. Therefore, the current NEA population is a relatively recent product that has to be continually re-supplied. Spectroscopic analysis of NEAs helps characterize their taxonomic distribution and identify potential source regions which would then enhance our understanding of the origin of the current population. Although this is of interest scientifically, it can also help estimate the magnitude of the hazard threat from still undiscovered asteroids as well as provide guidance to optimize ground-based telescope search strategies. Slit-based spectroscopy is time consuming and has limitations on how faint an object can be studied. Therefore, the goal of this current project is to determine whether a lower resolution (by a factor of 10 with respect to the slit-based spectrometer), readily available slitless grating is sufficient for rough taxonomic classification in the study of fainter target-of-opportunity NEAs. The grating provides spectral information in 20nm

  2. SEM, optical, and Moessbauer studies of submicrometer chromite in Allende

    Science.gov (United States)

    Housley, R. M.

    1982-01-01

    New scanning electron and optical microscope results are presented showing that sub-micrometer chromite is abundant along healed cracks and grain boundaries in Allende chondrule olivine. Some wider healed cracks also contain pentlandite and euhedral Ni3Fe grains. Also reported are Moessbauer measurements on Allende HF-HCl residues confirming a high Fe(+++)/Fe(++) ratio.

  3. Molecular dynamics in cytochrome c oxidase Moessbauer spectra deconvolution

    Energy Technology Data Exchange (ETDEWEB)

    Bossis, Fabrizio [Department of Medical Biochemistry, Medical Biology and Medical Physics (DIBIFIM), University of Bari ' Aldo Moro' , Bari (Italy); Palese, Luigi L., E-mail: palese@biochem.uniba.it [Department of Medical Biochemistry, Medical Biology and Medical Physics (DIBIFIM), University of Bari ' Aldo Moro' , Bari (Italy)

    2011-01-07

    Research highlights: {yields} Cytochrome c oxidase molecular dynamics serve to predict Moessbauer lineshape widths. {yields} Half height widths are used in modeling of Lorentzian doublets. {yields} Such spectral deconvolutions are useful in detecting the enzyme intermediates. -- Abstract: In this work low temperature molecular dynamics simulations of cytochrome c oxidase are used to predict an experimentally observable, namely Moessbauer spectra width. Predicted lineshapes are used to model Lorentzian doublets, with which published cytochrome c oxidase Moessbauer spectra were simulated. Molecular dynamics imposed constraints to spectral lineshapes permit to obtain useful information, like the presence of multiple chemical species in the binuclear center of cytochrome c oxidase. Moreover, a benchmark of quality for molecular dynamic simulations can be obtained. Despite the overwhelming importance of dynamics in electron-proton transfer systems, limited work has been devoted to unravel how much realistic are molecular dynamics simulations results. In this work, molecular dynamics based predictions are found to be in good agreement with published experimental spectra, showing that we can confidently rely on actual simulations. Molecular dynamics based deconvolution of Moessbauer spectra will lead to a renewed interest for application of this approach in bioenergetics.

  4. Magnetic frustration in ferric fluorides investigated by Moessbauer spectrometry

    Energy Technology Data Exchange (ETDEWEB)

    Greneche, J.-M. [UPRESA CNRS 6087, Faculte des Sciences, Universite du Maine, Laboratoire de Physique de l' Etat Condense (France)

    1999-11-15

    The origin of magnetic frustration in antiferromagnetic ionic systems is discussed in terms first of cationic topology and then of competing superexchange and supersuperexchange interactions. Some selected examples based on ferric fluorides and oxyfluorides are presented to illustrate both the origins of magnetic frustration and the contribution of zero-field and in-field Moessbauer experiments.

  5. Moessbauer thermal scan study of a spin crossover system

    Energy Technology Data Exchange (ETDEWEB)

    Zelis, P Mendoza; Pasquevich, G A; Sanchez, F H; Veiga, A; Cabrera, A F [Departamento de Fisica, FCE-UNLP, La Plata (Argentina); Ceolin, M [Instituto de Investigaciones FIsico-Quimicas Teoricas y Aplicadas (UNLP-CONICET), La Plata (Argentina); Coronado-Miralles, E; Monrabal-Capilla, M; Galan-Mascaros, J R, E-mail: pmendoza@fisica.unlp.edu.a [Instituto de Ciencias Moleculares, Universidad de Valencia, Valencia (Spain)

    2010-03-01

    Programmable Velocity equipment was used to perform a Moessbauer Thermal Scans to allow a quasi-continuous temperature study of the magnetic transition between the low-spin and a high-spin configurations in [Fe(Htrz){sub 2}(trz)](BF4) system. The material was studied both in bulk as in nanoparticles sample forms.

  6. Application of Moessbauer Spectroscopy to the Carbon Oxides Hydrogenation Reactions

    Energy Technology Data Exchange (ETDEWEB)

    Cubeiro, M. L. [UCV, Centro de Catalisis, Petroleo y Petroquimica, Escuela de Quimica (Venezuela, Bolivarian Republic of)], E-mail: mcubeiro@strix.ciens.ucv.ve; Gonzalez-Jimenez, F.; Goldwasser, M. R.; Perez-Zurita, M. J.; Pietri, E.; Garcia, L. [Centro de Catalisis, Petroleo y Petroquimica, Escuela de Quimica, UCV (Venezuela, Bolivarian Republic of)

    2001-05-15

    Iron-based catalysts have favorable activity and selectivity properties for the CO and CO{sub 2} hydrogenation reactions. Several Fe phases (oxides and carbides) can be present in these catalysts. The interaction of Fe with the other components of the catalyst (support, promoters) can affect the ease of reduction and also its transformation during the reactions. In this work, the relationship between catalytic behavior in the CO and CO{sub 2} hydrogenation reactions and the Fe phase composition of fresh and reacted catalysts was studied. Two types of catalysts were tested: a laterite and the other one made of iron supported on alumina, both unpromoted and promoted with K and Mn. Only those Fe species which can be reduced-carburized, by means of a pretreatment or by an in situ transformation under the reaction, seem to be able to perform the CO or CO{sub 2} hydrogenation. The reoxidation of the Fe carbide to magnetite was not associated to deactivation. The selectivity seems to be more affected by Fe species difficult to reduce than by magnetite produced by reoxidation.

  7. Observation of Kondo resonance in rare-earth hexaborides using high resolution photoemission spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Maiti, Kalobaran; Patil, Swapnil; Adhikary, Ganesh [Department of Condensed Matter Physics and Materials Science, Tata Institute of Fundamental Research, Homi Bhabha Road, Colaba, Mumbai 400005 (India); Balakrishnan, Geetha, E-mail: kbmaiti@tifr.res.in [Department of Physics, University of Warwick, Coventry, CV4 7AL (United Kingdom)

    2011-01-01

    We studied the electronic structure of rare earth hexaborides, CeB{sub 6}, PrB{sub 6} and NdB{sub 6} using state-of-the-art high resolution photoemission spectroscopy. CeB{sub 6} is a dense Kondo system. PrB{sub 6} and NdB{sub 6} are antiferromagnetic (Neel temperature {approx}7 K), known to be stable moment systems and do not exhibit Kondo effect. Photoemission spectra exhibit distinct signature of surface and bulk electronic structures of these compounds. The energy position of the surface feature is not influenced by the 4f density of states. High resolution spectra of CeB{sub 6} reveal multiple Kondo resonance features in the bulk spectra due to various photoemission final states. Interestingly, high resolution photoemission spectra of antiferromagnetic PrB{sub 6} also exhibit a sharp feature at the Fermi level that shows temperature dependence similar to the Kondo resonance features.

  8. Telling twins apart: Exo-Earths and Venuses with transit spectroscopy

    CERN Document Server

    Barstow, Joanna K; Irwin, Patrick G J; Kendrew, Sarah; Fletcher, Leigh N

    2016-01-01

    The planned launch of the James Webb Space Telescope in 2018 will herald a new era of exoplanet spectroscopy. JWST will be the first telescope sensitive enough to potentially characterize terrestrial planets from their transmission spectra. In this work, we explore the possibility that terrestrial planets with Venus-type and Earth-type atmospheres could be distinguished from each other using spectra obtained by JWST. If we find a terrestrial planet close to the liquid water habitable zone of an M5 star within a distance of 10 parsecs, it would be possible to detect atmospheric ozone if present in large enough quantities, which would enable an oxygen-rich atmosphere to be identified. However, the cloudiness of a Venus-type atmosphere would inhibit our ability to draw firm conclusions about the atmospheric composition, making any result ambiguous. Observing small, temperate planets with JWST requires significant investment of resources, with single targets requiring of order 100 transits to achieve sufficient s...

  9. Temperature dependence of the Moessbauer effect on the semiconductors Pb{sub 0.78}Sn{sub 0.22}Te and Pb{sub 0.80}Sn{sub 0.20}Te:In

    Energy Technology Data Exchange (ETDEWEB)

    Ragimova, T. [Universidad de Antioquia, A.A, Departamento de Fisica (Colombia); Pacheco Serrano, W.A. [Universidad Pedagogica y Tecnologica, A.A. 1094, Departamento de Fisica (Colombia); Abras, A. [Universidade Federal de Minas Gerais, Departamento de Fisica, ICEx (Brazil)

    1999-11-15

    Crystals of the semiconductors Pb{sub 0.78}Sn{sub 0.22}Te and Pb{sub 0.80}Sn{sub 0.20}Te:In were grown by Bridgman method, and investigated by Moessbauer spectroscopy and X-ray diffraction. Moessbauer spectra were taken at temperatures between 80 and 300 K. The absence of the quadrupole splitting shows a cubic symmetry of the environment for the tin atom, which is in accordance with X-ray data. The temperature dependence of the spectral area is discussed and the Debye temperature is estimated.

  10. On the electronic phase diagram of Ba{sub 1-x}K{sub x}(Fe{sub 1-y}Co{sub y}){sub 2}As{sub 2} and EuFe{sub 2}(As{sub 1-x}P{sub x}){sub 2} superconductors. A local probe study using Moessbauer spectroscopy and muon spin relaxation

    Energy Technology Data Exchange (ETDEWEB)

    Goltz, Til

    2015-10-28

    In this thesis, I study the electronic and structural phase diagrams of the superconducting 122 iron pnictides systems Ba{sub 1-x}K{sub x}(Fe{sub 1-y}Co{sub y}){sub 2}As{sub 2} and EuFe{sub 2}(As{sub 1-x}P{sub x}){sub 2} by means of the local probe techniques {sup 57}Fe Moessbauer spectroscopy (MS) and muon spin relaxation (μSR). For both isovalent substitution strategies - Co/K for Fe/Ba and P for As, respectively - the antiferromagnetic Fe ordering and orthorhombic distortion of the parent compounds BaFe{sub 2}As{sub 2} and EuFe{sub 2}As{sub 2} are subsequently suppressed with increasing chemical substitution and superconductivity arises, once long-range and coherent Fe magnetic order is sufficiently but not entirely suppressed. For Ba{sub 1-x}K{sub x}(Fe{sub 1-y}Co{sub y}){sub 2}As{sub 2} in the charge compensated state (x/2 ∼ y), a remarkably similar suppression of both, the orthorhombic distortion and Fe magnetic ordering, as a function of increasing substitution is observed and a linear relationship between the structural and the magnetic order parameter is found. Superconductivity is evidenced at intermediate substitution with a maximum T{sub SC} of 15 K coexisting with static magnetic order on a microscopic length scale. The appearance of superconductivity within the antiferromagnetic state can by explained by the introduction of disorder due to nonmagnetic impurities to a system with a constant charge carrier density. Within this model, the experimental findings are compatible with the predicted s{sup ±} pairing symmetry. For EuFe{sub 2}(As{sub 1-x}P{sub x}){sub 2}, the results from {sup 57}Fe MS and ZF-μSR reveal an intriguing interplay of the local Eu{sup 2+} magnetic moments and the itinerant magnetic Fe moments due to the competing structures of the iron and europium magnetic subsystems. For the investigated single crystals with x = 0.19 and 0.28, {sup 57}Fe MS evidences the interplay of Fe and Eu magnetism by the observation of a transferred

  11. Quantitative estimation of concentrations of dissolved rare earth elements using reflectance spectroscopy

    Science.gov (United States)

    Dai, Jingjing; Wang, Denghong; Wang, Runsheng; Chen, Zhenghui

    2013-01-01

    Characteristic spectral parameters such as the wavelength and depth of absorption bands are widely used to quantitatively estimate the composition of samples from hyperspectral reflectance data in soil science, mineralogy as well as vegetation study. However, little research has been conducted on the spectral characteristic of rare earth elements (REE) and their relationship with chemical composition of aqueous solutions. Reflectance spectra of ore leachate solutions and contaminated stream water from a few REE mines in the Jiangxi Province, China, are studied for the first time in this work. The results demonstrate that the six diagnostic absorption features of the rare earths are recognized in visible and near-infrared wavelengths at 574, 790, 736, 520, 861, and 443 nm. The intensity of each of these six absorption bands is linearly correlated with the abundance of total REE, with the r2 value >0.95 and the detection limit at ≥75,000 μg/L. It is suggested that reflectance spectroscopy provides an ideal routine analytical tool for characterizing leachate samples. The outcome of this study also has implications for monitoring the environmental effect of REE mining, in particular in stream water systems by hyperspectral remote sensing.

  12. An {sup 57}Fe Moessbauer study of three Australian L5 ordinary-chondrite meteorites: dating Kinclaven-001

    Energy Technology Data Exchange (ETDEWEB)

    Cadogan, J. M., E-mail: s.cadogan@adfa.edu.au [The University of New South Wales, School of Physical, Environmental and Mathematical Sciences (Australia); Rebbouh, L.; Mills, J. V. J. [University of Manitoba, Department of Physics and Astronomy (Canada); Bland, P. A. [Imperial College London, Impacts and Astromaterials Research Centre (IARC), Department of Earth Science and Engineering (United Kingdom)

    2013-12-15

    Three L5-type ordinary chondrite meteorites recovered from the Nullarbor Region of Western Australia were studied by {sup 57}Fe Moessbauer spectroscopy: Kinclaven-001, Camel Donga-007 and Gunnadorah-002. The relative amounts of the various Fe-bearing phases including the primary minerals (Olivine, Pyroxene, Troilite and Fe-Ni metal) and the ferric alteration products (Goethite, Maghemite/Magnetite) were obtained to determine the percentage of iron converted to Fe{sup 3 + } by weathering processes. These data allow us to estimate the terrestrial age of Kinclaven-001 at 1,700 {+-} 1,300 yrs.

  13. Moessbauer studies of one representative hydromorphic soil of the coastal area of the Rio de La Plata

    Energy Technology Data Exchange (ETDEWEB)

    Guichon, B. A. [Universidad Nacional de La Plata, Instituto de Geomorfologia y Suelos (Argentina); Desimoni, J.; Mercader, R. C., E-mail: mercader@fisica.unlp.edu.ar [Universidad Nacional de La Plata, Departamento de Fisica, IFLP-CONICET, Facultad de Ciencias Exactas (Argentina); Imbellone, P. A. [Universidad Nacional de La Plata, Instituto de Geomorfologia y Suelos (Argentina)

    2010-01-15

    In the present work, we have applied Moessbauer spectroscopy as well as the traditional chemical analyses to assess the contents of different states of Fe in oxides and hydroxides in an Entisol soil from the Argentine coastal plain of the Rio de La Plata. Tentative assignments for the different Fe ion sites are proposed. Our findings show that the isomer shift and quadrupole splitting are sensitive to the changes detected in the Fe{sup 2+} contents of the soluble phase while others remain constant within the experimental uncertainties.

  14. A Moessbauer and Electrochemical Characterization of the Corrosion Products Formed from Marine and Marine-Antartic Environments

    Energy Technology Data Exchange (ETDEWEB)

    Ohanian, M.; Caraballo, R.; Dalchiele, E. A.; Quagliata, E. [Instituto de Ingenieria Quimica, Facultad de Ingenieria (Uruguay)

    2003-06-15

    Corrosion products formed on low alloy steel under two marine environments are characterised. Both environments are classified as C4 according to the ISO 9223 Standard. The corrosion products are identified and their relative proportion is determined by Moessbauer spectroscopy (transmission geometry). Free potentials of corrosion are measured to evaluate the activity of their surfaces. Structural characterisation by XRD were performed on selected samples. It is concluded that the principal phases are goethite, lepidocrocite, ferrihidrite and maghemite. The relative amount of each of them changes with time and with the atmospheric dynamics of each environment.

  15. The origin of copiapite from chlorite pyritic schist (Wiesciszowice, Lower Silesia, Poland) in the light of Moessbauer analysis

    Energy Technology Data Exchange (ETDEWEB)

    Adamczyk, Z., E-mail: zdzislaw.adamczyk@polsl.pl [Silesian University of Technology, Institute of Applied Geology (Poland); Komraus, J. L., E-mail: komraus@us.edu.pl [University of Silesia, Institute of Physics (Poland)

    2008-01-15

    This work presents the results of the analysis of copiapite, formed from weathering and oxidation of pyrite in pyritic schist from Wiesciszowice, Lower Silesia (Poland). The pure phase of copiapite was found in secondary minerals after pyrite and identified by optical microscopy, XRD and Moessbauer spectroscopy. In the analyzed copiapite major cations appear to be Fe{sup 2+} and Fe{sup 3+}. Some Fe{sup 3+} is substituted by other cations, mainly Al{sup 3+}. Al{sup 3+} probably comes from leaching of chlorite from which hydrated sulphates of iron, mainly szomolnokite, form followed by hydrated sulphates fibroferrite, which is replaced by copiapite.

  16. Moessbauer Spectroscopic Studies of {sup 237}Np in frozen nitric acid solution

    Energy Technology Data Exchange (ETDEWEB)

    Nakada, M; Wang, J; Kitazawa, T; Takahashi, M; Takeda, M; Masaki, N M; Yamashita, T [Department of Materials Science, Japan Atomic Energy Research Institute (JAERI, present JAEA: Japan Atomic Energy Agency), Tokai, Naka, Ibaraki 319-1195 (Japan); Tsutsui, S, E-mail: wangjh@dicp.ac.c [Advanced Science Research Center, JAERI, Tokai, Naka, Ibaraki 319-1195 (Japan)

    2010-03-01

    We applied Moessbauer spectroscopy to {sup 237}Np in nitric acid solutions to study chemical states. Sample solutions were adjusted to 50 mg/ml of Np(V) and Np(VI) concentration in 0.6 M nitric acid solutions. These solutions were put into original designed containers for samples and mounted to sample holders. The values of isomer shift (IS, relative to NpAl{sub 2}) of Np(V) and Np(VI) in 0.6 M nitric acid were -17.4(1) and -37.2(3) mm/s at about 10 K, respectively. It was found that Np(V) had 7 coordination number and Np(VI) had 8 in nitric acid solutions from values of IS.

  17. Moessbauer study of the Ordinary-Chondrite meteorite Thylacine Hole-001

    Energy Technology Data Exchange (ETDEWEB)

    Cadogan, J. M., E-mail: cadogan@physics.umanitoba.ca [University of Manitoba, Department of Physics and Astronomy (Canada); Devlin, E. J. [NCSR Demokritos, Institute of Materials Science (Greece)

    2012-03-15

    The Thylacine Hole-001 meteorite was recovered from the Nullarbor Desert (Australia) in 1977 and is an Ordinary Chondrite, Group H4/5br, which has undergone moderate to severe (B/C) weathering. We have characterised the Fe-bearing phases in Thylacine Hole-001 by {sup 57}Fe Moessbauer Spectroscopy at 300 K, 100 K, 50 K and 4 K. The spectrum at 300 K is dominated by the paramagnetic doublets of Olivine, Pyroxene and a Ferric component which is most likely nanoparticulate Goethite. Magnetically split sextets due to Maghemite or Magnetite are also present, consistent with the relatively advanced terrrestrial age of 28,500 yrs The nanoparticulate Goethite component shows a blocked, magnetically split sextet at low temperatures. We also observe the effects of magnetic ordering of the Olivine and Pyroxene below 50 K.

  18. Moessbauer study of the Fe mineralogy in two different Argentine soils

    Energy Technology Data Exchange (ETDEWEB)

    Mijovilovich, A. [Departamento de Fisica, Comision Nacional de Energia Atomica (Argentina); Morras, H. [Instituto de Suelos, INTA-CIRN (Argentina); Causevic, H. [Universidad de Buenos Aires, Ciudad Universitaria, Facultad de Ciencias Exactas y Naturales (Argentina); Saragovi, C. [Departamento de Fisica, Comision Nacional de Energia Atomica (Argentina)

    1999-11-15

    Two Argentine soils featuring different characteristics and compositions (mollisols and ultisols) have been studied by Moessbauer spectroscopy and X-ray diffraction. The first type has a weakly developed profile with a solum thickness of 40 cm; the Fe oxyhydroxides are present in low concentrations in mixtures with other slightly weathered minerals (e.g., quartz, feldspars, 2 : 1 phyllosilicates, etc.). The second one is a typic kandihumult, which is a highly weathered red coloured, deep soil. The Fe oxyhydroxides are abundant, mixed mainly with kaolinite clay minerals. Analyses of iron mineralogy show hematite and goethite in both soils. Their ratio is low in the first case and high in the last case. Magnetite-maghemite are also present in both situations, but in the mollisol their content is much lower than in the ultisol. The mineralogy found is related to the different lithological characteristics and processes of pedological evolution on both soils.

  19. Iron-57 Moessbauer spectroscopic studies of the weathering of L-chondrite meteorites

    Energy Technology Data Exchange (ETDEWEB)

    Berry, F.J. [Open Univ., Milton Keynes (United Kingdom). Dept. of Chem.; Bland, P.A. [Open Univ., Milton Keynes (United Kingdom). Dept. of Earth Sciences; Oates, G. [Open Univ., Milton Keynes (United Kingdom). Dept. of Chem.; Pillinger, C.T. [Open Univ., Milton Keynes (United Kingdom). Dept. of Earth Sciences

    1994-11-01

    Some L-chondrite meteorites found in the arid desert region of Roosevelt County in New Mexico, USA, and {sup 14}C dated to determine the terrestrial age have been examined by {sup 57}Fe Moessbauer spectroscopy. The preliminary results reported here suggest that the initial weathering processes involve oxidation of iron in the iron-nickel alloy. After prolonged exposure to terrestrial weathering for approximately 36 000 years, the iron(II)-sulphide and -silicate phases are also oxidised. The corrosion products are complex and include paramagnetic Fe{sup 3+} species and macroscopic iron(III) oxide and/or oxyhydroxide phases. A meteorite which fell approximately 16 500 years ago at the end of the last glaciation showed extensive corrosion despite its relatively short terrestrial age. The result is associated with climatic changes which occurred at that time. (orig.)

  20. Moessbauer Study of Serpentine Minerals in the Ultramafic Body of Tehuitzingo, Southern Mexico

    Energy Technology Data Exchange (ETDEWEB)

    Gonzalez-Mancera, G., E-mail: ggm@servidor.unam.mx [Ciudad Universitaria, Facultad de Quimica, Circuito Exterior, Edif. ' D' (Mexico); Ortega-Gutierrez, F. [Ciudad Universitaria, Instituto de Geologia, Circuito Exterior (Mexico); Nava, N. E. [Instituto Mexicano del Petroleo (Mexico); Arriola, H. S. [Ciudad Universitaria, Facultad de Quimica, Circuito Exterior, Edif. ' D' (Mexico)

    2003-06-15

    Serpentine 'polymorph' minerals (chrysotile, lizardite, and antigorite) are hydrous Mg-Fe silicates that commonly form serpentine rock (serpentinite) by hydration of olivine-pyroxene peridotites from the mantle of the Earth. During the complex geologic history of orogenic belts, the redox and hydration state of the mantle changes, and olivine and pyroxenes are replaced by serpentine group minerals during tectonic deformation and uplift. Unfortunately, modern microanalysis of minerals by electron probe does not distinguish the oxidation state of iron, and it has to be assumed or estimated by precise methods, such as Moessbauer spectrometry. The studied samples were collected in the Xayacatlan Formation of the Tehuitzingo area, State of Puebla, within the Paleozoic Acatlan Complex. The original mantle peridotite was completely converted to serpentinite, with secondary crystallization of Fe-Mg oxides, calcsilicates, and carbonates. The three serpentine 'polymorphs' were identified in the studied samples, although with a clear predominance of the high-temperature member antigorite, which was preliminary determined by optical petrography, X-ray diffraction, electron probe, and scanning electron microscopy. Microprobe total iron content in most specimens was <2%, but some were higher. Principal substitutions involving ferrous and ferric iron in serpentine minerals occur in the octahedral site, but minor and infrequent Fe{sup +3} substitution at the tetrahedral site may also occur according to some Moessbauer studies. This paper studied the iron valence state and its position in serpentine minerals of the Tehuitzingo ultramafic body using Moessbauer techniques. The analyses in most samples detected one doublet, compatible with Fe{sup +2} in octahedral coordination, but only two specimens displayed two doublets corresponding to Fe{sup +2} and Fe{sup +3} in octahedral coordination. Doublets corresponding to Fe{sup +3} in tetrahedral sites were not found

  1. Moessbauer studies of impactites from Huamalies province in Huanuco Region

    Energy Technology Data Exchange (ETDEWEB)

    Bustamante, A., E-mail: abustamanted@unmsm.edu.pe; Espinoza, S. [San Marcos University, Faculty of Physical Sciences (Peru); Morales, G. [Museo de Historia Natural(Museum of Natural History) (Peru); Scorzelli, R. B. [Centro Brasileiro de Pesquisas Fisicas (Brazilian Center for Research in Physics) (Brazil)

    2005-11-15

    This report is about the X-ray diffraction and Moessbauer studies of three impactite samples denominated PMe-8, PMe-9 and PMe-11 from Huamalies Province in Huanuco Region, Peru. When terrestrial rocks are submitted to pressures higher than 60 GP, the majority is completely melted, forming a kind of glass called impactites. X-ray diffraction indicates the presence of quartz as the principal mineralogical phase in all samples. The {sup 57}Fe Moessbauer spectra at room temperature of samples PMe-8 and PMe-9 show broadened spectra that were fitted using a distribution model. The most probable field of the magnetic component is 34 T, corresponding to the presence of small particles of goethite, confirmed by the 4.2 K spectrum. For the sample PMe-11, the MS showed the presence of well crystallized hematite.

  2. Moessbauer study of carbon coated iron magnetic nanoparticles produced by simultaneous reduction/pyrolysis

    Energy Technology Data Exchange (ETDEWEB)

    Mendonca, Fernanda G. [Universidade Federal de Minas Gerais, Departamento de Quimica - ICEx (Brazil); Ardisson, Jose D. [CDTN, Laboratorio de Fisica Aplicada, Centro de Desenvolvimento de Tecnologia Nuclear (Brazil); Rosmaninho, Marcelo G.; Lago, Rochel M.; Tristao, Juliana C., E-mail: juliana@ufv.br [Universidade Federal de Minas Gerais, Departamento de Quimica - ICEx (Brazil)

    2011-11-15

    Magnetic iron nanoparticles immersed in a carbon matrix were produced by a combined process of controlled dispersion of Fe{sup 3 + } ions in sucrose, thermal decomposition with simultaneous reduction of iron cores and the formation of the porous carbonaceous matrix. The materials were prepared with iron contents of 1, 4 and 8 in %wt in sucrose and heated at 400, 600 and 800 Degree-Sign . The samples were analyzed by XRD, Moessbauer spectroscopy, magnetization measurements, TG, SEM and TEM. The materials prepared at 400 Degree-Sign are composed essentially of Fe{sub 3}O{sub 4} particles and carbon, while treatments at higher temperatures, e.g. 600 and 800 Degree-Sign produced as main phases Fe{sup 0} and Fe{sub 3}C. The Moessbauer spectra of samples heated at 400 Degree-Sign showed two sextets characteristic of a magnetite phase and other contributions compatible with Fe{sup 3 + } and Fe{sup 2 + } phases in a carbonaceous matrix. Samples treated at temperatures above 600 Degree-Sign showed the presence of metallic iron with concentrations between 16-43%. The samples heated at 800 Degree-Sign produced higher amounts of Fe{sub 3}C (between 20% and 58%). SEM showed for the iron 8% sample treated at 600-800 Degree-Sign C particle sizes smaller than 50 nm. Due to the presence of Fe{sup 0} particles in the carbonaceous porous matrix the materials have great potential for application as magnetic adsorbents.

  3. Earth

    CERN Document Server

    Carter, Jason

    2017-01-01

    This curriculum-based, easy-to-follow book teaches young readers about Earth as one of the eight planets in our solar system in astronomical terms. With accessible text, it provides the fundamental information any student needs to begin their studies in astronomy, such as how Earth spins and revolves around the Sun, why it's uniquely suitable for life, its physical features, atmosphere, biosphere, moon, its past, future, and more. To enhance the learning experience, many of the images come directly from NASA. This straightforward title offers the fundamental information any student needs to sp

  4. Quasi-thermal noise and shot noise spectroscopy on a CubeSat in Earth's ionosphere

    Science.gov (United States)

    Maj, Ronald; Cairns, Iver H.

    2017-03-01

    We investigate the practicality of using quasi-thermal noise (QTN) and shot noise spectroscopy on a CubeSat in the Earth's ionosphere and constrain the satellite antenna length for optimal detection of these signals. The voltage spectra predicted for thermal Langmuir waves (QTN) and particle "shot noise" are modeled, and it is shown that the signals detected can provide two very good, independent, passive, in situ methods of measuring the plasma density and temperature in the ionosphere. The impact of the antenna potential ϕ is also discussed, and we show that the negative potential calculated for the ionosphere due to natural current flows has a significant impact on the voltage power level of the shot noise spectrum. The antenna configuration is also shown to play an important role in the shot noise, with a monopole configuration enhancing the spectrum significantly compared with a dipole. Antenna lengths on the order of 20-40 cm are found to be ideal for ionospheric plasma conditions, nicely matching CubeSat sizes and producing detectable thermal Langmuir waves and shot noise at the microvolt level. Further, with a continuous stream of data points at different latitudes and longitudes an orbiting CubeSat can produce a global picture for the ionospheric plasma density and temperature using QTN and shot noise signals. If implemented, especially in a constellation, these data would be more frequent and cover a much greater domain than current ground-based or single-satellite methods. This could lead to improved ionospheric models, such as the empirically based International Reference Ionosphere.

  5. High-dispersion spectroscopy of extrasolar planets: from CO in hot Jupiters to O2 in exo-Earths.

    Science.gov (United States)

    Snellen, Ignas

    2014-04-28

    Ground-based high-dispersion spectroscopy could reveal molecular oxygen as a biomarker gas in the atmospheres of twin-Earths transiting red dwarf stars within the next 25 years. The required contrasts are only a factor of 3 lower than that already achieved for carbon monoxide in hot Jupiter atmospheres today but will need much larger telescopes because the target stars will be orders of magnitude fainter. If extraterrestrial life is very common and can therefore be found on planets around the most nearby red dwarf stars, it may be detectable via transmission spectroscopy with the next-generation extremely large telescopes. However, it is likely that significantly more collecting area is required for this. This can be achieved through the development of low-cost flux collector technology, which combines a large collecting area with a low but sufficient image quality for high-dispersion spectroscopy of bright stars.

  6. Moessbauer and X-ray diffraction studies of nanostructured Fe{sub 70}Al{sub 30} powders elaborated by mechanical alloying

    Energy Technology Data Exchange (ETDEWEB)

    Kezrane, M., E-mail: mohamedkezrane@yahoo.fr [LMP2M Laboratory, University of Medea, (26000) (Algeria); Guittoum, A. [Nuclear Research Centre of Algiers, 2 Bd Frantz Fanon, BP 399, Algiers (Algeria); Boukherroub, N.; Lamrani, S. [LMMC, M' hamed Bougara University, Boumerdes, 35000 (Algeria); Sahraoui, T. [Laboratory of Materials and Surface Treatments, LTSM, University of Saad Dahleb Blida, BP. 270 route de Soumaa, Blida (09000) (Algeria)

    2012-09-25

    Highlights: Black-Right-Pointing-Pointer Nanocrystalline Fe{sub 70}Al{sub 30} powders were successfully elaborated by mechanical alloying. Black-Right-Pointing-Pointer The Moessbauer spectra show that from 4 h of milling, a disordered ferromagnetic. Black-Right-Pointing-Pointer Fe{sub 70}Al{sub 30} starts to form and dominates after 36 h. - Abstract: We have studied the effect of milling time on the structural and hyperfine properties of Fe{sub 70}Al{sub 30} compound elaborated by mechanical alloying. The elaboration was performed with a vario-planetary ball mill P4 at different milling times. The milled powders were characterized by X-ray diffraction (XRD) and Moessbauer spectroscopy. From XRD diffraction spectra, we show that the bcc Fe(Al) solid solution was completely formed after 27 h of milling time. When the milling time increases, the lattice parameter increases, whereas the grain size decreases and the mean level of microstrains increases. The analysis of Moessbauer spectra shows that from 4 h of milling, a disordered ferromagnetic Fe{sub 70}Al{sub 30} starts to form and dominates after 36 h.

  7. Moessbauer spectroscopic study on inorganic compounds. Pt. 2

    Energy Technology Data Exchange (ETDEWEB)

    Takahashi, Masashi; Kitazawa, Takafumi; Nanba, Hiroshi; Yoshinaga, Tomohiro; Nakajima, Norio; Sumisawa, Yasuhiro; Takeda, Masuo [Toho Univ., Funabashi, Chiba (Japan). Faculty of Science; Sawahata, Hiroyuki; Ito, Yasuo

    1998-01-01

    {sup 166}Er and {sup 127}I Moessbauer spectra were observed. {sup 166}Er Moessbauer spectrum of Er metal and 9 compounds were measured by {sup 166}Ho/Y{sub 0.6}Ho{sub 0.4}H{sub 2} source at 12K and the parameters such as e{sup 2}qQ(mm s{sup -1}), Heff(T) and {tau}(ns) were determined. The relaxation time of ErCl{sub 3}{center_dot}6H{sub 2}O was 0.7ns, long, but that of ErCl{sub 3} was 10 ps, short time. {sup 127}I Moessbauer spectrum of PhI(O{sub 2}CR){sub 2} (R=CH{sub 3}, CHF{sub 2}, CH{sub 2}Cl, CHCl{sub 2}, CCl{sub 3}, CH{sub 2}Br, CHBr{sub 2} and CBr{sub 3}) were observed and compared with that of R`{sub 3}Sb(O{sub 2}CR){sub 2} was similar to that of PhI(O{sub 2}CR){sub 2}. The correlation coefficient between e{sup 2}qQ({sup 127}I) and Mulliken population of carboxylic hydrogen atom of R{sub 2}CO{sub 2}H was -0.87. The relation between the hypervalent bond of O-I-O and that of O-Sb-0 was shown by the equation: e{sup 2}qQ({sup 121}Sb)/mm s{sup -1} = -47.2 + 1.32 e{sup 2}qQ({sup 127}I)/mm s{sup -1}. Hypervalent iodine complex such as (PhI(py){sub 2}){sup 2+} salt and E-Sb-I (E=O, I, N and C) were studied, too. (S.Y.)

  8. Moessbauer characterisation of Fe-polygalacturonate as a medicine for human anaemia: the effect of iron concentration

    Energy Technology Data Exchange (ETDEWEB)

    Fodor, Judit, E-mail: fodorj@chemres.hu [Hungarian Academy of Sciences, Institute of Materials and Environmental Chemistry, Chemical Research Center (Hungary); Kuzmann, Erno [Hungarian Academy of Sciences, Department of Nuclear Chemistry, Institute of Nanochemistry and Catalysis, Chemical Research Center (Hungary); Vertes, Attila; Homonnay, Zoltan [Eoetvoes Lorand University, Institute of Chemistry (Hungary); Klencsar, Zoltan [Hungarian Academy of Sciences, Department of Surface Modifications and Nanostructures, Institute of Nanochemistry and Catalysis, Chemical Research Center (Hungary); May, Zoltan; Szentmihalyi, Klara [Hungarian Academy of Sciences, Institute of Materials and Environmental Chemistry, Chemical Research Center (Hungary)

    2009-04-15

    {sup 57}Fe Moessbauer spectroscopy was used to study the effect of iron concentration on the oxidation state and microenvironments of iron in Fe-polygalacturonate compounds prepared by a novel method from pectin. The iron concentration of the coordination compounds was determined by inductively coupled plasma optical emission spectrometry analysis. The Moessbauer spectra of the studied compounds could be decomposed into three markedly different quadrupole doublets referring to three microenvironments. Two of these have ferrous and one has ferric oxidation state. In the applied concentration range the relative occurrence of the ferric component was found to increase considerably with iron concentration. At the same time, with increasing iron concentration the relative occurrence characteristic of the three components showed saturation behaviour up to the iron concentration at which for each pair of galacturonic acid units there is on average one iron atom in the system, which iron concentration value is interpreted as to be related to the complete fill up of certain iron complexation sites of the polygalacturonate chains.

  9. {sup 119}Sn Moessbauer characterization of self assembled organotin(IV) complexes with Schiff bases containing amino acetate skeletons

    Energy Technology Data Exchange (ETDEWEB)

    Basu, Smita; Mizar, Archana; Baul, Tushar S. Basu, E-mail: basubaul@nehu.ac.in [North-Eastern Hill University, NEHU Permanent Campus, Department of Chemistry (India); Rivarola, Eleonora [Universita di Palermo, Dipartimento di Chimica Inorganica e Analitica ' Stanislao Cannizzaro' (Italy)

    2008-07-15

    Several organotin(IV) compounds, viz., diorganotin(IV) compounds of the types Ph{sub 2}SnLH (monomer), {sup n}Bu{sub 2}SnLH.OH{sub 2} (monomer), [Me{sub 2}SnLH.OH{sub 2}]{sub 2} (centrosymmetric dimer), [{sup n}Bu{sub 2}SnLH]{sub 3} (cyclic trinuclear), [Ph{sub 2}SnLH]{sub n} (polymer), {l_brace}[{sup n}Bu{sub 2}Sn(LH)]{sub 2}O{r_brace}{sub 2} (centrosymmetric tetranuclear), dinuclear di-/tri-mixed organotin(IV) compounds Ph{sub 2}SnLH.Ph{sub 3}SnCl (monomer) and triorganotin(IV) compounds of the types [Bz{sub 3}SnLH]{sub 2} (centrosymmetric dimer) and [Me{sub 3}SnL{sup 1}H]{sub n} (Polymer) (LH Schiff base carboxylate) have been studied in the solid state at liquid nitrogen temperature using {sup 119}Sn Moessbauer spectroscopy. The tin coordination geometry of the compounds determined from crystallography was correlated with the {sup 119}Sn Moessbauer results.

  10. Moessbauer studies of raw materials from Misti volcano of Arequipa (Peru) for its potential application in the ceramic field

    Energy Technology Data Exchange (ETDEWEB)

    Bustamante, Angel, E-mail: angelbd1@gmail.com [Universidad Nacional Mayor de San Marcos (Peru); Capel, Francisco; Barba, Flora, E-mail: flora@icv.csic.es; Callejas, Pio [Consejo Superior de investigaciones Cientificas (CSIC), Instituto de Ceramica y Vidrio (Spain); Guzman, Rivalino [Universidad Nacional de San Agustin de Arequipa (Peru); Trujillo, Alejandro [Universidad Nacional Mayor de San Marcos (Peru)

    2009-04-15

    We would like to introduce, the study of two different colour 'sillar' samples: white and pink, belonging to the Anashuayco quarry in the Arequipa Region (Peru). The X-ray diffraction (XRD) analysis indicates the presence of several mineralogical phases, such as feldpars and biotite for the both white and pink 'sillar' whereas cristobalite and quartz are detected only in the first sample and amorphous phase in the second one. In room temperature, Moessbauer spectroscopy, the presence of hematite ({alpha}-Fe{sub 2}O{sub 3}) was detected as the main phase for both samples, this was not detected in the XRD measurements. Moreover, corresponding doublets in the Moessbauer spectra indicate the presence of iron in the aluminium-silicate minerals. The rates Fe{sup 2+}/Fe{sup 3+} are 0.0752 and 0.0526 to the white and pink samples respectively. The minerals composing the white tuff form a heterogeneous aggregate of uniform aspect. Mining of these materials generates a great amount of waste in the form of lumps of varying size and which are raw materials studied in the present work for potential application in the ceramic field.

  11. Alkaline Earth Core Level Photoemission Spectroscopy of High-Temperature Superconductors

    Science.gov (United States)

    Vasquez, R.

    1993-01-01

    This paper examines photoemission measurements of the alkaline Earth core levels of high-temperature superconductors and related materials, models that seek to explain the large negative shifts observed relative to the corresponding alkaline Earth metals, and the effect of lattice site disorder on the core level spectra and the presence or absence of intrinsic surface peaks.

  12. Alkaline Earth Core Level Photoemission Spectroscopy of High-Temperature Superconductors

    Science.gov (United States)

    Vasquez, R.

    1993-01-01

    This paper examines photoemission measurements of the alkaline Earth core levels of high-temperature superconductors and related materials, models that seek to explain the large negative shifts observed relative to the corresponding alkaline Earth metals, and the effect of lattice site disorder on the core level spectra and the presence or absence of intrinsic surface peaks.

  13. Synthesis of Co Diffused Cu matrix for Applying Moessbauer Source

    Energy Technology Data Exchange (ETDEWEB)

    Choi, Sang Mu; Uhm, Young Rang; Kim, Jong Bum; Son, Kwang Jae [Korea Atomic Energy Research Institute, Daejeon (Korea, Republic of)

    2015-10-15

    To establish the coating conditions for {sup 57}Co, nonradioactive Co ions are dissolved in an acid solution and electroplated on to a copper plate. Then, the thermal diffusion of electroplated Co into a copper matrix was studied to apply a {sup 57}Co Moessbauer source. Nanocrystalline Co particles were coated on a Cu substrate using DC electro-deposition at a pH of 1.89 to 5 and 20-30 mA/cm{sup 2}. The average grain size was up to 54 nm as the pH increased to 5. The second phase of Co-oxide was formatted as the pH was increased above 4. The influence of different annealing conditions was investigated. The diffusion depth of Co depends on the annealing temperature and time. Charged Co ions are formed by sulfate, sulfamate, chloride, and a Watts bath. However, charged {sup 57}Co ions are formed by dissolving metal {sup 57}Co. To establish the coating conditions for {sup 57}Co, non-radioactive Co ions are dissolved in an acid solution and electroplated on to a copper plate. Then, the thermal diffusion of electroplated Co into a copper matrix was studied to apply a {sup 57}Co Moessbauer source.

  14. Moessbauer In Situ Studies of the Surface of Mars

    Energy Technology Data Exchange (ETDEWEB)

    Klingelhoefer, G., E-mail: klingel@mail.uni-mainz.de [Johannes Gutenberg Universitaet, Inst. Anorganische and Analytische Chemie (Germany)

    2004-11-15

    For the first time in history, a Moessbauer spectrometer was placed on the surface of another planet. Our miniaturized Moessbauer spectrometer MIMOS II is part of the instrument payload of NASA's twin Mars Exploration Rovers (MER) 'Spirit' and 'Opportunity', which in January 2004 successfully landed at the Gusev crater and the Meridiani Planum landing sites, respectively. MIMOS II determines the Fe-bearing mineralogy of Martian soils and rocks at the Rovers' respective landing sites. The main goals of this planetary twin mission are to: (1) identify hydrologic, hydrothermal, and other processes that have operated and affected materials at the landing sites; (2) identify and investigate the rocks and soils at both landing sites, as there is a possible chance that they may preserve evidence of ancient environmental conditions and possible prebiotic or biotic activities. With MIMOS II, besides other minerals the Fe silicate olivine has been identified in both soil and rocks at both landing sites. At the Meridiani site the Fe sulfate jarosite has been identified by MIMOS II which is definitive mineralogical proof of the presence of water at this site in the past.

  15. Mossbauer spectroscopy of magnetic minerals in basalt on Earth and Mars

    DEFF Research Database (Denmark)

    Gunnlaugsson, H. P.; Rasmussen, H.; Kristjansson, L.;

    2008-01-01

    Mossbauer spectroscopy of iron-titanium containing spinel phases is reviewed. New techniques are presented for determination of their composition using room-temperature Mossbauer spectroscopy. An example of thermal alteration processes is described. The speciality of olivine-containing basalt is ...

  16. Moessbauer studies of YBa[sub 2](Cu[sub 1-x]Fe[sub x])[sub 3]O[sub 7-d] annealed in an inert atmosphere

    Energy Technology Data Exchange (ETDEWEB)

    Maknani, J. (Lab. de Magnetisme et Materiaux Magnetiques, CNRS, 92 Meudon (France)); Dormann, J.L. (Lab. de Magnetisme et Materiaux Magnetiques, CNRS, 92 Meudon (France)); Terziev, V.G. (Lab. de Magnetisme et Materiaux Magnetiques, CNRS, 92 Meudon (France)); Jove, J. (Inst. Curie, Paris (France)); Pankowska, H. (Lab. de Physique des Solides, CNRS, 92 Meudon (France)); Gorochov, O. (Lab. de Physique des Solides, CNRS, 92 Meudon (France)); Suryanarayanan, R. (Lab. de Physique des Solides, CNRS, 92 Meudon (France))

    1994-11-01

    YBa[sub 2](Cu[sub 1-x]Fe[sub x])[sub 3]O[sub 7-d] annealed in an Ar atmosphere, then reoxygenated at various temperatures, has been studied by Moessbauer spectroscopy at 300 K and low temperature with and without an applied field of 5.5 T. The results are interpreted as being due to Fe clustering remaining in the chains rather than a significant transfer to the planes. (orig.)

  17. Moessbauer study of iron(II) and iron(III) complexes of some nitrogen-, oxygen- and sulphur donor ligands, reduction of iron(III) by the mercaptide group

    Energy Technology Data Exchange (ETDEWEB)

    Sawhney, G.L.; Baijal, J.S. (Delhi Univ. (India). Dept. of Physics and Astrophysics); Chandra, S. (Zakir Hussain College, Ajmeri Gate, Delhi (India). Dept. of Chemistry); Pandeya, K.B. (Delhi Univ. (India). Dept. of Chemistry)

    1981-01-01

    Complex formation reactions of iron(II) and iron(III) with semicarbazones and thiosemicarbazones of pyruvic acid and phenyl pyruvic acid have been studied by magnetic measurements and Moessbauer spectroscopy. With iron(II), all the ligands form hexa-coordinated octahedral complexes of the type Fe(ligand-H/sub 2/). With iron(III) semicarbazones, complexes of the composition (Fe(ligand-H)/sub 2/)(OH) are formed. Thiosemicarbazones first reduce iron(III) to iron(II) and then form iron(II) complexes of the type Fe(ligand-H)/sub 2/.

  18. Moessbauer studies of Haltern 70 amphorae from Castro do Vieito, North of Portugal, and of amphora sherds from kilns in the Roman provinces Hispania Baetica and Lusitania

    Energy Technology Data Exchange (ETDEWEB)

    Costa, B. F. O., E-mail: benilde@ci.uc.pt [University of Coimbra, CEMDRX, Physics Department (Portugal); Silva, A. J. M. [Centro de Estudos Arqueologicos das Universidades de Coimbra e do Porto/CAM, Palacio de Sub-Ripas (Portugal); Wagner, F. E.; Wagner, U. [Technical University of Munich, Physics Department (Germany)

    2011-11-15

    Haltern 70 amphora sherds from Castro do Vieito and from kilns in the Roman provinces Baetica and Lusitania were studied by Moessbauer spectroscopy, EDX and XRD. An amphora whose handle was carefully studied must have been fired reducingly at a temperature of or above about 900 Degree-Sign C and cooled in oxidizing conditions in the end. Oxidation and hematite formation went hand in hand, and the amount of hematite formed depended sensitively of the speed of penetration of the oxygen and the cooling rate in the interior of the ceramic body.

  19. A Moessbauer spectroscopic study on the action of Ce in the catalyst for dehydrogenation of etylbenzene to styrene

    Energy Technology Data Exchange (ETDEWEB)

    Jiang Keyu, E-mail: keyujiang@126.com [East China Normal University, Department of Physics (China); Fan Qin; Chen Tong; Miao Changxi [Shanghai Research Institute of Petrochemical Technology, SINOPEC (China); Zhao Zhenji; Yang Xielong [East China Normal University, Department of Physics (China)

    2012-03-15

    Two series of Fe-K catalysts for dehydrogenation of ethylbenzene to styrene were prepared with different amounts and different compounds of the additional element Ce. Moessbauer spectroscopy has been used to determine the Fe compound in the catalyst and to investigate the effect of Ce. The catalytic properties of the catalysts have also been measured. The results show that the element Ce in the catalyst is favorable to form the predecessor of the catalytic active phase, the compound KFe{sub 11}O{sub 17} and that the optimal percentage of CeO{sub 2} is 8%{approx}15% in the catalyst which is favorable to the formation of KFe{sub 11}O{sub 17} and to get better catalytic properties.

  20. On the Analysis of the Moessbauer Spectra of the Rust Converted by Tannic and Phosphoric Acids

    Energy Technology Data Exchange (ETDEWEB)

    Barrero, C. A. [Universidad de Antioquia, Grupo de Estado Solido, Instituto de Fisica (Colombia); Rios, J. F. [Universidad de Antioquia, Grupo de Corrosion y Proteccion, Facultad de Ingenierias (Colombia); Morales, A. L. [Universidad de Antioquia, Grupo de Estado Solido, Instituto de Fisica (Colombia); Bohorquez, A.; Perez-Alcazar, G. [Universidad del Valle, Grupo de Metalurgia Fisica y Transiciones de Fase, Departamento de Fisica (Colombia)

    2003-06-15

    In previous work, we reported results on the action of rust converters based on a mixture of tannic and phosphoric acids, upon the rust formed on mild steel coupons. There, the rust before and after the application of converters were characterized by room-temperature Moessbauer spectroscopy, among other techniques. The present work is an extension of this one, and additional MS at 77 K, 130 K and 300 K for some samples are presented. Special emphasis is given to the methodology of analysis. Our results confirm previous findings that an important portion of the magnetite remains without conversion. New information was also derived: (i) the converters seem to affect more the magnetite octahedral (B) than the tetrahedral (A) sites; (ii) among the magnetite B sites, the Fe{sup 2+} is the most affected; (iii) at least 31% of magnetic goethite at 77 K is transformed by the converter; and (iv) the presence of an additional phase identified as ferrous phosphate, could be resolved unambiguously only at these lower temperatures.

  1. Electrochemical and conversion electron Moessbauer study of corrosion induced by acid rain

    Energy Technology Data Exchange (ETDEWEB)

    Vertes, C.; Lakatos-Varsanyi, M.; Vertes, A. (Dept. of Physical Chemistry and of Nuclear Chemistry, Eoetvoes Univ., Budapest (Hungary)); Meisel, W.; Guetlich, P. (Inst. of Inorganic Chemistry and Analytical Chemistry, Univ. Mainz (Germany))

    1993-04-01

    The passivation of low carbon steel was studied in aqueous solution of 0.5M Na[sub 2]SO[sub 4]+0.001M NaHSO[sub 3] (pH 3.5, 6.5 and 8.5) which can be considered as a model of acid rain. The used conversion electron Moessbauer spectroscopy (CEMS) with the complementary electrochemical investigations proved that the sulfite ions induce pitting corrosion at pH 3.5 and 6.5, while the measurements showed much weaker pitting at pH 8.5. The compositions and thicknesses of the passive films formed during the electrochemical treatments are determined from the CEM spectra. Only [gamma]-FeOOH was found on the surface of the samples at pH 6.5 and 8.5. Nevertheless, at pH 3.5 the sextet belonging to Fe[sub 3]C appears in the spectra, and also FeSO[sub 4].H[sub 2]O could be detected in low concentration. (orig.).

  2. Moessbauer and magnetic studies of parent material from argentine pampas soils

    Energy Technology Data Exchange (ETDEWEB)

    Bidegain, J. C. [Laboratorio de Entrenamiento Multidisciplinario para la Investigacion Tecnologica (Argentina); Bartel, A. A. [Universidad Nacional de La Pampa, Facultad de Ciencias Exactas y Naturales (Argentina); Sives, F. R.; Mercader, R. C., E-mail: mercader@fisica.unlp.edu.ar [Universidad Nacional de La Plata, Departamento de Fisica, Facultad de Ciencias Exactas (Argentina)

    2007-02-15

    In order to establish a correlation between the different types of soils using hyperfine and magnetic parameters as climatic and environmental proxies, we have studied the differentiation of soil developed around 38.5{sup o} south latitude, in the central Pampas of Argentina, by means of Moessbauer spectroscopy and environmental magnetism. The soils transect (climosequence) investigated stretches from the drier west (around 64{sup o} W) to the more humid east (at around 59{sup o} W) in the Buenos Aires Province, covering a distance of 600 km. The soils studied developed during recent Holocene geologic times in a landscape characterized by small relict plateaus, slopes and depressions, dunes and prairies. The parent material consists of eolian sandy silts overlying calcrete layers. The low mean annual precipitation in the western parts of the region gives rise to soils without B-horizons, which limits the agricultural use of land. The preliminary results show an increase of the paramagnetic Fe{sup 3+} relative concentration from west to east in the soils investigated. Magnetite is probably mainly responsible for the observed enhancement in the susceptibility values. The magnetic response of the parent material is similar to that of the loess part of the previously investigated loess-paleosol sequences of the Argentine loess plateau.

  3. Moessbauer and XRD study of pulse plated Fe-P and Fe-Ni thin layers

    Energy Technology Data Exchange (ETDEWEB)

    Miko, Annamaria [Bay Zoltan Institute for Material Science (Hungary); Kuzmann, Erno, E-mail: kuzmann@para.chem.elte.hu [Eoetvoes Lorand University, Research Group for Nuclear Methods in Structural Chemistry, Hungarian Academy of Sciences, Department of Nuclear Chemistry (Hungary); Lakatos-Varsanyi, Magda [Bay Zoltan Institute for Material Science (Hungary); Kakay, Attila [Research Institute for Solid State Physics and Optics (Hungary); Nagy, Ferenc [Eoetvoes Lorand University, Research Group for Nuclear Methods in Structural Chemistry, Hungarian Academy of Sciences, Department of Nuclear Chemistry (Hungary); Varga, Lajos Karoly [Research Institute for Solid State Physics and Optics (Hungary)

    2005-09-15

    {sup 57}Fe conversion electron Moessbauer spectroscopy, X-ray diffraction, electrochemical and magnetic measurements were used to study pulse electroplated Fe-P and Ni-Fe coatings. XRD and {sup 57}Fe CEMS measurements revealed the amorphous character of the novel pulse plated Fe-P alloys. CEM spectra indicated significant differences in the short range order and in the magnetic anisotropy between the Fe-P deposits pulse plated at medium long deposition time (t{sub on} = 2 ms), with short relaxation time (t{sub off} = 9 ms) and low current density (I{sub p} = 0.05 Acm{sup -2}) or at short deposition time (t{sub on} = 1 ms) with long relaxation time (t{sub off} = 250 ms) and high current density (I{sub p} = 1.0 Acm{sup -2}). The broad peaks centred around the fcc reflections in XRD of the pulse plated Ni-22 wt.% Fe deposit reflected a microcrystalline Ni-Fe alloy with a very fine, 5-8 nm, grain size. The CEM spectrum of the pulse plated Ni-22 wt.% Fe coating corresponded to a highly disordered solid solution alloy containing a minute amount of ferrihydrite. Extreme favourable soft magnetic properties were observed with these Ni-Fe and Fe-P pulse plated thin layers.

  4. On simfitting MER Moessbauer data to characterize Martian hematite

    Energy Technology Data Exchange (ETDEWEB)

    Agresti, David G [University of Alabama at Birmingham, Birmingham, AL 35294-1170 (United States); Fleischer, Iris; Klingelhoefer, Goestar [Institut fuer Anorganische und Analytische Chemie, Universitaet Mainz (Germany); Morris, Richard V, E-mail: agresti@uab.ed, E-mail: fleischi@uni-mainz.d [NASA Johnson Space Center, Houston, Texas 77058 (United States)

    2010-03-01

    Moessbauer spectra of Eagle Crater outcrop rocks in Meridiani Planum were acquired by the Mars Exploration Rover (MER) Opportunity. Sixty spectra, containing {approx}20 to 60% hematite by area, were simultultaneously fit (simfit) in a self-consistent manner to a single chi-squared minimum, where relations among parameters from different spectra were defined for both sol (Martian day) and acquisition temperature (200-280 K). Different spectral models were compared, hematite being modeled optimally with two sextets. Sextet S1 ({approx}35% of total sextet area) has narrower linewidths, a larger magnetic hyperfine field, and a quadrupole shift that changes smoothly from positive to negative values as the temperature increases through the bulk Morin transition temperature. Sextet S2 has broader linewidths, a likely skewed line shape, a smaller hyperfine field, and a quadrupole shift that remains negative at all temperatures, implying the S2 phase is weakly ferromagnetic at all temperatures.

  5. Studies on Intermolecular Energy Transfer and Relaxation Processes in Solid Rare Earth Complexes by Photoacoustic Spectroscopy

    Institute of Scientific and Technical Information of China (English)

    伍荣护; 赵化章; 于锡娟; 宋慧宇; 苏庆德

    2001-01-01

    The photoacoustic spectra of Eu(benz)3*(phen)2 (benz: benzoate, phen: phenanthroline) and Eu0.8Ln0.2(benz)3*(phen)2 (Ln3+: La3+ or Nd3+) were reported. The intermolecular energy transfer processes were studied from the point of the nonradiative transitions. Combined with the fluorescence spectroscopy, photoacoustic spectroscopy reflects the variation of the luminescence efficiencies of solid samples. The luminescence efficiency increases when La3+ is introduced, but it decreases greatly when Nd3+ is added, which is due to the difference of intermolecular energy transfer processes. The models of intramolecular and intermolecular energy transfer and relaxation processes were established.

  6. Near-Infrared Spectroscopy of Warm Spitzer-observed Near-Earth Objects

    NARCIS (Netherlands)

    Thomas, Cristina A.; Emery, J. P.; Trilling, D. E.; Delbo, M.; Hora, J. L.; Mueller, M.

    2013-01-01

    We have completed a spectroscopic observing campaign to complement the ExploreNEOs Warm Spitzer program. ExploreNEOs or “The Warm Spitzer NEO Survey: Exploring the history of the inner Solar System and near-Earth space” was allocated 500 hours over two years (2009-2011) to determine diameters and al

  7. Near-Infrared Spectroscopy of Warm Spitzer-observed Near-Earth Objects

    NARCIS (Netherlands)

    Thomas, Cristina A.; Emery, J. P.; Trilling, D. E.; Delbo, M.; Hora, J. L.; Mueller, M.

    2013-01-01

    We have completed a spectroscopic observing campaign to complement the ExploreNEOs Warm Spitzer program. ExploreNEOs or “The Warm Spitzer NEO Survey: Exploring the history of the inner Solar System and near-Earth space” was allocated 500 hours over two years (2009-2011) to determine diameters and

  8. Spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Hellman, Hal

    1968-01-01

    This booklet discusses spectroscopy, the study of absorption of radiation by matter, including X-ray, gamma-ray, microwave, mass spectroscopy, as well as others. Spectroscopy has produced more fundamental information to the study of the detailed structure of matter than any other tools.

  9. Spectroscopy

    CERN Document Server

    Walker, S

    1976-01-01

    The three volumes of Spectroscopy constitute the one comprehensive text available on the principles, practice and applications of spectroscopy. By giving full accounts of those spectroscopic techniques only recently introduced into student courses - such as Mössbauer spectroscopy and photoelectron spectroscopy - in addition to those techniques long recognised as being essential in chemistry teaching - sucha as e.s.r. and infrared spectroscopy - the book caters for the complete requirements of undergraduate students and at the same time provides a sound introduction to special topics for graduate students.

  10. Role of Mo in the local configuration and structure stabilization of amorphous steels, a Synchrotron X-ray diffraction and Moessbauer study

    Energy Technology Data Exchange (ETDEWEB)

    Pineda, E., E-mail: eloi.pineda@upc.edu [Departament de Fisica i Enginyeria Nuclear, ESAB, Universitat Politecnica de Catalunya, Esteve Terradas 8, 08860 Castelldefels (Spain); Bruna, P. [Departament de Fisica Aplicada, EPSC, Universitat Politecnica de Catalunya, Avda. del Canal Olimpic s/n, 08860 Castelldefels (Spain); Serrano, J. [Departament de Fisica Aplicada, EPSC, Universitat Politecnica de Catalunya, Avda. del Canal Olimpic s/n, 08860 Castelldefels (Spain); Institucio Catalana de Recerca i Estudis Avancats, Catalonia (Spain); Torrens-Serra, J. [Grup de Nanomaterials i Microsistemes, Departament de Fisica, Universitat Autonoma de Barcelona. Edifici Cc, 08193 Bellaterra (Spain); Crespo, D. [Departament de Fisica Aplicada, EPSC, Universitat Politecnica de Catalunya, Avda. del Canal Olimpic s/n, 08860 Castelldefels (Spain)

    2011-06-15

    Highlights: > Mo substitution of Fe atoms stabilizes structure in amorphous steels. > Moessbauer spectroscopy evidences two distinct Fe atoms environments in the amorphous structure of the Mo containing glassy alloys. > Structural relaxation before crystallization produces homogenization of the Fe environments reducing population of sites with low hyperfine fields. - Abstract: Amorphous steels are promising materials with potential structural applications. The glass-forming ability (GFA) and mechanical properties of metallic glasses are intimately related to the local structure. In Fe-based alloys, Cr and Mo content seem to play a key role in stabilizing the amorphous atomic-level structure. Here we present a study on the effects of changing Mo content in Fe{sub 72-x}C{sub 7}Si{sub 3.3}B{sub 5.5}P{sub 8.7}Cr{sub 2.3}Al{sub 2}Mo{sub x} amorphous steels. We study the local structure of these alloys by Synchrotron X-ray diffraction and Moessbauer spectroscopy. The results show how the amorphous phase evolves from a ferromagnetic Fe-rich structure to a structure with predominance of paramagnetic environments with the increase of Mo content. The changes in the distribution of magnetic environments cannot be attributed only to the Fe-Mo substitution but to a change of local configuration in the amorphous phase.

  11. Spin density wave in (Fe{sub x}V{sub 3-x})S{sub 4} and the coexistence of normal and condensate states: A Moessbauer study

    Energy Technology Data Exchange (ETDEWEB)

    Embaid, B.P., E-mail: pembaid@fisica.ciens.ucv.ve [Laboratorio de Magnetismo, Escuela de Fisica, Universidad Central de Venezuela, Apartado 47586, Los Chaguaramos, Caracas 1041-A (Venezuela, Bolivarian Republic of); Gonzalez-Jimenez, F. [Laboratorio de Magnetismo, Escuela de Fisica, Universidad Central de Venezuela, Apartado 47586, Los Chaguaramos, Caracas 1041-A (Venezuela, Bolivarian Republic of)

    2013-03-15

    Iron-vanadium sulfides of the monoclinic system Fe{sub x}V{sub 3-x}S{sub 4} (1.0{<=}x{<=}2.0) have been investigated by {sup 57}Fe Moessbauer Spectroscopy in the temperature range 30-300 K. Incommensurate spin density waves (SDW) have been found in this system. An alternative treatment of the spectra allows a direct measurement of the temperature evolution of condensate density of the SDW state which follows the Maki-Virosztek formula. For composition (x=1.0) the SDW condensate is unpinned while for compositions (x>1.0) the SDW condensate is pinned. Possible causes of the pinning-unpinning SDW will be discussed. - Highlights: Black-Right-Pointing-Pointer Fe{sub x}V{sub 3-x}S{sub 4}(1.0{<=}x{<=}2.0) system was investigated by {sup 57}Fe Moessbauer Spectroscopy. Black-Right-Pointing-Pointer Incommensurate spin density wave (SDW) has been found in this system. Black-Right-Pointing-Pointer We report the temperature evolution of the condensate density of SDW state. Black-Right-Pointing-Pointer For composition (x=1.0) the SDW is unpinned while for (x>1.0) is pinned.

  12. Optical spectroscopy of low-dimensional rare-earth iron borates

    Science.gov (United States)

    Popova, M. N.

    2009-04-01

    The family of RFe 3(BO 3) 4 borates (R=Pr, Nd, Eu-Er, Y) was studied by high-resolution optical absorption and Raman spectroscopies. Structural and magnetic phase transitions were detected and the types of magnetic structure were determined. Energy of crystal-field (CF) levels and exchange splitting of the ground state of the R 3+ ion were obtained from the analysis of optical spectra. CF calculations were carried out. Effective magnetic field at the R 3+ site was found, using the calculated value of the magnetic g-factor. Some peculiarities of modeling the paramagnetic susceptibility of NdFe 3(BO 3) 4 are discussed.

  13. Imaging spectroscopy: Earth and planetary remote sensing with the USGS Tetracorder and expert systems

    Science.gov (United States)

    Clark, R.N.; Swayze, G.A.; Livo, K.E.; Kokaly, R.F.; Sutley, S.J.; Dalton, J.B.; McDougal, R.R.; Gent, C.A.

    2003-01-01

    Imaging spectroscopy is a tool that can be used to spectrally identify and spatially map materials based on their specific chemical bonds. Spectroscopic analysis requires significantly more sophistication than has been employed in conventional broadband remote sensing analysis. We describe a new system that is effective at material identification and mapping: a set of algorithms within an expert system decision-making framework that we call Tetracorder. The expertise in the system has been derived from scientific knowledge of spectral identification. The expert system rules are implemented in a decision tree where multiple algorithms are applied to spectral analysis, additional expert rules and algorithms can be applied based on initial results, and more decisions are made until spectral analysis is complete. Because certain spectral features are indicative of specific chemical bonds in materials, the system can accurately identify and map those materials. In this paper we describe the framework of the decision making process used for spectral identification, describe specific spectral feature analysis algorithms, and give examples of what analyses and types of maps are possible with imaging spectroscopy data. We also present the expert system rules that describe which diagnostic spectral features are used in the decision making process for a set of spectra of minerals and other common materials. We demonstrate the applications of Tetracorder to identify and map surface minerals, to detect sources of acid rock drainage, and to map vegetation species, ice, melting snow, water, and water pollution, all with one set of expert system rules. Mineral mapping can aid in geologic mapping and fault detection and can provide a better understanding of weathering, mineralization, hydrothermal alteration, and other geologic processes. Environmental site assessment, such as mapping source areas of acid mine drainage, has resulted in the acceleration of site cleanup, saving

  14. Imaging spectroscopy: Earth and planetary remote sensing with the USGS Tetracorder and expert systems

    Science.gov (United States)

    Clark, Roger N.; Swayze, Gregg A.; Livo, K. Eric; Kokaly, Raymond F.; Sutley, Steve J.; Dalton, J. Brad; McDougal, Robert R.; Gent, Carol A.

    2003-12-01

    Imaging spectroscopy is a tool that can be used to spectrally identify and spatially map materials based on their specific chemical bonds. Spectroscopic analysis requires significantly more sophistication than has been employed in conventional broadband remote sensing analysis. We describe a new system that is effective at material identification and mapping: a set of algorithms within an expert system decision-making framework that we call Tetracorder. The expertise in the system has been derived from scientific knowledge of spectral identification. The expert system rules are implemented in a decision tree where multiple algorithms are applied to spectral analysis, additional expert rules and algorithms can be applied based on initial results, and more decisions are made until spectral analysis is complete. Because certain spectral features are indicative of specific chemical bonds in materials, the system can accurately identify and map those materials. In this paper we describe the framework of the decision making process used for spectral identification, describe specific spectral feature analysis algorithms, and give examples of what analyses and types of maps are possible with imaging spectroscopy data. We also present the expert system rules that describe which diagnostic spectral features are used in the decision making process for a set of spectra of minerals and other common materials. We demonstrate the applications of Tetracorder to identify and map surface minerals, to detect sources of acid rock drainage, and to map vegetation species, ice, melting snow, water, and water pollution, all with one set of expert system rules. Mineral mapping can aid in geologic mapping and fault detection and can provide a better understanding of weathering, mineralization, hydrothermal alteration, and other geologic processes. Environmental site assessment, such as mapping source areas of acid mine drainage, has resulted in the acceleration of site cleanup, saving

  15. Remote sensing of the earth's atmosphere by infrared absorption spectroscopy - An update of the ATMOS program

    Science.gov (United States)

    Zander, R.; Gunson, M. R.; Farmer, C. B.

    1989-01-01

    The NASA's Atmospheric Trace Molecule Spectroscopy (ATMOS) experiment was designed to address the requirements of the remote sensing of atmospheric composition on a four-dimensional basis (latitude, longitude, altitude, and time), necessary for understanding and predicting the effect of changes on the chemical balance of the atmosphere. This paper describes the ATMOS program, overviews the ATMOS instrument and its performance, and presents the results obtained during its first flight as part of the Spacelab 3 Space Shuttle mission (April 29 through May 6, 1985). Also discussed are prospects for further missions.

  16. Spectroscopy of Kerr Black Holes with Earth- and Space-Based Interferometers.

    Science.gov (United States)

    Berti, Emanuele; Sesana, Alberto; Barausse, Enrico; Cardoso, Vitor; Belczynski, Krzysztof

    2016-09-02

    We estimate the potential of present and future interferometric gravitational-wave detectors to test the Kerr nature of black holes through "gravitational spectroscopy," i.e., the measurement of multiple quasinormal mode frequencies from the remnant of a black hole merger. Using population synthesis models of the formation and evolution of stellar-mass black hole binaries, we find that Voyager-class interferometers will be necessary to perform these tests. Gravitational spectroscopy in the local Universe may become routine with the Einstein Telescope, but a 40-km facility like Cosmic Explorer is necessary to go beyond z∼3. In contrast, detectors like eLISA (evolved Laser Interferometer Space Antenna) should carry out a few-or even hundreds-of these tests every year, depending on uncertainties in massive black hole formation models. Many space-based spectroscopical measurements will occur at high redshift, testing the strong gravity dynamics of Kerr black holes in domains where cosmological corrections to general relativity (if they occur in nature) must be significant.

  17. Spectroscopy of Kerr black holes with Earth- and space-based interferometers

    CERN Document Server

    Berti, Emanuele; Barausse, Enrico; Cardoso, Vitor; Belczynski, Krzysztof

    2016-01-01

    We estimate the potential of present and future interferometric gravitational-wave detectors to test the Kerr nature of black holes through "gravitational spectroscopy," i.e. the measurement of multiple quasinormal mode frequencies from the remnant of a black hole merger. Using population synthesis models of the formation and evolution of stellar-mass black hole binaries, we find that Voyager-class interferometers will be necessary to perform these tests. Gravitational spectroscopy in the local Universe may become routine with the Einstein Telescope, but a 40-km facility like Cosmic Explorer is necessary to go beyond $z\\sim 3$. In contrast, eLISA-like detectors should carry out a few - or even hundreds - of these tests every year, depending on uncertainties in massive black hole formation models. Many space-based spectroscopical measurements will occur at high redshift, testing the strong gravity dynamics of Kerr black holes in domains where cosmological corrections to general relativity (if they occur in nat...

  18. Spectroscopy of Kerr Black Holes with Earth- and Space-Based Interferometers

    Science.gov (United States)

    Berti, Emanuele; Sesana, Alberto; Barausse, Enrico; Cardoso, Vitor; Belczynski, Krzysztof

    2016-09-01

    We estimate the potential of present and future interferometric gravitational-wave detectors to test the Kerr nature of black holes through "gravitational spectroscopy," i.e., the measurement of multiple quasinormal mode frequencies from the remnant of a black hole merger. Using population synthesis models of the formation and evolution of stellar-mass black hole binaries, we find that Voyager-class interferometers will be necessary to perform these tests. Gravitational spectroscopy in the local Universe may become routine with the Einstein Telescope, but a 40-km facility like Cosmic Explorer is necessary to go beyond z ˜3 . In contrast, detectors like eLISA (evolved Laser Interferometer Space Antenna) should carry out a few—or even hundreds—of these tests every year, depending on uncertainties in massive black hole formation models. Many space-based spectroscopical measurements will occur at high redshift, testing the strong gravity dynamics of Kerr black holes in domains where cosmological corrections to general relativity (if they occur in nature) must be significant.

  19. Theoretical study of the alkaline-earth (LiBe)+ ion: structure, spectroscopy and dipole moments

    Science.gov (United States)

    Ghanmi, C.; Farjallah, M.; Berriche, H.

    2017-03-01

    We study theoretically the structure and spectroscopic properties of the alkali alkaline-earth (LiBe)+ ion. The potential energy curves and their spectroscopic parameters, permanent and transition dipole moments are determined with a quantum chemistry approach. The (LiBe)+ ion is modelled as two valence electron system moving in the field of Be2+ and Li+ cores, which are described by pseudopotentials. In addition, effective core-polarization potentials are included to correct the energy. The molecular calculations are performed using a standard quantum chemistry approach based on the pseudopotential model, Gaussian basis sets, effective core polarization potentials, and full configuration interaction (CI) calculations. The precision of our spectroscopic parameters are discussed by comparison with currently available theoretical results. A rather good agreement is observed for the ground and first excited states. The permanent dipole moments reveal many abrupt changes, which are localized at particular distances corresponding to the positions of the avoided crossings.

  20. X-ray diffraction and Moessbauer studies on superparamagnetic nickel ferrite (NiFe{sub 2}O{sub 4}) obtained by the proteic sol–gel method

    Energy Technology Data Exchange (ETDEWEB)

    Nogueira, N.A.S. [Departamento de Engenharia Metalúrgica e de Materiais, Centro de Tecnologia, Campus do Pici, Universidade Federal do Ceará – UFC, 60455-760 Fortaleza, CE (Brazil); Utuni, V.H.S.; Silva, Y.C. [Departamento de Física, Universidade Federal do Ceará – UFC, Campus do Pici, 60440-970 Fortaleza, CE (Brazil); Kiyohara, P.K. [Instituto de Física, Universidade de São Paulo – USP, 05315-970 São Paulo, SP (Brazil); Vasconcelos, I.F. [Departamento de Engenharia Metalúrgica e de Materiais, Centro de Tecnologia, Campus do Pici, Universidade Federal do Ceará – UFC, 60455-760 Fortaleza, CE (Brazil); Miranda, M.A.R., E-mail: marcus.a.r.miranda@gmail.com [Departamento de Física, Universidade Federal do Ceará – UFC, Campus do Pici, 60440-970 Fortaleza, CE (Brazil); Sasaki, J.M. [Departamento de Física, Universidade Federal do Ceará – UFC, Campus do Pici, 60440-970 Fortaleza, CE (Brazil)

    2015-08-01

    Nickel ferrite (NiFe{sub 2}O{sub 4}) nanoparticles were synthesized by the proteic sol–gel method at synthesis temperature of 250 °C, 300 °C and 400 °C, with the objective of obtaining superparamagnetic nanoparticles. Thermogravimetric analysis (TGA) and temperature-programed oxidation (TPO) presented peaks around 290 °C indicating that nickel ferrite was forming at this temperature. X-ray powder diffraction (XRPD) confirmed that the polycrystalline sample was single phased NiFe{sub 2}O{sub 4} with space group Fd3m. Scherrer equation applied to the diffraction patterns and transmission electron microscopy (TEM) images showed that the size of the nanoparticles ranged from 9 nm to 13 nm. TEM images also revealed that the nanoparticles were agglomerated, which was supported by the low values of surface area provided by the Brunauer-Emmet-Teller (BET) method. Moessbauer spectroscopy presented spectra composed of a superposition of three components: a sextet, a doublet and a broad singlet pattern. The sample synthetized at 300 °C had the most pronounced doublet pattern characteristic of superparamagnetic nanoparticles. In conclusion, this method was partially successful in obtaining superparamagnetic nickel ferrite nanoparticles, in which the synthetized samples were a mixture of nanoparticles with blocking temperature above and below room temperature. Magnetization curves revealed a small hysteresis, supporting the Moessbauer results. The sample with the higher concentration of superparamagnetic nanoparticles being the one synthetized at 300 °C. - Highlights: • Superparamagnetic nickel ferrite nanoparticles were grown by the proteic sol–gel method. • The proteic sol–gel method provided superparamagnetic nickel ferrite nanoparticles with sizes in the range of 9–13 nm. • Nickel ferrite nanoparticles were prepared at temperatures as low as 250 °C. • The nickel ferrite nanoparticles were studied by x-ray diffraction and Moessbauer.

  1. Development of realtime monitoring technology for laser photoreaction product - Study on spectroscopy of rare earth elements by using diode laser and hollow cathode glow discharge

    Energy Technology Data Exchange (ETDEWEB)

    Lee, Sang Chun [Kyungnam University, Masan (Korea); Lee, Gea Ho [Chungnam National University, Taejon (Korea); Lee, Yong Il [Changwon National University, Changwon (Korea); Kim, Hyo Jin [Dongduk Women' s University, Seoul (Korea); Huh, Yong Dck [Dankook University, Seoul (Korea)

    1998-05-01

    Currently, fast and precise analysis of rare earth and actinide elements are much concerned and required for the safe treatments and storage of nuclear wastes generated by nuclear power plants. However, current technology is still far from the requirements for accurate realtime monitoring and measurement of radioactive elements. This project is of development of new technology of realtime monitoring and analysis of rare earth elements by using glow discharge and diode laser spectroscopy, and the study of spectroscopic characteristics of rare earth elements in glow discharge plasma. And, saturated absorption spectroscopy of rare earth elements was investigated with diode lasers. A see-through hollow cathode glow discharge (st-HCGD) cell was developed for the purpose of a portable atomizer and and its characteristics were investigated. High resolution spectroscopy was achieved with diode laser assisted saturated absorption spectroscopy. it is considered for major improvement of radioactive isotope detection technology. We expect a portable high resolution spectrometry with a see-through HCGD atomizer and diode lasers in near future. (Author). 63 refs., 39 figs., 7 tabs.

  2. Moessbauer-Fresnel zone plate as nuclear monochromator

    Energy Technology Data Exchange (ETDEWEB)

    Mooney, T.M.; Alp, E.E.; Yun, W.B.

    1992-06-01

    Zone plates currently used in x-ray optics derive their focusing power from (a spatial variation of) the electronic refractive index -- that is, from the collective effect of electronic x-ray-scattering amplitudes. Nuclei also scatter x rays, and resonant nuclear-scattering amplitudes, particularly those associated with Moessbauer fluorescence, can dominate the refractive index for x-rays whose energies are very near the nuclear-resonance energy. A zone plate whose Fresnel zones are filled alternately with {sup 57}Fe and {sup 56}Fe ({sup 57}Fe has a nuclear resonance of natural width {Gamma} = 4.8 nano-eV at 14.413 keV; {sup 56}Fe has no such resonance) has a resonant focusing efficiency; it focuses only those x-rays whose energies are within several {Gamma} of resonance. When followed by an absorbing screen with a small pinhole, such a zone plate can function as a synchrotron-radiation monochromator with an energy resolution of a few parts in 10{sup 12}. The energy-dependent focusing efficiency and the resulting time-dependent response of a resonant zone plate are discussed.

  3. Valence determination of rare earth elements in lanthanide silicates by L 3-XANES spectroscopy

    Science.gov (United States)

    Kravtsova, Antonina N.; Guda, Alexander A.; Goettlicher, Joerg; Soldatov, Alexander V.; Taroev, Vladimir K.; Kashaev, Anvar A.; Suvorova, Lyudmila F.; Tauson, Vladimir L.

    2016-05-01

    Lanthanide silicates have been hydrothermally synthesized using Cu and Ni containers. Chemical formulae of the synthesized compounds correspond to K3Eu[Si6O15] 2H2O, HK6Eu[Si10O25], K7Sm3[Si12O32], K2Sm[AlSi4O12] 0.375H2O, K4Yb2[Si8O21], K4Ce2[Al2Si8O24]. The oxidation state of lanthanides (Eu, Ce, Tb, Sm, Yb) in these silicates has been determined using XANES spectroscopy at the Eu, Ce, Tb, Sm, Yb, L 3- edges. The experimental XANES spectra were recorded using the synchrotron radiation source ANKA (Karlsruhe Institute of Technology) and the X-ray laboratory spectrometer Rigaku R- XAS. By comparing the absorption edge energies and white line intensities of the silicates with the ones of reference spectra the oxidation state of lanthanides Eu, Ce, Tb, Sm, Yb has been found to be equal to +3 in all investigated silicates except of the Ce-containing silicate from the run in Cu container where the cerium oxidation state ranges from +3 (Ce in silicate apatite and in a KCe silicate with Si12O32 layers) to +4 (starting CeO2 or oxidized Ce2O3).

  4. Instrumental analysis of bacterial cells using vibrational and emission Moessbauer spectroscopic techniques

    Energy Technology Data Exchange (ETDEWEB)

    Kamnev, Alexander A. [Laboratory of Biochemistry of Plant-Bacterial Symbioses, Institute of Biochemistry and Physiology of Plants and Microorganisms, Russian Academy of Sciences, 410049 Saratov (Russian Federation)]. E-mail: aakamnev@ibppm.sgu.ru; Tugarova, Anna V. [Laboratory of Biochemistry of Plant-Bacterial Symbioses, Institute of Biochemistry and Physiology of Plants and Microorganisms, Russian Academy of Sciences, 410049 Saratov (Russian Federation); Antonyuk, Lyudmila P. [Laboratory of Biochemistry of Plant-Bacterial Symbioses, Institute of Biochemistry and Physiology of Plants and Microorganisms, Russian Academy of Sciences, 410049 Saratov (Russian Federation); Tarantilis, Petros A. [Laboratory of Chemistry, Department of Science, Agricultural University of Athens, 11855 Athens (Greece); Kulikov, Leonid A. [Laboratory of Nuclear Chemistry Techniques, Department of Radiochemistry, Faculty of Chemistry, M.V. Lomonosov Moscow State University, 119992 Moscow (Russian Federation); Perfiliev, Yurii D. [Laboratory of Nuclear Chemistry Techniques, Department of Radiochemistry, Faculty of Chemistry, M.V. Lomonosov Moscow State University, 119992 Moscow (Russian Federation); Polissiou, Moschos G. [Laboratory of Chemistry, Department of Science, Agricultural University of Athens, 11855 Athens (Greece); Gardiner, Philip H.E. [Division of Chemistry, School of Science and Mathematics, Sheffield Hallam University, Sheffield S1 1WB (United Kingdom)

    2006-07-28

    In biosciences and biotechnology, the expanding application of physicochemical approaches using modern instrumental techniques is an efficient strategy to obtain valuable and often unique information at the molecular level. In this work, we applied a combination of vibrational (Fourier transform infrared (FTIR), FT-Raman) spectroscopic techniques, useful in overall structural and compositional analysis of bacterial cells of the rhizobacterium Azospirillum brasilense, with {sup 57}Co emission Moessbauer spectroscopy (EMS) used for sensitive monitoring of metal binding and further transformations in live bacterial cells. The information obtained, together with ICP-MS analyses for metals taken up by the bacteria, is useful in analysing the impact of the environmental conditions (heavy metal stress) on the bacterial metabolism and some differences in the heavy metal stress-induced behaviour of non-endophytic (Sp7) and facultatively endophytic (Sp245) strains. The results show that, while both strains Sp7 and Sp245 take up noticeable and comparable amounts of heavy metals from the medium (0.12 and 0.13 mg Co, 0.48 and 0.44 mg Cu or 4.2 and 2.1 mg Zn per gram of dry biomass, respectively, at a metal concentration of 0.2 mM in the medium), their metabolic responses differ essentially. Whereas for strain Sp7 the FTIR measurements showed significant accumulation of polyhydroxyalkanoates as storage materials involved in stress endurance, strain Sp245 did not show any major changes in cellular composition. Nevertheless, EMS measurements showed rapid binding of cobalt(II) by live bacterial cells (chemically similar to metal binding by dead bacteria) and its further transformation in the live cells within an hour.

  5. Spectroscopy

    DEFF Research Database (Denmark)

    Berg, Rolf W.

    This introductory booklet covers the basics of molecular spectroscopy, infrared and Raman methods, instrumental considerations, symmetry analysis of molecules, group theory and selection rules, as well as assignments of fundamental vibrational modes in molecules.......This introductory booklet covers the basics of molecular spectroscopy, infrared and Raman methods, instrumental considerations, symmetry analysis of molecules, group theory and selection rules, as well as assignments of fundamental vibrational modes in molecules....

  6. {sup 237}Np and {sup 57}Fe Moessbauer study of NpFeGa{sub 5}

    Energy Technology Data Exchange (ETDEWEB)

    Homma, Y., E-mail: yhomma@imr.tohoku.ac.jp [Tohoku University, Institute for Materials Research (Japan); Nakada, M. [Japan Atomic Energy Research Institute, Nuclear Science and Engineering Directorate (Japan); Nakamura, A. [Japan Atomic Energy Research Institute, Advance Science Research Center (Japan); Nasu, S.; Aoki, D. [Tohoku University, Institute for Materials Research (Japan); Sakai, H.; Ikeda, S.; Yamamoto, E.; Haga, Y.; Onuki, Y. [Japan Atomic Energy Research Institute, Advance Science Research Center (Japan); Shiokawa, Y. [Tohoku University, Institute for Materials Research (Japan)

    2006-02-15

    {sup 57}Fe and {sup 237}Np Moessbauer Omeasurements have been performed for NpFeGa{sub 5}, which is one of the so-called neptunium 1-1-5 compounds. The {sup 57}Fe Moessbauer spectra below T{sub N} = 118 K show the magnetically ordered state. The magnitude of the hyperfine magnetic field at the {sup 57}Fe nucleus is determined to be 1.98 {+-} 0.05 T at 10 K. From the {sup 237}Np Moessbauer spectrum at 10 K, the hyperfine magnetic field at the {sup 237}Np nucleus is 203 T and the hyperfine coupling constant is determined to be 237 T/{mu}{sub B} using the Np atomic magnetic moment of 0.86 {mu}{sub B} determined by the neutron diffraction study.

  7. Characterization of alkali-metal and alkaline-earth nitrates by vibrational spectroscopy

    Directory of Open Access Journals (Sweden)

    Martínez, S.

    1992-09-01

    Full Text Available Infrared spectra of sodium and potassium alkaline-metal nitrates and magnesium and calcium alkali-earth nitrates in solid phase had been recorded in order to assign the fundamental bands. The influence of the dispersal médium (alkaline halide, employed in the solid sample preparation have been discussed. The quantitative measurements of the band in ten sities at 1387 cm-1 (present in the I.R. spectra of the four nitrates in KBr médium allowed us to determine the Lambert-Beer law slopes for each compound. These values are differents (bearing in mind experimental random errors, so we have could to affirm the nonexistence of solid solution between the nitrate and the alkaline halide médium. The L-B law obtained by us can be used for the Identification differentiation and quantitative analysis of these nitrates in solid phase, even if they are present in a very low concentration.

    Se ha realizado la asignación de los espectros infrarrojo (IR de los nitratos alcalinos, sódico y potásico, y de los alcalinotérreos, magnésico y cálcico, en estado sólido. Se ha visto la influencia del medio dispersante (haluro alcalino, utilizado en la preparación de la muestra sólida. El estudio cuantitativo de la absorbencia de la banda a 1.387 cm-1 (presente en los espectros IR de los cuatro nitratos en medio KBr permite determinar las pendientes de la Ley de Lambert-Beer Se comprueba que dichas pendientes son diferentes lo que conduce a poder afirmar que no se produce disolución sólida entre el KBr y el nitrato alcalino o alcalinotérreo. La determinación de la ley de Lambert-Beer permite la identificación y el análisis cualitativo y cuantitativo por espectroscopia IR de estos nitratos cuando están presentes en bajas concentraciones en muestras sólidas.

  8. Moessbauer study of Celtic pottery from Bopfingen, Baden-Wuerttemberg, Germany

    Energy Technology Data Exchange (ETDEWEB)

    Friederich, J; Gebhard, R [Archaeologische Staatssammlung Muenchen, 80538 Muenchen (Germany); Riederer, J [Rathgen-Forschungslabor, Schlossstrasse la, 14059 Berlin (Germany); Wagner, F E; Wagner, U [Physik-Department E15, Technische Universitaet Muenchen, 85747 Garching (Germany); Krause, R, E-mail: uwagner@ph.tum.d

    2010-03-01

    In the course of a study of pottery from Celtic Central Europe, we report on an investigation of pottery found in the context of a Celtic ditched square enclosure near the modern town of Bopfingen in Baden-Wurttemberg, Germany. The studied pottery may be visually subdivided into wheel-turned ware, graphite ware, and coarse ware. The Moessbauer spectra are surprisingly uniform, indicating that all types of pottery were fired in a similar manner. Firing in a reducing environment at 800 {sup 0}C was usually followed by re-oxidation during cooling, which leads to unique features in the low temperature Moessbauer patterns.

  9. Transmission of Moessbauer rays through ferromagnets in radio-frequency magnetic field

    Energy Technology Data Exchange (ETDEWEB)

    Dzyublik, A. Ya., E-mail: dzyublik@ukr.net [Institute for Nuclear Research (Ukraine); Sadykov, E. K. [Kazan (Volga region) Federal University (Russian Federation); Petrov, G. I. [Kazan State Power Engineering University (Russian Federation); Arinin, V. V.; Vagizov, F. G. [Kazan (Volga region) Federal University (Russian Federation); Spivak, V. Yu. [Institute for Nuclear Research (Ukraine)

    2013-08-15

    The transmission of Moessbauer radiation through a thick ferromagnetic crystal, exposed to a radio-frequency (rf) magnetic field, is studied. The quantum-mechanical dynamical scattering theory is developed, taking into account the periodical reversals of the magnetic field at the nuclei. The Moessbauer forward scattering (FS) spectra of the weak ferromagnet FeBO{sub 3} placed into rf field are measured. It is found that the coherent gamma wave in the crystal absorbs or emits only couples of the rf photons. As a result, the FS spectra consist of equidistant lines spaced by twice the frequency of the rf field in contrast to the absorption spectra.

  10. Moessbauer absorption by thick ferromagnets in radio-frequency magnetic field

    CERN Document Server

    Dzyublik, A Y

    2002-01-01

    The dynamical scattering theory is developed for transmission of the Moessbauer radiation through a ferromagnetic absorber of arbitrary thickness whose magnetization periodically reverses under the influence of an external radio-frequency (RF) magnetic field. The thickness dependence of the Moessbauer absorption spectrum as well as the time dependence and energy distribution of the transmitted beam are analyzed. The transmitted spectrum as a function of the frequency of transmitted gamma-quanta, reveals a sideband structure separated by twice the frequency of the RF field, which collapses to a single line at high frequencies.

  11. Moessbauer studies of perovskite Gd sub 0 sub . sub 5 Sr sub 0 sub . sub 5 FeO sub 3 sub - sub y

    CERN Document Server

    Kim, C S; Sur, J C

    2000-01-01

    Perovskite powder Gd sub 0 sub . sub 5 Sr sub 0 sub . sub 5 FeO sub 3 sub - sub y was studied by X-ray diffraction, Moessbauer spectroscopy, vibrating samples magnetometry, and Mohr's salt analysis. Gd sub 0 sub . sub 5 Sr sub 0 sub . sub 5 FeO sub 3 sub - sub y was synthesized by using the solid-solid reaction method. The crystal structure was found to be orthorhombic with lattice parameters, a sub 0 =5.531 A, b sub 0 =5.608 A and c sub 0 =7.724 A. Moessbauer spectra of Gd sub 0 sub . sub 5 Sr sub 0 sub . sub 5 FeO sub 3 sub - sub y have been taken at various temperatures ranging from 4.2 to 600 K. The spectrum pattern at 4.2 K consisted of four sets of six Lorentzians, and the magnetic hyperfine fields are found to be 275, 486, 514 and 540 kOe. The Neel temperature, T sub N , was found to be 478 K. Mohr's salt analysis for Gd sub 0 sub . sub 5 Sr sub 0 sub . sub 5 FeO sub 3 sub - sub y demonstrated the existence of the mixed valence states, Fe sup 3 sup + (73%) and Fe sup 4 sup + (27%), and y=0.11 at room t...

  12. Moessbauer Studies of Stannous Fluoride Reactivity with Synthetic Tooth Enamel - A Model for the Tooth Cavity Protection Actions of Novel Dentifrices

    Energy Technology Data Exchange (ETDEWEB)

    Denes, Georges, E-mail: gdenes@vax2.concordia.ca; Muntasar, Abdualhafeed [Concordia University, Laboratory of Moessbauer Spectroscopy and Solid State Chemistry, Laboratories for Inorganic Materials, Department of Chemistry and Biochemistry (Canada); Kozak, Kathy M.; Baig, Arif A.; White, Donald J. [Procter and Gamble Company (United States)

    2002-06-15

    SnF{sub 2} is an important toothpaste ingredient, added for the provision of clinical efficacy for hard and soft tissue diseases and in breath protection. Synthetic calcium hydroxyapatite powders were exposed to liquid supernates (25 w/w% toothpaste water slurries, centrifuged) of Crest Gum Care (registered) (SnF{sub 2}) dentifrice. One-minute treatments were followed by 3x water washing, centrifugation and lyophilization. Post treatment, powders were analyzed by Moessbauer spectroscopy with 0.5-1 gram of treated apatite powder. Results show that tooth mineral stannous fluoride interactions include: (1) formation of surface reaction products with both Sn(II) and Sn(IV) oxidation states; (2) Sn-F binding on mineral surfaces with no evidence of SnO. The surface binding is, however, not pure Sn-F but contains contributions of other ligands, probably oxygens from surface phosphates or hydroxyl groups. Results also suggest that surface reacted stannous tin is oxidized with time, even when bound as a layer on the tooth surface. This study demonstrates for the first time the presence of Sn-F on tooth enamel post treatment and the contribution of passivation to long term stannous chemistry on tooth surfaces. The study also illustrates the practical applications of the Moessbauer technique.

  13. NMR and Moessbauer Study of Al{sub 2}O{sub 3}-Eu{sub 2}O{sub 3}

    Energy Technology Data Exchange (ETDEWEB)

    Nava, N., E-mail: tnava@imp.mx; Salas, P.; Llanos, M. E. [Programa de Ingenieria Molecular, Instituto Mexicano del Petroleo (Mexico); Perez-Pastenes, H.; Viveros, T. [Universidad Autonoma Metropolitana-Iztapalapa, Departamento de IPH (Mexico)

    2005-02-15

    Alumina-europia mixed oxides with 5 and 10 wt.% Eu{sub 2}O{sub 3} were studied by Moessbauer spectroscopy, {sup 27}Al MAS-NMR and X-ray diffraction (XRD). The samples were prepared by the sol-gel technique. The XRD patterns for the calcined samples show a broad peak around 2{theta} = 30{sup o} which is assigned to the Eu{sub 2}O{sub 3}; after treatment with hydrogen at 1073 K no reduction to Eu{sup +2} or Eu{sup 0} was observed. The NMR spectra show three peaks, which are assigned to the octahedral, pentahedral and tetrahedral aluminum sites; the intensity of each peak depends on the concentration of europium ions. The Moessbauer spectra of the calcined samples show a single peak near zero velocity which is attributed to the Eu{sup +3}; after H{sub 2} treatment at 1073 K similar spectra were obtained, suggesting Eu{sup +3} is not reducibly at this temperature.

  14. Moessbauer and X-ray Study of Fe{sub 1-x}Al{sub x}, 0.2{<=}x{<=}0.5, Samples Produced by Mechanical Alloying

    Energy Technology Data Exchange (ETDEWEB)

    Oyola Lozano, D., E-mail: doyola@ut.edu.co; MartInez, Y. Rojas; Bustos, H.; Perez Alcazar, G. A. [Universidad del Tolima, Departamento de Fisica (Colombia)

    2004-12-15

    In this work we report the magnetic and structural properties obtained by Moessbauer spectroscopy and X-ray diffraction, of the Fe{sub 1-x}Al{sub x}, 0.2{<=}x{<=}0.5, alloys produced by mechanical alloying. Alloys with x=0.2, 0.3, 0.4 and 0.5, were for milled 12, 24, 36, and 48 hours. All the obtained alloys are in the bcc phase. The obtained Moessbauer spectra are characteristic of disordered ferromagnetic system. The lattice parameter remains nearly constant ({approx}2.91 A) for all the milling times and compositions. The mean grain sizes in the (110) and (211) direction are nearly constants with the milling time but vary from 15.5 to 11 nm and from 10.5 to 8.5 nm when Al content grow between x=0.2 to x=0.4, respectively. The difference between the mean grain sizes in these two directions shows that the grains are of prolate spheroid form.

  15. Precise determination of Moessbauer lineshape parameters including interference

    Energy Technology Data Exchange (ETDEWEB)

    Mullen, J.G.; Djedid, A.; Bullard, B.; Schupp, G.; Cowan, D.; Cao, Y.; Crow, M.L.; Yelon, W.

    1987-01-01

    Using 100 Ci /sup 183/Ta and 5 Ci /sup 182/Ta sources, with LiF and NaCl crystal monochromating filters, we have measured the lineshape parameters for the 46.5 keV and 99.1 keV Moessbauer effect (ME) transitions of /sup 183/W and the 100.1 keV transition of /sup 182/W. Using an analytic representation of the convolution integral and utilizing asymptotic analyses of the lineshape, we find, for both transmission and microfoil internal conversion (MICE) experiments, accurate values of all ME parameters including width, position, cross section, and interference. This new approach allows deconvolution of source and absorber spectra and gives a simple analytic expression for both as well as their Fourier transforms. The line widths for the 46.5, 99.1, and 100.1 keV transitions are 3.10(10), 0.369(18), and 0.195(12) cm/s, respectively. The interference parameters are -0.00257(9), -0.0093(12), and -0.0107(12) in the same respective order. The agreement between transmission and MICE measurements for the above lineshape parameters is within the experimental errors. We believe these measurements are the first having sufficient precision to allow a quantitative comparison with dispersion theory and they indicate interference parameters 10 to 20% smaller than predicted. Our measured line widths are less than earlier reported values. This is because our analysis of the true lineshape and the study of line asymptotics permits a quantitative determination of the isomer lifetimes rather than the usual lower bound found in earlier ME experiments. 37 refs., 4 figs., 2 tabs.

  16. Iron Mineralogy and Aqueous Alteration on Mars from the MER Moessbauer Spectrometers. Chapter 15

    Science.gov (United States)

    Morris, Richard V.; Klingelhoefer, Goestar

    2007-01-01

    The twin Mars Exploration Rovers Spirit (Gusev crater) and Opportunity (Meridiani Planum) used MIMOS II Moessbauer spectrometers to analyze martian surface materials in the first application of extraterrestrial Moessbauer spectroscopy. The instruments acquired spectra that identified the speciation of Fe according to oxidation state, coordination state, and mineralogical composition and provided quantitative information about the distribution of Fe among oxidation states, coordination states, and Fe-bearing phases. A total of 12 unique Fe-bearing phases were identified: Fe(2+) in olivine, pyroxene, and ilmenite; Fe(2+) and Fe(3+) in magnetite and chromite; Fe(3+) in nanophase ferric oxide (npOx), hematite, goethite, jarosite, an unassigned Fe3+ sulfate, and an unassigned Fe(3+) phase associated with jarosite; and Fe(0) in kamacite. Weakly altered basalts at Gusev crater (SO3 = 2.5 +/- 1.4 wt.% and Fe(3+)/Fe(sub T) = 0.24 +/- 0.11) are widespread on the Gusev plains and occur in less abundance on West Spur and Husband Hill in the Columbia Hills. Altered low-S rocks (SO3 = 5.2 +/- 2.0 wt.% and Fe(3+)/Fe(sub T) = 0.63 +/- 0.18) are the most common type of rock in the Columbia Hills. Ilm-bearing, weakly altered basalts were detected only in the Columbia Hills, as was the only occurrence of chromite in an altered low-S rock named Assemblee. Altered high-S rocks (SO3 > 14.2 wt.% and Fe(3+)/Fe(sub T) = 0.83 +/- 0.05) are the outcrop rocks of the ubiquitous Burns formation at Meridiani Planum. Two Fe(0)-bearing rocks at Meridiani Planum (Barberton and Heat Shield Rock) are meteorites. Laguna Class soil is weakly altered (SO3 = 6 +/- 2 wt.% and Fe(3+)/Fe(sub T) = 0.29 +/- 0.08) and widely distributed at both Gusev crater and Meridiani Planum, implying efficient global mixing processes or a global distribution of precursor rocks with comparable Fe mineralogical compositions. Paso Robles Class soil is heavily altered (SO3 approx. 31 wt.% and Fe(3+)/Fe(sub T) = 0.83 +/- 0

  17. First-principles calculations of Moessbauer hyperfine parameters for solids and large molecules

    Energy Technology Data Exchange (ETDEWEB)

    Guenzburger, Diana [Centro Brasileiro de Pesquisas Fisicas (CBPF), Rio de Janeiro, RJ (Brazil); Ellis, D.E. [Northwestern Univ., Evanston, IL (United States). Dept. of Physics; Zeng, Z. [Academia Sinica, Hefei, AH (China). Inst. of Solid-State Physics

    1997-10-01

    Electronic structure calculations based on Density Functional theory were performed for solids and large molecules. The solids were represented by clusters of 60-100 atoms embedded in the potential of the external crystal. Magnetic moments and Moessbauer hyperfine parameters were derived. (author) 22 refs., 8 figs., 1 tab.

  18. Moessbauer study on the antiferromagnetic FeO synthesized under high pressure

    Energy Technology Data Exchange (ETDEWEB)

    Yoshikawa, Takuro [University of Tsukuba, Institute of Applied Physics (Japan); Kanke, Yasushi [National Institute of Materials Science (Japan); Yanagihara, Hideto; Kita, Eiji, E-mail: kita@bk.tsukuba.ac.jp [University of Tsukuba, Institute of Applied Physics (Japan); Tsunoda, Yorihiko [Waseda University, School of Science and Engineering (Japan); Siratori, Kiiti [University of Tsukuba, Institute of Applied Physics (Japan); Kohn, Kay [Waseda University, School of Science and Engineering (Japan)

    2012-03-15

    Moessbauer study and magnetic measurements were carried out on the stoichiometric FeO, prepared with the high pressure ({approx}5.5GPa) synthesis technique. Well known defects (Koch-Cohen clusters) in FeO are detected even in the stoichiometric specimen, prepared at high temperatures.

  19. Analysis of earth pigments in Palomino's frescoes in the Santos Juanes Church in Valencia (Spain) by solid state voltammetry and FTIR spectroscopy

    OpenAIRE

    DOMENECH CARBO, ANTONIO; Domenech Carbo, Mª Teresa; Ciarrocchi, Julia; Cialei, Vania; Monteagudo, Antonio

    2006-01-01

    A combination of solid-state voltammetry and Fourier transform infrared spectroscopy in the attenuated total reflectance mode was applied to identify earth pigments in samples from the frescoes of Antonio Palomino (dated 1707) taken from the vault of the Santos Juanes church in Valencia (Spain). Such frescoes suffered considerable damage by fire during the Spanish Civil War in 1936, resulting in severe chemical and chromatic alterations. Se ha utilizado una combinación de voltamperometría ...

  20. Heterogeneous mixed valence in YbPd sub 3 S sub 4 : evidence from sup 1 sup 7 sup 0 Yb Moessbauer and x-ray L sub I sub I sub I -edge absorption measurements

    CERN Document Server

    Bonville, P; Alleno, E; Takahashi, F; Matsuoka, E; Ishikawa, M

    2003-01-01

    The intermetallic bronze YbPd sub 3 S sub 4 is shown to be a heterogeneous mixed-valence system, by means of sup 1 sup 7 sup 0 Yb Moessbauer spectroscopy and x-ray L sub I sub I sub I -edge absorption and magnetic measurements. Two valence states coexist in this compound: Yb sup 3 sup + and close-to-divalent Yb. The trivalent fraction (about 50%) undergoes a transition to magnetic ordering at about 2 K, with the GAMMA sub 7 doublet as the ground crystal field state. The possibility of charge (or valence) ordering is discussed. (letter to the editor)

  1. Moessbauer study of Fe[sub 3-x]Cr[sub x]Si alloys with DO[sub 3]-type ordering. [Fe-Cr-Si

    Energy Technology Data Exchange (ETDEWEB)

    Satula, D.; Szymanski, K.; Dobrzynski, L.; Waliszewski, J. (Faculty of Physics, Warsaw Univ. Branch, Bialystok (Poland))

    1993-02-01

    The influence of chromium atoms substituting for iron in the Fe[sub 3-x]Cr[sub x]Si alloys with DO[sub 3]-type ordering is investigated by Moessbauer spectroscopy at room temperature. Using the correlation between local hyperfine magnetic field and magnetic moments observed for Fe[sub 3]Si it is inferred that the magnetic moment of iron in Fe[sub 3-x]Cr[sub x]Si decreases linearly with x for both (A,C) and B sites. A few models intended to describe an influence of Cr on local hyperfine fields are tested. It is found that the local hyperfine magnetic field depends primarily on the chemical composition of the nearest neighbour shell. The isomer shift and magnetic hyperfine field show no substantial dependence on the alloy composition. Chromium atoms occupy, unexpectedly, both B and (A, C) sites, although the B sites are preferentially occupied. (orig.).

  2. Quadrupole coupling constants and isomeric Moessbauer shifts for halogen-containing gold, platinum, niobium, tantalum and antimony compounds

    Energy Technology Data Exchange (ETDEWEB)

    Poleshchuk, O. K., E-mail: poleshch@tspu.edu.ru [Tomsk State Pedagogical University (Russian Federation); Branchadell, V. [Universitat Autonoma de Barcelona, Departament de Quimica (Spain); Ritter, R. A.; Fateev, A. V. [Tomsk State Pedagogical University (Russian Federation)

    2008-01-15

    We have analyzed by means of Density functional theory calculations the nuclear quadrupole coupling constants of a range of gold, antimony, platinum, niobium and tantalum compounds. The geometrical parameters and halogen nuclear quadrupole coupling constants obtained by these calculations substantially corresponded to the data of microwave and nuclear quadrupole resonance spectroscopy. An analysis of the quality of the calculations that employ pseudo-potentials and all-electron basis sets for the halogen compounds was carried out. The zero order regular approximation (ZORA) method is shown to be a viable alternative for the calculation of halogen coupling constants in molecules. In addition, the ZORA model, in contrast to the pseudo-potential model, leads to realistic values of all metal nuclear quadrupole coupling constants. From Klopman's approach, it follows that the relationship between the electrostatic bonding and covalent depends on the nature of the central atom. The results on Moessbauer chemical shifts are also in a good agreement with the coordination number of the central atom.

  3. Moessbauer study of Martensitic transformation and collective magnetic excitations in Fe9Ni1 fine particles

    Institute of Scientific and Technical Information of China (English)

    H.M.Widatallah; 黄润生; 等

    1996-01-01

    The austenite to martensity ransformation in fine Fe90Ni.10 particles prepared by evaporation is studied by Moessbauer technique.Unlike bulk Fe.9Ni.1 which is entirely transformed to martensite.these particles show a remarkable austenite stability upon cooling upto liquid nitrogen temperature.This stability is associated with the oxide surface layer formed on the particles and also with their small size.A hyperfine field approach is employed to analyze the martensitic transformation in the particles.It is also shown that,in contrast with large particles ,the temperature variation of the Moessbauer average hyperfine field of the fine particles can be satisfactorily explained in terms of the collective magnetic excitations model.

  4. Muon spin relaxation and Moessbauer studies of iron pnictide superconductors

    Energy Technology Data Exchange (ETDEWEB)

    Klauss, Hans-Henning; Maeter, H.; Dellmann, T. [Technische Universitaet, Dresden (Germany); Luetkens, H.; Khasanov, R.; Amato, A. [PSI, Villigen (Switzerland); Pashkevich, Y. [Donetsk Phystech, NASU (Ukraine); Hess, C.; Klingeler, R.; Buechner, B. [IFW, Dresden (Germany); Leithe-Jasper, A.; Rosner, H.; Geibel, C.; Schnelle, W. [MPI-CPfS, Dresden (Germany); Braden, M. [Universitaet Koeln (Germany); Litterst, J. [Technische Universitaet, Braunschweig (Germany)

    2010-07-01

    We have determined the electronic phase diagrams and order parameters of ReO{sub 1-x}F{sub x}FeAs and (Sr,Eu)Fe{sub 2-x}Co{sub x}As{sub 2} superconductors. The results prove an important role of the structural distortion for the SDW magnetism and reveal two gap multiband superconductivity. We examined the interplay of iron and rare earth magnetic order in ReO{sub 1-x}F{sub x}FeAs. The undoped compounds show different magnetic coupling strength of the rare earth ion to the antiferromagnetic iron layers ranging from independent order to strong polarization of the rare earth moments by the ordered iron. Finally, we present recent studies on (Ca,Sr,Ba,Eu)Fe{sub 2}As{sub 2} and (Fe{sub 2}As{sub 2})(Sr{sub 4}T{sub 2}O{sub 6})based pnictide superconductors.

  5. Moessbauer and magnetic studies of cobalt substituted lithium zinc ferrites prepared by citrate precursor method

    Energy Technology Data Exchange (ETDEWEB)

    Soibam, Ibetombi [Department of Physics, Manipur University, Canchipur, Imphal 795003, Manipur (India)], E-mail: ibetombi_phys@rediffmail.com; Phanjoubam, Sumitra [Department of Physics, Manipur University, Canchipur, Imphal 795003, Manipur (India); Prakash, Chandra [Directorate of ER and IPR, DRDO Bhawan, Rajaji Marg, New Delhi 110011 (India)

    2009-05-05

    Nanocrystalline lithium zinc ferrites substituted with cobalt were synthesized by the citrate precursor method. X-ray diffraction was used to confirm the spinel phase. Moessbauer studies at room temperature were carried out to study the effect of cobalt concentration on the various hyperfine interactions. Variation of the saturation magnetization with respect to composition was discussed. The result shows some anomalous behaviour when cobalt is substituted to lithium ferrite in presence of zinc.

  6. 1H and 23Na MAS NMR spectroscopy of cationic species in CO2 selective alkaline earth metal porous silicoaluminophosphates prepared via liquid and solid state ion exchange

    Science.gov (United States)

    Arévalo-Hidalgo, Ana G.; Dugar, Sneha; Fu, Riqiang; Hernández-Maldonado, Arturo J.

    2012-07-01

    The location of extraframework cations in Sr2+ and Ba2+ ion-exchanged SAPO-34 was estimated by means of 1H and 23Na MAS NMR spectroscopy and spectral deconvolution. Incorporation of the alkaline earth metal cations onto the SAPO framework was achieved via liquid state ion exchange, coupled partial detemplation/solid-state ion exchange, and combination of both techniques. MAS NMR revealed that the level of ion exchange was limited by the presence of protons and sodium cations near hexagonal prisms (site SI), which are relatively difficult to exchange with the alkaline earth metal due to steric and charge repulsion criteria. In addition, the presence of ammonium cations in the supercages facilitated the exchange of otherwise tenacious hydrogen as corroborated by unit cell compositional data as well as enhanced CO2 adsorption at low partial pressures. The extraframework ammonium species were produced from partial detemplation of the structure-directing agent employed for the SAPO-34 synthesis, tetraethylammonium.

  7. Detection of rare earth elements in Powder River Basin sub-bituminous coal ash using laser-induced breakdown spectroscopy (LIBS)

    Energy Technology Data Exchange (ETDEWEB)

    Tran, Phuoc [National Energy Technology Lab. (NETL), Pittsburgh, PA, (United State; Mcintyre, Dustin [National Energy Technology Lab. (NETL), Pittsburgh, PA, (United State

    2015-10-01

    We reported our preliminary results on the use of laser-induced breakdown spectroscopy to analyze the rare earth elements contained in ash samples from Powder River Basin sub-bituminous coal (PRB-coal). We have identified many elements in the lanthanide series (cerium, europium, holmium, lanthanum, lutetium, praseodymium, promethium, samarium, terbium, ytterbium) and some elements in the actinide series (actinium, thorium, uranium, plutonium, berkelium, californium) in the ash samples. In addition, various metals were also seen to present in the ash samples

  8. Iron-Sulfur Proteins Investigated by EPR-, Moessbauer- and EXAFS-Spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Wegner, P.; Bever, M.; Schuenemann, V.; Trautwein, A. X. [University of Luebeck, Institute of Physics (Germany); Schmidt, C. [University of Luebeck, Institute of Biochemistry (Germany); Boenisch, H. [Center for Structural Biochemistry, Karolinska Institutet, Dept. of Biosciences at NOVUM (Sweden); Gnida, M.; Meyer-Klaucke, W. [DESY, EMBL Outstation Hamburg (Germany)

    2004-12-15

    The structural and spectroscopic properties of the biologically active [Fe-4S] site of three different mutants of the wild-type rubredoxin from the archaeon Pyrococcus abyssi were investigated and compared with each other and additionally with those of the rubredoxin from the bacterium Clostridium pasteurianum.

  9. Some recent aspects of relaxation line shapes in Moessbauer spectroscopy. [White noise approximation

    Energy Technology Data Exchange (ETDEWEB)

    Shenoy, G.K.; Dunlap, B.D.

    1977-01-01

    Theoretical development in the line shape calculation of Mossbauer resonance spectra involving spin relaxation effects is introduced. The ''eigenvalue'' procedure of calculating line shapes saves computational times by two orders of magnitude compared to traditional methods. This was illustrated by calculating the relaxation spectra of hemoglobin cyanide and a GAMMA/sub 8/ quartet electronic state. The ''white noise approximation'' involved in all the relaxation theory is discussed, and its limitations are pointed out. The theory without such an approximation is used to analyze the data for Cs/sub 2/NaYbCl/sub 6/.

  10. Recent progress on the spectroscopy of rare earth ions in core-shells, nanowires, nanotubes, and other novel nanostructures.

    Science.gov (United States)

    Chen, Xueyuan; Liu, Liqin; Liu, Guokui

    2008-03-01

    Research and development of nanoscale luminescent and laser materials are part of the rapidly advancing nanoscience and nanotechnology. Because of unique spectroscopic properties and luminescent dynamics of f-electron states, doping luminescent rare earth ions into nano-hosts has been demonstrated as an optimistic approach to developing highly efficient and stable nanophosphors for various applications. In this article, we review the most recent progress in spectroscopic measurements of rare earth ion-activated low-dimensional nanostructures including nanolayers, core-shells, nanowires, nanotubes, and nanodisks. Among a large volume of work reported in the literature on many members of the rare earth series including Ce3+, Pr3+, Nd3+, Eu3+, and Er3+, we focus on recent findings in the spectroscopic and luminescence properties of Eu3+ doped nanolayers, core-shells, and nanotubes, because Eu3+ ions have been extensively studied and widely used as an ideal probe for fundamental understanding of nano-phenomena. Specifically, the dependence of the optical properties of rare earth ions on nanostructures is discussed in detail.

  11. [Review on Application of Optical Scattering Spectroscopy for Elastic Wave Velocity Study on Materials in Earth's Interior].

    Science.gov (United States)

    Jiang, Jian-jun; Li, He-ping; Dai, Li-dong; Hu, Hai-ying; Wang, Yan; Zhao, Chao-shuai

    2015-09-01

    In-situ experimental results on the elastic wave velocity of Earth materials at high pressure and high temperature in combination with data from seismic observation can help to inverse the chemical composition, state and migration of materials in Earth's interior, providing an important approach to explore information of deep earth. Applying the Brillouin scattering into the Diamond Anvil Cell (DAC) to obtain the in situ elastic wave velocities of minerals, is the important approach to investigate elastic properties of Earth's Interior. With the development of DAC technology, on the one hand, the high temperature and high pressure experimental environment to simulate different layers of the earth can be achieved; on the other hand, the optical properties of DAC made many kinds of optical analysis and test methods have been widely applied in this research field. In order to gain the elastic wave velocity under high temperature and high pressure, the accurate experimental pressure and heating temperature of the sample in the cavity should be measured and calibrated first, then the scattering signal needs to dealt with, using the Brillouin frequency shift to calculate the velocity in the sample. Combined with the lattice constants obtained from X ray technique, by a solid elastic theory, all the elastic parameters of minerals can be solved. In this paper, firstly, application of methods based on optical spectrum such as Brillouin and Raman scattering in elasticity study on materials in Earth's interior, and the basic principle and research progress of them in the velocity measurement, pressure and temperature calibration are described in detail. Secondly, principle and scope of application of two common methods of spectral pressure calibration (fluorescence and Raman spectral pressure standard) are analyzed, in addition with introduce of the application of two conventional means of temperature calibration (blackbody radiation and Raman temperature scale) in

  12. Low-Spin Ferriheme Models of the Cytochromes: Correlation of Molecular Structure with EPR and Moessbauer Spectral Parameters

    Energy Technology Data Exchange (ETDEWEB)

    Teschner, T.; Trautwein, A. X.; Schuenemann, V. [University of Luebeck, Institute of Physics (Germany); Yatsunyk, L. A.; Walker, F. A. [University of Arizona, Department of Chemistry (United States)

    2004-12-15

    The magnetic Moessbauer spectra of a series of low-spin ferriheme complexes have been investigated and compared with their EPR spectral parameters and molecular structures. To date there has been little systematic analysis of either estimated or fitted values of the hyperfine coupling constants for low-spin ferriheme centers and no meaningful correlation has been established between the Moessbauer parameters and the axial ligands of such species. With the results of the present study, we have been able to find correlations of molecular structures with iron-orbital splittings, g-tensor values derived from EPR signals and magnetic hyperfine interaction components A{sub zz} obtained from magnetic Moessbauer spectra. These correlations should be useful to future workers in the field of heme-containing enzymes.

  13. Triangular Zn{sub 3} and Ga{sub 3} units in Sr{sub 2}Au{sub 6}Zn{sub 3}, Eu{sub 2}Au{sub 6}Zn{sub 3}, Sr{sub 2}Au{sub 6}Ga{sub 3}, and Eu{sub 2}Au{sub 6}Ga{sub 3}. Structure, magnetism, {sup 151}Eu Moessbauer and {sup 69;71}Ga solid state NMR spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Gerke, Birgit; Niehaus, Oliver; Poettgen, Rainer [Muenster Univ. (Germany). Inst. fuer Anorganische und Analytische Chemie; Korthaus, Alexander; Haarmann, Frank [RWTH Aachen Univ. (Germany). Inst. fuer Anorganische Chemie

    2016-08-01

    The gold-rich intermetallic compounds Sr{sub 2}Au{sub 6}Zn{sub 3}, Eu{sub 2}Au{sub 6}Zn{sub 3}, Sr{sub 2}Au{sub 6}Ga{sub 3}, and Eu{sub 2}Au{sub 6}Ga{sub 3} were synthesized from the elements in sealed tantalum ampoules in induction or muffle furnaces. The europium compounds are reported for the first time and their structures were refined from single crystal X-ray diffractometer data: Sr{sub 2}Au{sub 6}Zn{sub 3} type, R anti 3c, a = 837.7(1), c = 2184.5(4) pm, wR2 = 0.0293, 572 F{sup 2} values for Eu{sub 2}Au{sub 6.04}Zn{sub 2.96} and a = 838.1(2), c = 2191.7(5) pm, wR2 = 0.0443, 513 F{sup 2} values for Eu{sub 2}Au{sub 6.07}Ga{sub 2.93} with 20 variables per refinement. The structures consist of a three-dimensional gold network with a 6R stacking sequence, similar to the respective diamond polytype. The cavities of the network are filled in a ratio of 2:1 by strontium (europium) atoms and Ga{sub 3} (Zn{sub 3}) triangles in an ordered manner. Sr{sub 2}Au{sub 6}Zn{sub 3} and Sr{sub 2}Au{sub 6}Ga{sub 3} are diamagnetic with room temperature susceptibilities of -3.5 x 10{sup -4} emu mol{sup -1}. Temperature dependent susceptibility and {sup 151}Eu Moessbauer spectroscopic measurements show a stable divalent ground state for both europium compounds. Eu{sub 2}Au{sub 6}Zn{sub 3} and Eu{sub 2}Au{sub 6}Ga{sub 3} order antiferromagnetically below Neel temperatures of 16.3 and 12.1 K, respectively. Anisotropic electrical conductivity of Sr{sub 2}Au{sub 6}Ga{sub 3} is proven by an alignment of the crystallites in the magnetic field. Orientation-dependent {sup 69;71}Ga NMR experiments combined with quantum mechanical calculations (QM) give evidence for a highly anisotropic charge distribution of the Ga atoms.

  14. Aspartic acid interaction with cobalt(II) in dilute aqueous solution: A {sup 57}Co emission Moessbauer spectroscopic study

    Energy Technology Data Exchange (ETDEWEB)

    Kamnev, Alexander A.; Tugarova, Anna V. [Institute of Biochemistry and Physiology of Plants and Microorganisms, Russian Academy of Sciences (Russian Federation); Kovacs, Krisztina; Homonnay, Zoltan, E-mail: homonnay@ludens.elte.hu; Kuzmann, Erno; Vertes, Attila [Eoetvoes Lorand University, Institute of Chemistry (Hungary)

    2012-03-15

    Emission ({sup 57}Co) Moessbauer spectra of the aspartic acid-{sup 57}CoCl{sub 2} system were measured at T = 80 K in frozen aqueous solution and in the form of a dried residue of this solution. The Moessbauer spectra, besides a weak contribution from after-effects, showed two Fe{sup 2 + }/Co{sup 2 + } components which were ascribed to octahedrally and tetrahedrally coordinated {sup 57}Co{sup II} microenvironments in the Asp-cobalt(II) complex. This dual coordination mode may be due to the involvement of the second terminal carboxylic group of aspartic acid in the coordination sphere of Co.

  15. Co{sup 2 + } interaction with Azospirillum brasilense Sp7 cells: a {sup 57}Co emission Moessbauer spectroscopic study

    Energy Technology Data Exchange (ETDEWEB)

    Kamnev, Alexander A.; Tugarova, Anna V. [Russian Academy of Sciences, Institute of Biochemistry and Physiology of Plants and Microorganisms (Russian Federation); Biro, Borbala [Hungarian Academy of Sciences, Research Institute for Soil Science and Agricultural Chemistry (Hungary); Kovacs, Krisztina, E-mail: kkriszti@chem.elte.hu; Homonnay, Zoltan; Kuzmann, Erno; Vertes, Attila [Eoetvoes Lorand University, Institute of Chemistry (Hungary)

    2012-03-15

    Preliminary {sup 57}Co emission Moessbauer spectroscopic data were obtained for the soil bacterium Azospirillum brasilense Sp7 (T = 80 K) in frozen {sup 57}Co{sup 2 + }-containing suspensions and in their dried residues. The Moessbauer parameters were compared with those for A. brasilense strain Sp245 differing from strain Sp7 by ecological behaviour. Live cells of both strains showed metabolic transformations of {sup 57}Co{sup 2 + } within an hour. Differences in the parameters observed for the two strains under similar conditions suggest dissimilarities in their metabolic response to Co{sup 2 + }.

  16. Moessbauer and mineral magnetic studies on archaeological potteries from Adhichanallur, Tamilnadu, India

    Energy Technology Data Exchange (ETDEWEB)

    Venkatachalapathy, R., E-mail: venkatr5@rediffmail.com [Annamalai University, C.A.S in Marine Biology (India); Bakas, T. [University of Ioannina, Department of Physics (Greece); Basavaiah, N.; Deenadayalan, K. [New Panvel, Indian Institute of Geomagnetism (India)

    2008-09-15

    Megalithic potteries collected from Adhichanallur, Tamilnadu, India (Lat. 8{sup o}44' N; Long. 77{sup o}42' E) have been subjected to various spectroscopic and rock magnetic studies. The type of clay, their origin, level of structural deformation due to firing, firing temperature and atmospheric condition followed during making the potteries are analyzed. The potteries were subjected to Moessbauer and X-ray diffraction studies to analyze the iron phases in them. It is found that the samples were made of local clay (red clay), fired above 600{sup o}C under open atmospheric and/or reduced atmospheric conditions and air has been allowed during cooling. The Moessbauer spectra reveal the presence of Fe{sup 3+}, Fe{sup 2+} and iron oxides of hematite and magnetite. The firing temperature and firing conditions established from Moessbauer studies are similar to the observation made from FT-IR studies. The magnetic mineral types, the mass fractions and the domain states of the constituent magnetic grains were elucidated from a range of rock magnetic measurements including variation of susceptibility with low field, frequency and temperature, hysteresis parameters and isothermal remanence acquisition data. The magnetic mineralogy of most pottery samples was dominated by magnetite/(titano) magnetite, while magnetic grain size spectrum varies from very fine (super paramagnetic) to fine (stable single domain, pseudo single domain). The reversible thermo magnetic behavior reflects no mineralogical transformations during reheating and all the samples show same Curie temperature 580{sup o}C due to magnetite. From the above information it is demonstrated that these samples are suitable for determining the reliable ancient geomagnetic field intensity values existed during that period.

  17. Structure, magnetic properties and Moessbauer spectra of La{sub 0.67}Sr{sub 0.33}Fe{sub x}Mn{sub 1 - x}O{sub 3} manganites oxide prepared by mechanical ball milling method

    Energy Technology Data Exchange (ETDEWEB)

    Cherif, Wajdi, E-mail: wajdi_cherif@yahoo.fr; Ellouze, Mohamed, E-mail: mohamed.ellouze@fss.rnu.tn [Sfax University, Faculty of Sciences (Tunisia); Lehlooh, Abdel-Fatah, E-mail: alehlooh@yahoo.com [King Faisal University (Saudi Arabia); Mahmood, Sami H., E-mail: s.mahmood@ju.edu.jo [The University of Jordan (Jordan); Elhalouani, Foued, E-mail: foued.elhalouani@enis.rnu.tn [National School of Engineers, Sfax University (Tunisia)

    2012-05-15

    La{sub 0.67}Sr{sub 0.33}Fe{sub x}Mn{sub 1-x}O{sub 3}, with x = 0.0, 0.1, 0.2 and 1 have been elaborated by mechanical system. X-ray diffraction, Scanning electron microscopy, Magnetic measurements and Moessbauer spectroscopy for the systems have been investigated. Rietveld analysis of the X-ray powder diffraction show that the samples crystallise in the orthorhombic perovskite system with Pnma space group. The average particle size of about 60 nanometre was obtained from scanning electron microscopy and X-ray diffraction. The investigated samples exhibit a ferromagnetic to paramagnetic transition with increasing temperature. The presence of manganese in the structure leads to an increase of the Curie temperature as well as to spontaneous magnetization. The magnetization versus applied magnetic field shows a small coercive field and an unsaturated magnetization which indicates that the nanoparticles of all samples are superparamagnetic at around room temperature. Room temperature Moessbauer spectra show that the samples with x = 0.1 and x = 1.0 contain minority {alpha}-Fe{sub 2}O{sub 3} and other spinel ferrite species. Also, they indicate that Fe{sup 3 + } ions are present in slightly distorted octahedral sites in the samples with x = 0.1 and 0.2, while mixed Fe valency was observed for the sample with x = 1.0.

  18. Moessbauer- and EPR-Snapshots of an Enzymatic Reaction: The Cytochrome P450 Reaction Cycle

    Energy Technology Data Exchange (ETDEWEB)

    Schuenemann, V. [University of Luebeck, Institute of Physics (Germany); Jung, C. [Max-Delbrueck-Center for Molecular Medicine (Germany); Lendzian, F. [Technical University, PC 14, Max-Volmer Laboratory for Biophysical Chemistry (Germany); Barra, A.-L. [Grenoble High Magnetic Field Laboratory (France); Teschner, T.; Trautwein, A. X. [University of Luebeck, Institute of Physics (Germany)

    2004-12-15

    In this communication we present a complimentary Moessbauer- and EPR-study of the time dependance of the reaction of substrate free P450cam with peracetic acid within a time region ranging from 8 ms up to 5 min. An Fe(IV) species as well as a tyrosyl radical residing on the amino acid residue Tyr96 have been identified as reaction intermediates. These species possibly are formed by the reduction of compound I by means of transferring an electron from Tyr 96 to the heme moiety.

  19. Moessbauer study of a Fe-Zr-B-Cu-(Ge, Co) nanocrystalline alloy series

    Energy Technology Data Exchange (ETDEWEB)

    Blazquez, J.S. [Departamento de Fisica de la Materia Condensada. ICMSE-CSIC. Universidad de Sevilla, Apartado 1065, 41080 Sevilla (Spain); Franco, V. [Departamento de Fisica de la Materia Condensada. ICMSE-CSIC. Universidad de Sevilla, Apartado 1065, 41080 Sevilla (Spain); Conde, A. [Departamento de Fisica de la Materia Condensada. ICMSE-CSIC. Universidad de Sevilla, Apartado 1065, 41080 Sevilla (Spain)]. E-mail: conde@us.es

    2006-09-28

    Amorphous and nanocrystalline Fe-Zr-B-Cu alloys with partial substitution of Co for Fe and Ge for B have been studied by Moessbauer spectrometry (MS). The compositional and microstructural dependence of the different hyperfine parameters were related to the results obtained by X-ray diffraction (XRD) and saturation magnetization measurements. Combination of MS and XRD leads to estimate an interface region, of thickness {approx}0.6 nm. The magnetic moment per transition metal of the crystalline phase is reduced with respect to binary crystalline alloys due to the existence of the interface.

  20. Singular value decomposition approach to the yttrium occurrence in mineral maps of rare earth element ores using laser-induced breakdown spectroscopy

    Science.gov (United States)

    Romppanen, Sari; Häkkänen, Heikki; Kaski, Saara

    2017-08-01

    Laser-induced breakdown spectroscopy (LIBS) has been used in analysis of rare earth element (REE) ores from the geological formation of Norra Kärr Alkaline Complex in southern Sweden. Yttrium has been detected in eudialyte (Na15 Ca6(Fe,Mn)3 Zr3Si(Si25O73)(O,OH,H2O)3 (OH,Cl)2) and catapleiite (Ca/Na2ZrSi3O9·2H2O). Singular value decomposition (SVD) has been employed in classification of the minerals in the rock samples and maps representing the mineralogy in the sampled area have been constructed. Based on the SVD classification the percentage of the yttrium-bearing ore minerals can be calculated even in fine-grained rock samples.

  1. Moessbauer spectra of ferrite catalysts used in oxidative dehydrogenation

    Science.gov (United States)

    Cares, W. R.; Hightower, J. W.

    1971-01-01

    Room temperature Mossbauer spectroscopy was used to examine bulk changes which occur in low surface area CoFe2O4 and CuFe2O4 catalysts as a result of contact with various mixtures of trans-2-butene and O2 during oxidative dehydrogenation reactions at about 420 C. So long as there was at least some O2 in the gas phase, the CoFe2O4 spectrum was essentially unchanged. However, the spectrum changed from a random spinel in the oxidized state to an inverse spinel as it was reduced by oxide ion removal. The steady state catalyst lies very near the fully oxidized state. More dramatic solid state changes occurred as the CuFe2O4 underwent reduction. Under severe reduction, the ferrite was transformed into Cu and Fe3O4, but it could be reversibly recovered by oxidation. An intense doublet located near zero velocity persisted in all spectra of CuFe2O4 regardless of the state of reduction.

  2. Optically active mixed phthalocyaninato-porphyrinato rare-earth double-decker complexes: synthesis, spectroscopy, and solvent-dependent molecular conformations.

    Science.gov (United States)

    Zhang, Xiaomei; Muranaka, Atsuya; Lv, Wei; Zhang, Yuexing; Bian, Yongzhong; Jiang, Jianzhuang; Kobayashi, Nagao

    2008-01-01

    Reaction between the optically active metal-free phthalocyanine with a pi system with noncentrosymmetrical C(2) [corrected] symmetry ((S)- and (R)-H(2){Pc(OBNP)(2)}; OBNP=binaphthylphthalocyanine) and half-sandwich complexes [M(III)(acac)(TClPP)] (M=Y, Eu; TClPP=meso-tetrakis(4-chlorophenyl)porphyrinate; acac=acetylacetonate), which were generated in situ from [M(acac)(3)].n H(2)O and H(2)(TClPP) in n-octanol at reflux, provided the first optically active protonated mixed phthalocyaninato-porphyrinato rare-earth double-decker complexes [M(III)H{Pc(OBNP)(2)}(TClPP)] (M=Y, Eu) in good yield. In addition to electronic absorption spectroscopy and magnetic circular dichroism results, circular dichroism shows different spectroscopic features of these mixed-ring rare-earth double-decker compounds in different solvents, such as DMF and CHCl(3), which was well-reproduced on the basis of time-dependent density functional theory calculation results for the yttrium species (S)-[Y(III){Pc(OBNP)(2)}(Por)](-) (Por=porphyrinate, which is obtained by removing the four chlorophenyl groups from the TClPP ligand) in terms of the change in the rotation angle between the two macrocyclic ligands in the double-decker molecules. These results revealed the solvent-dependent nature of the molecular conformation of mixed-ring rare-earth double-decker complexes, which suggests a new way of tuning the optical and the electrochemical properties of sandwich-type bis(tetrapyrrole)-metal double-decker complexes in solution by changing the solvent.

  3. Anomaly observed in Moessbauer spectra near the neel temperature of FeBr sub 2

    CERN Document Server

    Naili Di

    2003-01-01

    In several decades, iron(II) bromide (FeBr sub 2) has been investigated as a typical Ising-type antiferromagnet by several kinds of experimental techniques. By the Moessbauer measurements, it was normally observed that only the magnetic spectrum appeared just below Neel temperature in FeBr sub 2. However, we found the anomalous spectra, in which paramagnetic component coexisted with magnetic one near Neel temperature. For two kinds of single crystal FeBr sub 2 samples, IM and IIM, we determined the Moessbauer parameters of the observed spectra by the computer analyses: the relative absorption intensity I sub p of the paramagnetic component to the total absorption area of the best fitting spectrum and the value of the hyperfine field H sub h sub f of the magnetic component and values of the quadrupole splitting 1/2 centre dot e sup 2 qQ of the magnetic and the paramagnetic components. The temperature variation of H sub h sub f is unique and the same as that observed for the sample in which the anomaly was not ...

  4. Moessbauer study of the cubic Laves phase intermetallic compound TmFe/sub 2/

    Energy Technology Data Exchange (ETDEWEB)

    Bleaney, B.; Bowden, G.J.; Cadogan, J.M. (New South Wales Univ., Kensington (Australia). School of Physics); Day, R.K.; Dunlop, J.B. (Commonwealth Scientific and Industrial Research Organization, Lindfield (Australia). Div. of Applied Physics)

    1982-04-01

    The results of a /sup 169/Tm and /sup 57/Fe Moessbauer study of the cubic Laves compound TmFe/sub 2/ over the temperature range 1.3-550 K are presented and discussed. The new results are used, in conjunction with existing NMR, Moessbauer and magnetic anisotropy data for TmFe/sub 2/ and Tm metal, to deduce a value of Psub(4f) 536 +- 14 MHz for the saturation value of the first excited state of the /sup 169/Tm nucleus. Estimates are also given for the exchange field ..mu..sub(B)Bsub(ex)(T = O K)/ksub(B) = 153 +- 3 K acting on the Tm/sup 3 +/ ion in TmFe/sub 2/, the quadrupole moment of the I = 3/2 state of the /sup 169/Tm nucleus. Q = -1.36 +- 0.11 b, and the lattice contribution to the nuclear quadrupole interaction in Tm metal, Psub(c) = -54.8 +- 5 MHz (for Q = -1.20 +- 0.07 b) and Psub(c) = -61 +- 8 MHz (for Q = -1.36 +- 0.11 b). In addition estimates are given for the various transferred and parent hyperfine fields in TmFe.

  5. Design and Construction of an Autonomous Control System for Moessbauer Spectrometry

    Energy Technology Data Exchange (ETDEWEB)

    Velasquez, A. A., E-mail: avelasq@fisica.udea.edu.co; Trujillo, J. M.; Morales, A. L.; Tobon, J. E.; Reyes, L. [Universidad de Antioquia, Grupo de Instrumentacion Cientifica y Microelectronica (Colombia); Gancedo, J. R. [Consejo Superior de Investigaciones Cientificas, Instituto de Quimica-Fisica, ' Rocasolano' (Spain)

    2005-02-15

    An autonomous control system for Moessbauer spectrometry based on two modules has been designed and built. The first module operates as a multichannel analyzer for the acquisition and storage of spectra, and the second one is a driver unit which controls and supplies the power for the velocity transducer. A microcontroller executes the digital control algorithm for the velocity transducer motion and manages the data acquisition and storage tasks. The user can monitor the system from an external PC through the serial port. A graphic interface made with the LabVIEW software allows the user to adjust digitally the control parameters for the velocity transducer motion, the channels number, to visualize as well as save spectra in a file. The microcontroller can be reprogrammed from the PC through the same serial port without intervention of a universal programmer, which allows the user to make proper software for different applications of the system. The system has been tested for linearity with several standard absorbers yielding satisfactory results. The low cost of its design, construction and maintenance make this equipment to be an attractive choice when assembling a Moessbauer spectrometer.

  6. On Spin Hamiltonian fits to Moessbauer spectra of high-spin Fe(II) porphyrinate systems

    Energy Technology Data Exchange (ETDEWEB)

    Schulz, Charles E., E-mail: cschulz@knox.edu [Knox College, Department of Physics (United States); Hu Chuanjiang, E-mail: scheidt.1@nd.edu; Scheidt, W. Robert [University of Notre Dame, Department of Chemistry and Biochemistry (United States)

    2006-06-15

    Fits to Moessbauer spectra of high-spin iron(II) porphyrinates have been applied to the Fe(II) model compounds octaethylporphyrin(1,2-dimethylimidazole) and tetra-paramethoxyporphyrin(1,2-dimethylimidazole). Moessbauer spectra have been measured on these compounds at 4.2 K in large applied fields. Spin Hamiltonians were used for fitting both the electronic and nuclear interactions. The fits are done by adjusting the Hamiltonian parameters to simultaneously minimize the total {chi}{sup 2} for three different applied fields. In order to get best fits, the EFG tensor need to be rotated relative to the ZFS tensor. A comparative sensitivity analysis of their Spin Hamiltonian parameters has also been done on the ZFS parameters D, and the EFG asymmetry parameter {eta}. The best fits suggest that both systems definitely have a negative quadrupole splitting, and that largest EFG component is tilted far from the z-axis of the ZFS tensor, which is likely to be near the heme normal.

  7. A study of J-coupling spectroscopy using the Earth's field nuclear magnetic resonance inside a laboratory.

    Science.gov (United States)

    Liao, Shu-Hsien; Chen, Ming-Jye; Yang, Hong-Chang; Lee, Shin-Yi; Chen, Hsin-Hsien; Horng, Herng-Er; Yang, Shieh-Yueh

    2010-10-01

    In this paper, an instrumentation of the Earth's field nuclear magnetic resonance (EFNMR) inside a laboratory is presented. A lock-in analysis (LIA) technique was proposed to enhance the signal-to-noise ratio (SNR). A SNR of 137.8 was achieved in a single measurement for 9 ml tap water, and the LIA technique significantly enhanced the SNR to 188 after a 10-average in a noisy laboratory environment. The proton-phosphorus coupling in trimethyl phosphate ((CH(3)O)(3)PO) with J-coupling J[H,F]=(10.99±0.013) Hz has been demonstrated. The LIA technique improves the SNR, and a 2.6-fold improvement in SNR over that of the frequency-adjusted averaging is achieved. To reduce the noise in EFNMR, it was suggested that the LIA technique and the first order gradient shim be used to achieve a subhertz linewidth.

  8. Thermal Emission Spectroscopy (5.2 To 38 Microns) And Analysis Of 10 Near-earth Asteroids

    Science.gov (United States)

    Dave, Riddhi; Emery, J.; Cruikshank, D.; Mueller, M.; Delbo, M.; Trilling, D. E.; Mommert, M.

    2010-10-01

    Near Earth Asteroids (NEAs- 0.983AUSolar System. Information about the albedo and size distribution of the NEAs is an essential prerequisite for exploring their physical nature, thermal properties, mineralogy, taxonomy and for developing reliable NEA population models. In support of the ExploreNEOs campaign of the Warm Spitzer program, we will present initial results from study of a sample of NEAs using the Infrared Spectrograph (IRS) on NASA's Spitzer Space Telescope [Programs 88 and 91- Extinct Comets and Low-Albedo Asteroids]. These data were reduced with Spitzer IRS Custom Extraction (SPICE) a JAVA-based tool built for interactive extraction of Spitzer IRS spectra. The 5.2-38 m thermal emission spectra[R 60-130] have been fitted with models of the thermal continuum employing the Near Earth Asteroid Thermal Model [NEATM](Harris 1998) and a Thermophysical model. Simultaneous measurements of the asteroid flux in the thermal infrared, combined with a thermal model, allow both the diameter and the albedo to be determined. The sample of Asteroids to be a part of this study are 1602 Geographos, 1580 Betulia, 433 Eros, 2212 Hephaistos, 1685 Toro, 1917 Cuyo, 1566 Icarus, 3200 Phaethon, 7092 Cadmus and 1866 Sisyphus. This study will give in-depth understanding of the applicability of the NEATM for NEAs observed at higher phase angles, having larger thermal inertia than main-belt asteroids, and/or displaying varied geometries. This work is based on observations made with the Spitzer Space Telescope, which is operated by the Jet Propulsion Laboratory, California Institute of Technology under a contract with NASA.

  9. Mapping of rare earth elements in nuclear waste glass–ceramic using micro laser-induced breakdown spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Wang, X.; Motto-Ros, V. [ILM, UMR5306, Université Lyon 1 — CNRS, Université de Lyon, F-69622, Lyon (France); Panczer, G., E-mail: gerard.panczer@univ-lyon1.fr [ILM, UMR5306, Université Lyon 1 — CNRS, Université de Lyon, F-69622, Lyon (France); De Ligny, D.; Yu, J.; Benoit, J.M. [ILM, UMR5306, Université Lyon 1 — CNRS, Université de Lyon, F-69622, Lyon (France); Dussossoy, J.L.; Peuget, S. [CEA, DEN, DTCD/SECM/LMPA-Marcoule, F-30207 Bagnols-sur-Cèze (France)

    2013-09-01

    A micro-LIBS system was set up based on a quadruple Nd:YAG laser at 266 nm coupled with a microscope. Elemental mapping was performed on a Mo-rich glass–ceramic sample containing CaMoO{sub 4} crystallites hundreds of microns in length and about 25 μm in section diameter. The topography of single-shot laser-induced craters was characterized using an atomic force microscope (AFM), which revealed a crater size less than 7 μm. Mappings of Mo, Ca, Sr, Al, Fe, Zr and rare earth elements such as Eu, Nd, Pr and La were undertaken. Laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) was conducted to validate the micro-LIBS analysis. Principal components analysis calculation was used to investigate the correlation of elements in the two phases of glass–ceramic. Correlation between Ca, Sr, rare earth elements and Mo indicates their preferential incorporation into the calcium molybdate crystalline phase. Anti-correlation between Fe, Zr, Al and Mo revealed their affinity to the glass phase. - Highlights: • A dedicated micro-LIBS system was set up to perform fast elemental mapping. • Mapping was conducted on a Mo-rich nuclear waste glass–ceramic for the first time. • Mo, Ca, Sr, Eu, Nd, La, Pr, Al, Fe and Zr were detected in one spectral range. • Crater size was about 5 μm on crystallites of the sample. • Fractionation behavior of elements was investigated by principal components analysis.

  10. Raman spectroscopy of rare-earth orthoferrites R FeO3 (R =La, Sm, Eu, Gd, Tb, Dy)

    Science.gov (United States)

    Weber, Mads Christof; Guennou, Mael; Zhao, Hong Jian; Íñiguez, Jorge; Vilarinho, Rui; Almeida, Abílio; Moreira, Joaquim Agostinho; Kreisel, Jens

    2016-12-01

    We report a Raman scattering study of six rare-earth orthoferrites R FeO3, with R = La, Sm, Eu, Gd, Tb, Dy. The use of extensive polarized Raman scattering of SmFeO3 and first-principles calculations enable the assignment of the observed phonon modes to vibrational symmetries and atomic displacements. The assignment of the spectra and their comparison throughout the whole series allow correlating the phonon modes with the orthorhombic structural distortions of R FeO3 perovskites. In particular, the positions of two specific A g modes scale linearly with the two FeO6 octahedra tilt angles, allowing the distortion to be tracked throughout the series. At variance with literature, we find that the two octahedra tilt angles scale differently with the vibration frequencies of their respective A g modes. This behavior, as well as the general relations between the tilt angles, the frequencies of the associated modes, and the ionic radii are rationalized in a simple Landau model. The reported Raman spectra and associated phonon-mode assignment provide reference data for structural investigations of the whole series of orthoferrites.

  11. Broadband Transmission Spectroscopy of the super-Earth GJ 1214b suggests a Low Mean Molecular Weight Atmosphere

    CERN Document Server

    Croll, Bryce; Jayawardhana, Ray; Kempton, Eliza Miller-Ricci; Fortney, Jonathan J; Murray, Norman; Neilson, Hilding

    2011-01-01

    We used WIRCam on CFHT to observe four transits of the super-Earth GJ 1214b in the near-infrared. For each transit we observed in two bands nearly-simultaneously by rapidly switching the WIRCam filter wheel back and forth for the duration of the observations. By combining all our J-band (~1.25 microns) observations we find a transit depth in this band of 1.338\\pm0.013% - a value consistent with the optical transit depth reported by Charbonneau and collaborators. However, our best-fit combined Ks-band (~2.15 microns) transit depth is deeper: 1.438\\pm0.019%. Formally our Ks-band transits are deeper than the J-band transits observed simultaneously by a factor of 1.072\\pm0.018 - a 4-sigma discrepancy. The most straightforward explanation for our deeper Ks-band depth is a spectral absorption feature from the limb of the atmosphere of the planet; for the spectral absorption feature to be this prominent the atmosphere of GJ 1214b must have a large scale height and a low mean molecular weight. That is, it would have ...

  12. Sorption Characteristics of Rare Earth Element Eu3+ onto Silica-Water Interfaces Studied by Fluorescence Spectroscopy

    Institute of Scientific and Technical Information of China (English)

    Yin Xiulan; Hu Ping; Li Dien

    2004-01-01

    The sorption of Eu species onto nano-size silica-water interfaces was investigated using fluorescence spectroscopy for Ph ranges of 1-8.5 and an initial Eu concentration (Ceu) of 2×10-4 M. The sorption rate of Eu was initially low, but significantly increased at Ph>4. The sorption density of Eu species on a silica surface was ~1.58×10-7 mol/m2 when the dissolved Eu species were completely sorbed onto silica-water interfaces at Ph=~5.8. The sorbed Eu species at Ph<6 is aquo Eu3+, which is sorbed onto silica-water interfaces as an outer-sphere complex at Ph<5, but may be sorbed as an inner-sphere bidentate complex at 5

  13. Crystal structure and magnetic properties of Mo-substituted 'Ba{sub 2}(Fe,W){sub 2}O{sub 6}' double-perovskites: a synchrotron diffraction, magnetization and Moessbauer study

    Energy Technology Data Exchange (ETDEWEB)

    Rammeh, N.; Bramnik, K.G.; Ehrenberg, H.; Stahl, B.; Fuess, H.; Cheikh-Rouhou, A

    2004-01-28

    Synchrotron diffraction and Moessbauer spectroscopy on Ba{sub 2}(Fe,W){sub 2}O{sub 6} confirmed an Fe excess in this double-perovskite, better described as Ba{sub 2}Fe(Fe{sub x}W{sub 1-x})O{sub 6-{delta}} with x=0.2. The crystal structure is cubic (Fm3-bar m) down to 10 K, and a recently reported tetragonal structure of Ba{sub 2}FeWO{sub 6} is critically reviewed. Magnetic properties of Ba{sub 2}(Fe,W{sub 1-x}Mo{sub x}){sub 2}O{sub 6} compounds were studied by SQUID measurements and revealed weak ferromagnetism at low temperatures, and T{sub C} increases with more substitution of Mo for W.

  14. Structures and Spectroscopy Studies of Two M(II-Phosphonate Coordination Polymers Based on Alkaline Earth Metals (M = Ba, Mg

    Directory of Open Access Journals (Sweden)

    Kui-Rong Ma

    2013-01-01

    Full Text Available The two examples of alkaline-earth M(II-phosphonate coordination polymers, [Ba2(L(H2O9]·3H2O (1 and [Mg1.5(H2O9]·(L-H21.5·6H2O (2 (H4L = H2O3PCH2N(C4H8NCH2PO3H2, N,N′-piperazinebis(methylenephosphonic acid, (L-H2 = O3PH2CHN(C4H8NHCH2PO3 have been hydrothermally synthesized and characterized by elemental analysis, FT-IR, PXRD, TG-DSC, and single-crystal X-ray diffraction. Compound 1 possesses a 2D inorganic-organic alternate arrangement layer structure built from 1D inorganic chains through the piperazine bridge, in which the ligand L−4 shows two types of coordination modes reported rarely at the same time. In 1, both crystallographic distinct Ba(1 and Ba(2 ions adopt 8-coordination two caps and 9-coordination three caps triangular prism geometry structures, respectively. Compound 2 possesses a zero-dimensional mononuclear structure with two crystallographic distinct Mg(II ions. Free metal cations   [MgO6]n2+ and uncoordinated anions (L-H2n2- are joined together by static electric force. Results of photoluminescent measurement indicate three main emission bands centered at 300 nm, 378.5 nm, and 433 nm for 1 and 302 nm, 378 nm, and 434.5 nm for 2 (λex=235 nm, respectively. The high energy emissions could be derived from the intraligand π∗-n transition stations of H4L (310 nm and 382 nm, λex=235 nm, while the low energy emission (>400 nm of 1-2 may be due to the coordination effect with metal(II ions.

  15. Moessbauer study of Fe{sup 3+}/Fe{sup 2+} ratio in amphiboles to search correlation with hydrogen isotope fractionation

    Energy Technology Data Exchange (ETDEWEB)

    Waczek, Zsofia [University of Lausanne, Institut de Mineralogie et Geochimie, Anthropole (Switzerland); Kuzmann, Ernoe; Homonnay, Zoltan, E-mail: homonnay@ludens.elte.hu [Eoetvoes University, Institute of Chemistry (Hungary); Vennemann, Torsten [University of Lausanne, Institut de Mineralogie et Geochimie, Anthropole (Switzerland)

    2009-04-15

    There is a general lack of understanding of the hydrogen isotope fractionations between different experimental approaches both at higher and at lower temperatures of exchange. The complexity of bonding related with the hydroxyl ion in most hydrous minerals makes theoretical treatments rather difficult. Though some of the differences between experimental findings have recently been shown to be related to pressure effects that influence the hydrogen isotope fractionation properties of water, some other factors may also have significance. One of the major unknowns is the compositional control, especially the Fe-content and effects of variable Fe{sup 3+}/Fe{sup 2+} ratios on hydrogen isotope fractionations between minerals and fluids (Suzuoki and Epstein, Geochim Cosmochim Acta 40:1229-1240, 1976; Chacko et al. 2001). We have studied a series of amphibole samples by Moessbauer spectroscopy, EPMA and TC-EA-IRMS to examine for possible correlations between D/H fractionation and Fe{sup 2+} to Fe{sup 3+} ratio/total iron content. Our measurements show that this correlation may exist for one particular origin of samples, but local conditions of mineral formation (most probably chemical composition and reactions accompanying the formation of minerals) may be more important in controlling the hydrogen isotope composition of minerals.

  16. Crystallization and Moessbauer studies of the Fe sub 7 sub 8 Al sub 4 Nb sub 5 B sub 1 sub 2 Cu sub 1 alloy

    CERN Document Server

    Kim, C S; Kim, S B; Park, J Y; Kim, K Y; Noh, T H; Oak, H N

    1998-01-01

    A melt-spun Fe sub 7 sub 8 Al sub 4 Nb sub 5 B sub 1 sub 2 Cu sub 1 alloy with an ultra-thin ribbon has been studied by x-ray diffraction, Moessbauer spectroscopy, and vibrating sample magnetometry. The average hyperfine field H sub h sub f (T) of the amorphous state shows temperature dependence of [H sub h sub f (T) - H sub h sub f (0)]/H sub h sub f (0) -0.53(T/T sub c) sup 3 sup / sup 2 - 0.21(T/T sub c < 0.7, indicative of spin-wave excitation. The quadrupole splitting just above the Curie temperature Tc is 0.42 mm/s, whereas the quadrupole shift below T sub c is zero. The Curie and the crystallization temperature are T sub c = 450 K and T sub x = 703 K, respectively, for a heating rate of 5 K/min. The occupied area ratio of the alpha-Fe phase flash-annealed at 723 K is 59% and remains unchanged. The crystallization temperature of the flash-annealed alloy becomes lower, and the formation of an alpha-Fe is easier than that of the conventional alloy. The flash-annealing technique is effective in improvin...

  17. Bonding and Moessbauer Isomer Shifts in (Hg,Pb)—1223 Cuprate

    Institute of Scientific and Technical Information of China (English)

    高发明; 田永君; 谌岩; 李东春; 董海峰; 张思远

    2003-01-01

    By using the chemical bond theory of dielectric description,the chemical bond parameters of(Hg,Pb)-1223 were calculated.The results show that the(Ba,Sr)-O and Ca-0 types of bond have higher ionic character,while the Cu-O and(Hg,Pb)-0 types of bond have more covalent character.Moessbauer isomer shifts of 57Fe and 119Sn doped in(Hg,Pb)-1223 were calculated by using the chemical environmental factor,he,defined by covalency and electronic polarizability.Four valence state tin and three valence iron sites were identified in 57Fe and 119Sn doped(Hg,Pb)-1223 superconductor.It can be concluded that all of the Fe atoms substitute the Cu at square planar Cu(1) site,Whereas Sn prefers to substitute the square pyramidal Cu(2) site.

  18. Moessbauer hyperfine spectra of DyCo/sub 2/Si/sub 2/

    Energy Technology Data Exchange (ETDEWEB)

    Boge, M.; Chappert, J. (CEA Centre d' Etudes Nucleaires de Grenoble, 38 (France). Dept. de Recherche Fondamentale); Asch, L.; Kalvius, G.M. (Technische Univ. Muenchen, Garching (Germany, F.R.). Fakultaet fuer Physik); Gal, J. (Israel Atomic Energy Commission, Beersheba. Nuclear Research Center-Negev); Goerlich, E.A. (Uniwersytet Jagiellonski, Krakow (Poland). Inst. Fizyki)

    1983-12-01

    Moessbauer spectra of /sup 161/Dy in DyCo/sub 2/Si/sub 2/ were taken between 4.2 K and 78 K. The tetragonal intermetallic has a Neel temperature of Tsub(N)=21 K. Up to 25 K spectra are characterized by extremely slow electronic relaxation, precluding the usual collapse of hyperfine splitting on approaching Tsub(N). Between Tsub(N) and 78 K relaxation spectra are seen. The most unusual feature is a slow, steady decrease of Bsub(hf) and e/sup 2/qQ with temperature. It is suggested that this arises from changes in the wave function of the electronic ground state by influences of the molecular and the crystalline electric fields.

  19. A Moessbauer study of the chemical stability of iron oxide nanoparticles in PMMA and PVB beads

    Energy Technology Data Exchange (ETDEWEB)

    Chen Wei [Department of Physics, Technical University of Denmark, Building 307, DK-2800 Kongens Lyngby (Denmark); College of Physics Science and Information Engineering, Hebei Normal University, Shijiazhuang 050016 (China); Morup, Steen [Department of Physics, Technical University of Denmark, Building 307, DK-2800 Kongens Lyngby (Denmark); Hansen, Mikkel F. [Department of Micro and Nanotechnology, Technical University of Denmark, DTU Nanotech, Building 345 East, DK-2800 Kongens Lyngby (Denmark)], E-mail: mfh@mic.dtu.dk; Banert, Tobias; Peuker, Urs A. [Institute of Chemical Engineering, Clausthal University of Technology, D-38678 Clausthal-Zellerfeld (Germany)

    2008-08-15

    We have prepared magnetic beads consisting of iron oxide nanoparticles in a polymethyl methacrylate (PMMA) and a polyvinyl butyral (PVB) matrix. High-field Moessbauer studies show that the particles have an almost perfect collinear spin structure and magnetization measurements show that they are superparamagnetic at room temperature at a time scale of seconds. We have followed the oxidation of the particles, which initially have a stoichiometry close to magnetite. The oxidation is fast during the first 2-3 weeks and then continues slowly such that even after 30 weeks the particles have not completely transformed to maghemite. The PVB beads are hydrophilic and biocompatible and are therefore well suited for applications in medicine and biology.

  20. Powders with superparamagnetic Fe{sub 3}C particles studied with Moessbauer spectrometry

    Energy Technology Data Exchange (ETDEWEB)

    David, B; Schneeweiss, O [Institute of Physics of Materials, Academy of Sciences of the Czech Republic, v.v.i., Ziz' kova 22, CZ-61662 Brno (Czech Republic); Dumitrache, F; Fleaca, C; Alexandrescu, R; Morjan, I [National Institute for Lasers, Plasma and Radiation Physics, PO Box MG-36, 077125 Bucharest-Magurele (Romania)

    2010-03-01

    Two nanopowders with superparamagnetic Fe{sub 3}C particles were synthesised by the method of laser-induced pyrolysis of gaseous precursors. Both were characterised by X-ray diffraction, Moessbauer spectrometry and standard magnetic measurements. The mean crystallite size of Fe{sub 3}C was 3 nm for the first sample and 10 nm for the second sample (Scherrer formula), i.e. it was lower than in our previously studied ferromagnetic Fe{sub 3}C-based sample. Fe{sub 3}C phase in both present samples exhibited by {approx}20 K reduced Curie temperature which is interpreted as a nanosize effect. After annealing of the samples at 1073 K for 30 minutes the Curie temperature of the Fe{sub 3}C phase in both samples matched its standard bulk value. Beside Fe{sub 3}C phase also Fe{sub 3}O{sub 4} and carbon black were present in the synthesised samples.

  1. Comparative Moessbauer study of the oxidation of pyrite under different conditions

    Energy Technology Data Exchange (ETDEWEB)

    Gracia, M.; Gancedo, J.R.; Martinez-Alonso, A.; Tascon, J.M.D. (Instituto de Quimica Fisica ' Rocasolano' , Madrid (Spain))

    1990-07-01

    Samples of pyrite-rich brown coal from As Pontes and Meirama coalfields (Spain) were oxidized either by air at atmospheric pressure or by a cool oxygen plasma generated by radiofrequency activation. Despite the very different nature and characteristics of the oxidizing media, in both cases the RT Moessbauer spectra were easily fitted to two doublets, whose parameters matched those of pyrite and jarosite (hydrated iron (III) sulphate). The extent of pyrite oxidation to jarosite was monitored by the relative spectral areas of pyrite and jarosite doublets. Both, air and plasma, oxidized pyrite to the same extent and in a similar way, in contrast to coal organic matter, which was scarcely modified by air but completely oxidized by the plasma at the same temperature (ca. 423 K). The incomplete oxidation of pyrite by plasma is attributed to the action of a thin calcium sulphate layer which hinders the access of activated oxygen to small pyrite crystals. 18 refs., 3 tabs., 2 figs.

  2. Preparation of the electroplated Ni and Co films for applying betavoltaic battery and Moessbauer source

    Energy Technology Data Exchange (ETDEWEB)

    Uhm, Young Rang; Choi, Sang Mu; Kim, Jin Joo; Kim, Jong Bum; Son, Kwang Jae; Hong, Jintae [Korea Atomic Energy Research Institute, Daejeon (Korea, Republic of)

    2016-10-15

    The reverse occurs at the anode where metallic nickel is dissolved to form divalent positively charged ions that enter the solution. The nickel ions discharged at the cathode are replenished by those formed at the anode. In this study, a Co-and Ni- plating solution is prepared using two different baths. One is the acid-based buffer (pH 3-4) containing boric acid, sodium chloride, and saccharin. The rest is the base-based buffer (pH 10) containing hydrazine hydrate and ammonium citrate. The optimization of the electroplating parameters for the deposition of Co on plate was considered as indispensable. A betavoltaic battery was fabricated using Ni-63 attached on a P-N junction semiconductor, and the I-V characteristics were measured using a probe station. The thickness-dependent self-shielding effect of the radioisotope layer was investigated. Also, the aim of this work was determination of the optimal parameters for thermal diffusion of the electroplated Co into the Rh structure. To establish preparation of betavoltaic battery, and Moessbauer source, natural Ni and Co were electroplated on the Rh plate. Both the acid-based buffer (pH 3) and the alkarine-based buffer (pH 10) are used for plating bath. The deposition yield of the alkarine electrolyte is relatively higher than those of the acidic bath. optimum conditions for the homogeneous diffusion is determined at annealing temperatures of 1100 .deg. C for 3h under the high vacuum atmosphere (10{sup -5} hPa). The proposed condition in this study should be applied to prepare 57Co/Rh Moessbauer source at near future.

  3. sup 119 Sn-Moessbauer spectroscopic study of the single phase of Bi(Pb)-Sr-Ca-Cu(Sn)-O

    Energy Technology Data Exchange (ETDEWEB)

    Matsumoto, Y. (Dept. of Electrical Engineering, Fukuoka Univ. (Japan)); Nishida, T. (Dept. of Chemistry, Kyushu Univ., Fukuoka (Japan)); Katada, M. (Dept. of Chemistry, Tokyo Metropolitan Univ. (Japan)); Deshimaru, Y.; Miura, N.; Yamazoe, N. (Dept. of Materials Science and Tech., Graduate School of Engineering Sciences, Kyushu Univ., Fukuoka (Japan))

    1991-12-01

    Tin-doped samples of the high-Tc (2223) phase of Bi-Pb-Sr-Ca-Cu-O superconductor have been prepared by a conventional sintering method. Sintering conditions were carefully selected to obtain the single high-Tc phase. {sup 119}Sn-Moessbauer spectra have been measured in the temperature range from 4.2 to 300 K. The temperature dependence of the recoilless fraction (f) is well understood by the temperature dependence of the normal phonon. (orig.).

  4. Moessbauer study of the composition and corrosion behaviour of electrodeposited and cast brass containing 1-4 m% tin

    Energy Technology Data Exchange (ETDEWEB)

    Vertes, A.; Suba, M.; Varsanyi-Lakatos, M.; Czako-Nagy, I. (Eoetvoes Lorand Tudomanyegyetem, Budapest (Hungary). Fizikai Kemiai es Radiologiai Tanszek); Pchelnikov, A.P.; Losev, V.V. (AN SSSR, Moscow. Inst. Fizicheskoj Khimii)

    1982-09-06

    Moessbauer measurements on electrodeposited and cast brass containing 1-4 m% tin were carried out using conversion electron detector. It was found that the tin formed phases with copper but not with zinc. The identified phases were ..beta.., ..gamma.., epsilon and eta and their ratio depended on the tin concentration and on the preparation process of the brass. The corrosion behaviour of the samples was also studied.

  5. Preparation, crystal structure and optical spectroscopy of the rare earth complexes (RE 3+=Sm, Eu, Gd and Tb) with 2-thiopheneacetate anion

    Science.gov (United States)

    Teotonio, Ercules E. S.; Brito, Hermi F.; Felinto, Maria Cláudia F. C.; Thompson, Larry C.; Young, Victor G.; Malta, Oscar L.

    2005-09-01

    Rare earth complexes with the formulae Sm(TPAC) 3·3H 2O, Eu 2(TPAC) 6·5.25H 2O and RE(TPAC) 3·3.5H 2O (where RE=Gd and Tb), and TPAC=2-thiopheneacetate) have been synthesized and characterized by complexometric titration, elemental analyses, infrared spectroscopy, and X-ray crystallography. Infrared data suggested the presence of both bridging and chelating TPAC anions. The crystal structure of the [Eu 2(TPAC) 6·(H 2O) 3]·2.25H 2O complex in the solid state, determined by X-ray diffraction, revealed that it crystallizes in the orthorhombic crystal system (space group Aba2), with two crystallographically independent Eu 3+ centers (Eu1 and Eu2). These europium centers are held together by one bidentate bridging and two tridentate bridging carboxylate groups. The existence of two Eu 3+ centers was also supported by the emission spectrum. The luminescence properties of the RE-TPAC complexes were investigated by measuring the excitation and emission spectra, and the intramolecular ligand-to-rare earth energy transfer mechanisms were discussed. The emission spectra of the Eu 3+ and Tb 3+ ions displayed only narrow bands arising from 5D 0→ 7F 0 and 5D 0→ 7F 0-4 transitions, respectively, indicating an efficient luminescence sensitization of these ions by the TPAC 'antenna'. On the other hand, the emission spectrum of the Sm 3+-complex displayed a broad band from the phosphorescence of the TPAC ligand which overlapped the 4f 5-intraconfigurational transitions. The theoretical intensity parameters Ωλ ( λ=2 and 4), maximum splitting of the 7F 1 state (Δ E) and the ratio between the 5D 0→ 7F 0 and 5D 0→ 7F 2 transition intensities ( R02) were calculated based on the X-ray crystalline structure for the Eu 3+-complex, and a comparison with experimental data were made. The emission quantum efficiency ( η) of the D5 emitting level of the Eu 3+ ion was also determined.

  6. Absorption spectroscopy of heavy alkaline earth metals Ba and Sr in rare gas matrices—CCSD(T) calculations and atomic site occupancies

    Energy Technology Data Exchange (ETDEWEB)

    Davis, Barry M.; McCaffrey, John G., E-mail: john.mccaffrey@nuim.ie [Department of Chemistry, Maynooth University, National University of Ireland—Maynooth, County Kildare (Ireland)

    2016-01-28

    Isolation of the heavier alkaline earth metals Ba and Sr in the solid rare gases (RGs) Ar, Kr, and Xe is analysed with absorption spectroscopy and interpreted partly with the assistance of ab initio calculations of the diatomic M ⋅ RG ground state interaction potentials. The y{sup 1}P←a{sup 1}S resonance transitions in the visible spectral region are used to compare the isolation conditions of these two metal atom systems and calcium. Complex absorption bands were recorded in all three metal atom systems even after extensive sample annealing. Coupled cluster calculations conducted on the ground states of the nine M ⋅ RG diatomics (M = Ca, Sr, and Ba; RG = Ar, Kr, and Xe) at the coupled cluster single, double, and non-iterative triple level of theory revealed long bond lengths (>5 Å) and shallow bound regions (<130 cm{sup −1}). All of the M ⋅ RG diatomics have bond lengths considerably longer than those of the rare gas dimers, with the consequence that isolation of these metal atoms in a single substitutional site of the solid rare gas is unlikely, with the possible exception of Ca/Xe. The luminescence of metal dimer bands has been recorded for Ba and Sr revealing very different behaviours. Resonance fluorescence with a lifetime of 15 ns is observed for the lowest energy transition of Sr{sub 2} while this transition is quenched in Ba{sub 2}. This behaviour is consistent with the absence of vibrational structure on the dimer absorption band in Ba{sub 2} indicating lifetime broadening arising from efficient relaxation to low-lying molecular states. More extensive 2D excitation-emission data recorded for the complex site structures present on the absorption bands of the atomic Ba and Sr systems will be presented in future publications.

  7. Mossbauer spectroscopy of actinide intermetallics

    Energy Technology Data Exchange (ETDEWEB)

    Kalvius, G.M.; Potzel, W.; Moser, J.; Litterst, F.J.; Asch, L.; Zankert, J.; Potzel, U.; Kratzer, A.; Wunsch, M.; Gal, J.

    1984-09-01

    Due to their wider radial extend the 5f electrons may form bands of different width and hybridization in metallic compounds of the light actinides. This leads to a broad spectrum of magnetic properties ranging from the localized magnetism of the lanthanides to the itinerant electron magnetism often found in transition metal compounds. Also, the influence of the crystalline electric field tends to be more pronounced than in rare earth compounds, but is usually not as dominant as in the 3d series. Magnetic structures and the question of 5f electron delocalization are reviewed with respet to actinide Moessbauer data and new results are presented. In particular the influence of applying external pressure is discussed. 60 references, 24 figures.

  8. Magnetic and Moessbauer studies of Ni substituted Li-Zn ferrite

    Energy Technology Data Exchange (ETDEWEB)

    Soibam, Ibetombi [Department of Physics, Manipur University, Canchipur 795 003 (India)], E-mail: ibetombi_phys@rediffmail.com; Phanjoubam, Sumitra [Department of Physics, Manipur University, Canchipur 795 003 (India); Prakash, C. [Directorate of ER and IPR, DRDO Bhawan, Rajaji Marg, New Delhi 110 011 (India)

    2009-09-15

    Li-Zn ferrites substituted with Ni having the compositional formula Li{sub 0.4-0.5x}Zn{sub 0.2}Ni{sub x}Fe{sub 2.4-0.5x}O{sub 4} where x=0.02{<=}x{<=}0.1 in steps of 0.02 were fabricated by the citrate precursor method. This method has been employed to get nanosized particles and good magnetic properties. The spinel phase structure of the prepared ferrites was confirmed by XRD analysis. The effect of Ni concentration on magnetic properties such as saturation magnetization and Curie temperature were investigated. A good knowledge of these magnetic properties is desirable from application point of view. The values observed are large and both quantities were found to decrease with substitution. The saturation magnetizations were found to vary from 78 to 94 emu/gm while the Curie temperature which limits the operating temperature of the system ranges between 563 and 584 {sup o}C. Moessbauer data were also recorded at room temperature and the hyperfine parameters like isomer shift, quadrupole splitting and internal magnetic field estimated. The results obtained and mechanisms involved are discussed.

  9. X-ray quantum optics with Moessbauer nuclei in thin-film cavities

    Energy Technology Data Exchange (ETDEWEB)

    Heeg, Kilian Peter

    2014-12-09

    In this thesis thin-film cavities with embedded Moessbauer nuclei probed by near-resonant X-ray light are studied from a quantum optical perspective. A theoretical framework is developed and compact expressions for the observables are derived for the linear excitation regime, which is encountered in current experiments. Even advanced cavity layouts can be modeled in excellent agreement with the results of previous experiments and semi-classical approaches. In the absence of magnetic hyperfine splitting, the spectral response of the system is found to be formed by tunable Fano profiles. An experimental implementation of this line shape control allows to extract spectroscopic signatures with high precision and to reconstruct the phase of the nuclear transition in good agreement with the theoretical predictions. The alignment of medium magnetization and polarization control of the X-rays enable to engineer advanced quantum optical level schemes, in which vacuum induced coherence effects are predicted and successfully demonstrated in an experiment. Furthermore, it is shown that group velocity control for x-ray pulses can be achieved in the cavity. A scheme for its observation is proposed and then employed to experimentally confirm sub-luminal X-ray propagation. Finally, non-linear effects, which could become accessible with future light sources, are explored and a non-linear line shape control mechanism is discussed.

  10. Rayleigh scattering of Moessbauer radiation in oriented fibres of hydrated biopolymers

    Energy Technology Data Exchange (ETDEWEB)

    Albanese, G. [Parma Univ. (Italy). Ist. di Fisica; Deriu, A. [Parma Univ. (Italy). Ist. di Fisica; Cavatorta, F. [Parma Univ. (Italy). Ist. di Fisica; Rupprecht, A. [Stockholm Univ. (Sweden). Dept. of Physical, Inorganic and Structural Chemistry

    1995-03-01

    The Rayleigh scattering of Moessbauer radiation (RSMR) has been measured on films of highly oriented hydrated polynucleotides (A-NaDNA) and polysaccharides (Na-hyaluronate). Both DNA and hyaluronate (HA) have helical secondary structures with a similar pitch (28.2 A for A-DNA, and 32.8 A for Na-HA), but they differ in the basic elements which make up the helices and in the extent of water-biopolymer interactions. These differences are responsible for the diverse stiffness of the polymer backbone, and also affect the dynamics of the first hydration layers. For both samples the elastic scattering intensity shows a sharp peak at about 2 A{sup -1} only for samples oriented with Q parallel to the fibre direction. Its position is close to that of the first maximum in the structure factor of bulk water; it is, however, much narrower than in pure H{sub 2}O and it is similar to a crystalline Bragg peak. It can be attributed to an ordered structure of water along the double helices. From the temperature dependence of the elastic intensity under the peak maximum, the mean square displacement of water oxygens in the direction parallel to the helices has been deduced. The thermal diffuse scattering intensity is also peaked at the same Q values of the elastic intensity, indicating the presence of coherent vibrational excitations propagating along the ordered water filaments. (orig.)

  11. Magnetic transitions in La{sub 1x}Y{sub x}Mn{sub 2}Si{sub 2} - Moessbauer effect study

    Energy Technology Data Exchange (ETDEWEB)

    Zhao, X.L.; Campbell, S.J. [Australian Defence Academy, Canberra, ACT (Australia). School of Physics, University College; Cadogan, J.M.; Li, H.S. [The University of New South Wales, Sydney, NSW (Australia). School of Physics

    1996-12-31

    Investigation of ternary rare-earth manganese silicides (RMn{sub 2S}i{sub 2}) with the tetragonal ThCr{sub 2}Si{sub 2} structure (space group I4/mmm) continues to attract a great deal of interest due to the large variety of magnetic behaviours which they exhibit. The set of La{sub 1{sub x}}Y{sub x}Mn{sub 2}Si{sub 2}({sup 57}Fe) samples (x = 0.00, 0.10, 0.15, 0.20, 0.25, 0.30, 0.50 and 1.00) was prepared using conventional argon-arc melting and examined by x-ray diffraction. One of the striking features of our results is that the ordering temperatures of the compounds with low Y concentration (x < 0.3) are significantly higher than previously reported values, while, also at low Y concentrations, a transferred magnetic hyperfine field associated with {sup 57}Fe atoms on the Si sites is found to persist well above Tc. These observations are in general agreement with the new findings of a high temperature antiferromagnetic phase in LaMn{sub 2}Si{sub 2}. Magnetic phase transitions (as indicated by distinct temperature- and concentration- dependent anomalies in the hyperfine magnetic field and quadrupole splitting ), have been determined for the La{sub 1-x}Y{sub x}Mn {sub 2}Si{sub 2}({sup 57}Fe) samples, leading to clarification of the magnetic phase diagram. Around the critical concentration (x{approx}0.2) which separates the predominant antiferromagnetic and ferromagnetic regions, the Moessbauer spectra exhibit broadened lines indicative of a spin glass-like or frustrated magnetic system Truncated abstract. 3 refs.

  12. On the interpretation of {sup 57}Fe Moessbauer spectra from CdTe thin films with substitutions of Fe, In, and Sb

    Energy Technology Data Exchange (ETDEWEB)

    Yee-Madeira, H. [Centro de Investigacion y de Estudios Avanzados, IPN, Mexico City (Mexico). Dept. de Fisica]|[Depto. de Fisica, Esc. Sup. de Fisica y Matematicas (ESFM) del IPN, Edif. 9, U. P. ALM, 07738, Mexico D.F. (Mexico); Reguera, E.; Zelaya-Angel, O.; Sanchez-Sinencio, F. [Centro de Investigacion y de Estudios Avanzados, IPN, Mexico City (Mexico). Dept. de Fisica; Montiel-Sanchez, H. [Depto. de Fisica, Esc. Sup. de Fisica y Matematicas (ESFM) del IPN, Edif. 9, U. P. ALM, 07738, Mexico D.F. (Mexico); Scorzelli, R.B. [Centro Brasileiro de Pesquisas Fisicas, Rua Xavier Sigaud 150, CEP 22290, Urca, Rio de Janeiro (Brazil)

    1999-02-26

    {sup 57}Fe Moessbauer spectra of well characterized CdTe thin films with substitutions of Fe, In and Sb were recorded and interpreted according to the changes in the ionic radii and electronic properties of these substitutions relative to Cd in the CdTe framework. The literature reports of certain correlations among the iron valence, Fe{sup 2+} or Fe{sup 3+}, and the crystallinity of the films are critically discussed and an explanation of their origin is provided. The Moessbauer results also allow direct understanding of the effect of In and Sb substitutions on the properties of the films. (orig.) 22 refs.

  13. Moessbauer Mineralogical Evidence for Aqueous Processes at Gusev Crater and Meridiani Planum

    Science.gov (United States)

    Morris, R. V.; Klingelhoefer, G.

    2004-12-01

    The Moessbauer spectrometers on the MER rovers have measured the relative abundances of iron with respect to both oxidation state and iron-bearing phase at Gusev Crater (Spirit rover) and Meridiani Planum (Opportunity rover). The assemblage of phases indicates aqueous alteration processes at both landing sites. Although the rock and soil of the Gusev Crater plains are dominated by Fe(2+) in olivine-bearing basalt (~Fo60), a Fe(3+)-rich component (nanophase ferric oxide, np-Ox) has significant abundance in surface soils (13-28% of total Fe) and in the surface coatings (rinds) of certain rocks (39%) but not in rock interiors exposed by grinding (5-6%). The mode of occurrence of np-Ox implies that it is the product of oxidative alteration of Fe(2+) silicate and oxide phases in the presence of H2O. The ubiquitous presence of sulfur in soil and in rock coatings, as determined by the MER-A APXS instrument, suggests that the alteration occurred under acid-sulfate conditions, so that both hydrolytic and sulfatic reactions are viable. A possible source for the weathering agents is volcanic emanations rich in H2O and SO2. Generally, rocks in the Columbia Hills are significantly more altered than those in the Gusev plains, with a higher proportion of Fe(3+) oxide phases compared to Fe(2+) silicate phases. This mineralogical dichotomy implies a difference in the timing, rate, duration, and/or mechanism of alteration for basaltic material in the Gusev plains compared to basaltic material in the Columbia Hills. It is possible, for example, that the basaltic material in the Columbia Hills underwent aqueous alteration in a paleoclimate that favored nearly complete alteration and that the basaltic material of the Gusev plains will not achieve the degree of alteration exhibited by the Columbia Hills under current martian surface conditions. Because its structure contains the hydroxide anion, the Moessbauer detection of the hydroxide sulfate jarosite (K,Na)Fe3(SO4)2(OH)6 in outcrops

  14. A Moessbauer effect study of structural ordering in rapidly quenched Fe-Ga alloys

    Energy Technology Data Exchange (ETDEWEB)

    Dunlap, R.A. [Defence R and D Canada-Atlantic, P.O. Box 1012, Dartmouth, Nova Scotia B2Y 3Z7 (Canada) and Department of Physics and Atmospheric Science, Dalhousie University, Halifax, Nova Scotia B3H 3J5 (Canada) and Institute for Research in Materials, Dalhousie University, Halifax, Nova Scotia B3H 3J5 (Canada)]. E-mail: dunlap@fizz.phys.dal.ca; McGraw, J.D. [Department of Physics and Atmospheric Science, Dalhousie University, Halifax, Nova Scotia B3H 3J5 (Canada); Farrell, S.P. [Defence R and D Canada-Atlantic, P.O. Box 1012, Dartmouth, Nova Scotia B2Y 3Z7 (Canada)

    2006-10-15

    Samples of Fe{sub 100-} {sub x} Ga {sub x} (x=8.3, 17.9, 20.5 and 23.3) were prepared by rapid solidification from the melt using a single Cu roller. X-ray diffraction studies of all samples showed them to be single phase with the disordered BCC structure. No evidence of superlattice reflections from D0{sub 3} ordering was observed for any of the samples. Room-temperature {sup 57}Fe Moessbauer effect spectra indicated that all samples were ferromagnetically ordered. Spectra were fit to distributions of hyperfine fields. The x=8.3 sample showed a hyperfine field distribution that was single peaked and indicated a reasonably random distribution of local Fe environments. The x=17.9 and 20.5 samples showed hyperfine field distributions that were bimodal and indicated two distinct local Fe environments. The x=23.3 sample showed three distinct field components. It is suggested that the x=8.3, 17.9 and 20.5 alloys are primarily a disordered BCC phase. The x=8.3 alloy shows a small amount of short-range Ga-Ga pairing, while this short-range pairing is significantly greater in the x=17.9 and 20.5 alloys. The three field components in the x=23.3 alloy correspond well to the two sites associated with the D0{sub 3} phase and a third component corresponding to a remaining L1{sub 2} phase suggesting the presence of at least short-range D0{sub 3} clustering in this alloy.

  15. Moessbauer and magnetic studies of Fe{sub 3-x}Co{sub x}Al

    Energy Technology Data Exchange (ETDEWEB)

    Szymanski, K. E-mail: kszym@alpha.uwb.edu.pl; Biernacka, M.; Dobrzynski, L.; Perzynska, K.; Recko, K.; Satula, D.; Waliszewski, J.; Zaleski, P

    2000-02-01

    Results of Moessbauer, magnetic and X-ray diffraction measurements of Fe{sub 3-x}Co{sub x}Al system are presented. At small concentration of Co the structure is of DO{sub 3}-type. For x=0.5, Fe{sub 3-x}Co{sub x}Al is located on the ternary Fe-Co-Al phase diagram in the region where two crystallographic phases coexists. It is shown how the presence of Co modifies the lattice parameter and the Debye temperature. Dependence of these two parameters on x are discussed and qualitatively explained as due to the lattice shrinking caused by Co-Al pair interaction. The magnetic moment of Co is estimated to be approximately equal to 0.5 {mu}{sub B} at x=0.0 and 1.1 {mu}{sub B} at x=2.0. The magnetic moment of Fe seems constant and equal to approximately 1.9 {mu}{sub B} for x<1 and increases to 2.7 {mu}{sub B} at x=2.0. Dependence of the average isomer shift on x and presence of one component only in the spectrum of FeCo{sub 2}Al indicate that Co locates preferentially at (A,C) sites which could have been expected based on earlier data. It is shown that a simple model of the disorder described by the binomial distribution and linear dependence of the hyperfine field of impurity atoms in the nearest neighbourhood is not adequate for description of the observed hyperfine magnetic field distribution.

  16. Characterization by Moessbauer Spectroscopy and Electron Paramagnetic Resonance of Peruvian Obsidians for Provenance Studies: A Preliminary Study

    Energy Technology Data Exchange (ETDEWEB)

    Bustamante, A.; Montoya, J. [Universidad Nacional Mayor de San Marcos, Facultad de Ciencias Fisicas (Peru); Delgado, M. [QALLTA (Peru); Scorzelli, R. B.; Rossi, A. M. [Centro Brasileiro de Pesquisas Fisicas (Brazil); Poupeau, G. [Institut de Recherche sur les Archeomateriaux, UMR 5060, CNRS/Universite Bordeaux 3, Maison de l' Archeologie, Esplanade des Antilles (France)

    2003-06-15

    The identification of geological sources of obsidians collected in archaeological sites provides important information about circulation routes and sociocultural relationships during prehistoric periods. This paper presents the preliminary results obtained by MS and EPR on geological obsidians from Ayacucho and Arequipa, in Peru and on archaeological obsidian artifacts from Cerrillos, an early Paracas site of the upper Ica valley, south of Lima (Peru).

  17. Moessbauer study of iron-carbide growth and Fischer-Tropsch activity

    Energy Technology Data Exchange (ETDEWEB)

    Rao, K.R.P.M.; Huggins, F.E.; Huffman, G.P. [Univ. of Kentucky, Lexington, (United States)] [and others

    1995-12-31

    There is a need to establish a correlation between the Fischer-Tropsch (FT) activity of an iron-based catalyst and the catalyst phase during FT synthesis. The nature of iron phases formed during activation and FT synthesis is influenced by the nature of the gas and pressure apart from other parameters like temperature, flow rate etc., used for activation. Moessbauer investigations of iron-based catalysts subjected to pretreatment at two different pressures in gas atmospheres containing mixtures of CO, H{sub 2}, and He have been carried out. Studies on UCI 1185-57 (64%Fe{sub 2}O{sub 3}/5%CuO/1%K{sub 2}O/30% Kaolin) catalyst indicate that activation of the catalyst in CO at 12 atms. leads to the formation of 100% magnetite and the magnetite formed gets rapidly converted to at least 90% of {chi}-Fe{sub 5}C{sub 2} during activation. The FT activity was found to be good at 70-80% of (H{sub 2}+CO) conversion. On the other hand, activation. The FT activity was found to be good at 70-80% of (H{sub 2}+CO) conversion. On the other hand, activation of the catalyst in synthesis gas at 12 atms. leads to formation of Fe{sub 3}O{sub 4} and it gets sluggishly converted to {chi}-Fe{sub 5}C{sub 2} and {epsilon}-Fe{sub 2.2}C during activation and both continue to grow slowly during FT synthesis. FT activity is found to be poor. Pretreatment of the catalyst, 100fe/3.6Si/0.71K at a low pressure of 1 atms. in syngas gave rise to the formation of {chi}-Fe{sub 5}C{sub 2} and good FT activity. On the other hand, pretreatment of the catalyst, 100Fe/3.6Si/0.71K at a relatively high pressure of 12 atms. in syngas did not give rise to the formation any carbide and FT activity was poor.

  18. In situ Moessbauer and magnetization studies of Fe-Si nanocrystallization in Fe{sub 73.5}Si{sub 13.5}B{sub 9}Cu{sub 1}Nb{sub 1} X{sub 2}, with X = Nb, Zr, Mo, amorphous alloys

    Energy Technology Data Exchange (ETDEWEB)

    Pena Rodriguez, V.A. [Universidad Nacional Mayor de San Marcos, Facultad de Ciencias Fisicas (Peru); Baggio-Saitovitch, E.M.; Takeuchi, A.Y.; Garcia, F. [Centro Brasileiro de Pesquisas Fisicas (Brazil); Passamani, E.C. [Universidade Federal de Espirito Santo, Vitoria, Departamento de Fisica (Brazil); Borrego, J.M.; Conde, A. [Universidad de Sevilla, Departamento de Fisica de la Materia Condensada (Spain)

    1999-11-15

    The Fe-Si nanosized particles were obtained by controlled partial crystallization of Fe{sub 73.5}Si{sub 13.5}B{sub 9}Cu{sub 1}Nb{sub 1}X{sub 2} (X = Nb, Zr, Mo) amorphous alloys. In situ Moessbauer spectroscopy and magnetization measurements have been used to follow the temperature-dependent magnetization of the amorphous as well as of the nanosized Fe-Si particles. Our results, for the residual amorphous and of nanoparticles phases, show that the temperature dependence of the hyperfine field and magnetization of both residual amorphous and nanocrystalline Fe(Si) phases are different from that of the as-quenched bulk amorphous or crystalline Fe{sub 3}Si alloys. Likewise, from the temperature dependence studies it was possible to determine that the onset temperature of the nanocrystallization process increases in the sequence Mo < Nb < Zr, for the same annealing conditions.

  19. Moessbauer effect and electrical properties studies of SmFe{sub x}Mn{sub 1-x}O{sub 3} (x = 0.7, 0.8 and 0.9)

    Energy Technology Data Exchange (ETDEWEB)

    Bashkirov, Sh.Sh. [Kazan State University, Kazan 420008 (Russian Federation); Parfenov, V.V. [Kazan State University, Kazan 420008 (Russian Federation); Abdel-Latif, I.A. [Reactor Physics Department, Reactor Division, NRC, Atomic Energy Authority, P.O. Box 13759, Cairo (Egypt)]. E-mail: ihab_abdellatif@yahoo.co.uk; Zaripova, L.D. [Kazan State University, Kazan 420008 (Russian Federation)

    2005-01-25

    The cation distributions in the B-site of the orthoferrites SmFe{sub x}Mn{sub 1-x}O{sub 3} (x = 0.7, 0.8, 0.9) were studied by {sup 57}Fe Moessbauer spectroscopy at room temperature. The spectra showed several nonequivalent sites of the iron ions. Five sextets were used in the fitting of the experimentally observed spectra and each one corresponds to different number of the Fe ions in the next nearest neighboring. A nonrandom cation distribution model in such compounds was proposed to interpret the multi-sextets spectra. According to the electric properties measurements, it was noted that the conductivity increases two times with increasing the Mn content but the activation energy decreases from 0.34 eV down to 0.22 eV. The sample with x = 0.7 is an electron semiconductor while the other samples display hole conduction. The magnetoresistance MR of the studied samples value is of 10% and has a negative sign at room temperature while a positive sign is obtained with temperature raising.

  20. Crystal structure, magnetism, {sup 89}Y solid state NMR, and {sup 121}Sb Moessbauer spectroscopic investigations of YIrSb

    Energy Technology Data Exchange (ETDEWEB)

    Benndorf, Christopher [Institut fuer Physikalische Chemie, Universitaet Muenster (Germany); Institut fuer Anorganische und Analytische Chemie, Universitaet Muenster (Germany); Heletta, Lukas; Block, Theresa; Poettgen, Rainer [Institut fuer Anorganische und Analytische Chemie, Universitaet Muenster (Germany); Eckert, Hellmut [Institut fuer Physikalische Chemie, Universitaet Muenster (Germany); Institute of Physics in Sao Carlos, University of Sao Paulo, Sao Carlos (Brazil)

    2017-02-15

    The ternary antimonide YIrSb was synthesized from the binary precursor YIr and elemental antimony by a diffusion controlled solid-state reaction. Single crystals were obtained by a flux technique with elemental bismuth as an inert solvent. The YIrSb structure (TiNiSi type, space group Pnma) was refined from single-crystal X-ray diffractometer data: a = 711.06(9), b = 447.74(5), c = 784.20(8) pm, wR{sub 2} = 0.0455, 535 F{sup 2} values, 20 variables. {sup 89}Y solid state MAS NMR and {sup 121}Sb Moessbauer spectra show single resonance lines in agreement with single-crystal X-ray data. YIrSb is a Pauli paramagnet. (copyright 2017 WILEY-VCH Verlag GmbH and Co. KGaA, Weinheim)

  1. A Moessbauer study of a new intermetallic phase Nd[sub 2](Fe,Ti)[sub 19] and its nitride

    Energy Technology Data Exchange (ETDEWEB)

    Cadogan, J.M. (School of Physics, Univ. of New South Wales, Kensington, NSW (Australia)); Day, R.K. (CSIRO Div. of Applied Physics, Lindfield, NSW (Australia)); Dunlop, J.B. (CSIRO Div. of Applied Physics, Lindfield, NSW (Australia)); Margarian, A. (CSIRO Div. of Applied Physics, Lindfield, NSW (Australia))

    1993-11-12

    In this paper we present [sup 57]Fe Moessbauer spectra of a new ternary intermetallic phase Nd[sub 2](Fe, Ti)[sub 19] and its nitride. Our previous work suggests that the 2-19 phase is related to the hexagonal TbCu[sub 7] structure. The average [sup 57]Fe magnetic hyperfine field of Nd[sub 2](Fe, Ti)[sub 19] at 295 K is 20.8 T which corresponds to an average Fe atomic magnetic moment of 1.33[mu][sub B]. After nitrogenation, the average [sup 57]Fe hyperfine field at 295 K is 29.6 T, which corresponds to an average Fe atomic magnetic moment of 1.90[mu][sub B]. This enhancement in the Fe atomic magnetic moment (at 295 K) is attributed mainly to the N-induced increase in Curie temperature of about 200 K. (orig.)

  2. Moessbauer and XRD study of the Fe{sub 65}Si{sub 35} alloy obtained by mechanical alloying

    Energy Technology Data Exchange (ETDEWEB)

    Velez, G. Y., E-mail: giovelez29@gmail.com [Universidad del Valle, Departamento de Fisica (Colombia); Rodriguez, R. R. [Corporacion Universidad Autonoma de Occidente (Colombia); Melo, C. A.; Perez Alcazar, G. A.; Zamora, Ligia E.; Tabares, J. A. [Universidad del Valle, Departamento de Fisica (Colombia)

    2011-11-15

    A study was made on the alloy Fe{sub 65}Si{sub 35} using x-ray diffraction and Moessbauer spectrometry. The alloy was obtained by mechanical alloying in a high energy planetary mill, with milling times of 15, 30, 50, 75 and 100 h. The results show that in the alloys two structural phases are present, a Fe-Si BCC disordered phase and ferromagnetic, and a Fe-Si SC phase, whose nature is paramagnetic and which decreases with milling time. In the temporal evolution of the milling two stages are differentiated: one between 15 and 75 h of milling, in which silicon atoms diffuse into the bcc matrix of iron and its effect is to reduce the hyperfine magnetic field; the other, after 75 h of milling, where the alloy is consolidated, the effect of the milling is only to increase the disorder of the system, increasing the magnetic order.

  3. Rayleigh scattering of Moessbauer radiation in superionic conductor RbAg/sub 4/I/sub 5/

    Energy Technology Data Exchange (ETDEWEB)

    Ovanesyan, N.S.; Goffman, V.G.; Sokolov, V.B.; Tkachev, V.V. (AN SSSR, Chernogolovka. Otdelenie Inst. Khimicheskoj Fiziki)

    1984-04-01

    The dynamical properties of RbAg/sub 4/I/sub 5/ has been investiaated by Rayleigh scattering of Moessbauer radiation (RSMR) with wave-length lambda = 0.86 A. The character of Ag/sup +/ ion oscillatory motion and diffusion in RbAg/sub 4/I/sub 5/ depending on temperature including the phase transitions region is studied. It is shown that in the superionic crystal RbAg/sub 4/I/sub 5/ the diffusion process is strongly correlated, i.e. a great number of initial and final states at diffusion jumps coincide. The observed broadening can be less than the expected one by value orders. Diffusion correlation can strongly reduce the activation barrier and lead to anomalously high ionic conduction.

  4. Volatile organic sulfur compounds as biomarkers complementary to methane: Infrared absorption spectroscopy of CH 3SH enables insitu measurements on Earth and Mars

    Science.gov (United States)

    Vance, Steve; Christensen, Lance E.; Webster, Christopher R.; Sung, Keeyoon

    2011-02-01

    As universal products of biological processes, volatile organic sulfur compounds such as methyl mercaptan (CH 3SH) may be essential in the search for signs of life on Mars and in exoplanet atmospheres. Methyl mercaptan is implicated in the origin of life at sites of low-temperature hydrothermal activity driven by serpentinization. Serpentinization may occur on Mars, in icy satellite oceans, and in other small wet bodies to a greater extent than on Earth, with important implications for life. We characterized absorption features in pure laboratory sample spectra of CH 3SH using the Carbon Isotope Laser Spectrometer (CILS), an infrared (3.27μm) tunable diode laser spectrometer with capabilities nearly identical to those of the Tunable Laser Spectrometer (TLS) instrument on the Mars Science Laboratory. The molecular species proves detectable by CILS and TLS at the sensitivities approaching the level of parts per trillion with pre-concentration. These measurements demonstrate the possibility for detection of methyl mercaptan, with implications for its possible use as an in situ biosignature for Earth-based and extraterrestrial exploration.

  5. Syntheses, Vibrational Spectroscopy, and Crystal Structure Determination from X-Ray Powder Diffraction Data of Alkaline Earth Dicyanamides M[N(CN)

    Energy Technology Data Exchange (ETDEWEB)

    Juergens, Barbara; Irran, Elisabeth; Schnick, Wolfgang

    2001-03-01

    The alkaline earth dicyanamides Mg[N(CN){sub 2}]{sub 2}, Ca[N(CN){sub 2}]{sub 2}, Sr[N(CN){sub 2}]{sub 2}, and Ba[N(CN){sub 2}]{sub 2} were synthesized by ion exchange using Na[N(CN){sub 2}] and the respective nitrates or bromides as starting materials. The crystal structures were determined from X-ray powder diffractometry: Mg[N(CN){sub 2}]{sub 2}, Pnnm, Z=2, a=617.14(3), b=716.97(3), and c=740.35(5) pm; Ca[N(CN){sub 2}]{sub 2} and Sr[N(CN){sub 2}]{sub 2}, C2/c, Z=4; Ca[N(CN){sub 2}]{sub 2}, a=1244.55(3), b=607.97(1), and c=789.81(1) pm, {beta}=98.864(2){degree}; Sr[N(CN){sub 2}]{sub 2}, a=1279.63(2), b=624.756(8), and c=817.56(1) pm, {beta}=99.787(1){degree}; Ba[N(CN){sub 2}]{sub 2}, Pnma, Z=4, a=1368.68(7), b=429.07(7), and c=1226.26(2) pm. The dicyanamides consist of the respective alkaline earth cations and bent planar [N(CN){sub 2}]{sup -} ions. The structural features were correlated with vibrational spectroscopic data. The thermal behavior was studied by thermoanalytical experiments.

  6. Simulated JWST/NIRISS Spectroscopy of Anticipated TESS Planets and Selected Super-Earths Discovered from K2 and Ground-Based Surveys

    Science.gov (United States)

    Louie, Dana; Albert, Loic; Deming, Drake

    2017-01-01

    The 2018 launch of James Webb Space Telescope (JWST), coupled with the 2017 launch of the Transiting Exoplanet Survey Satellite (TESS), heralds a new era in Exoplanet Science, with TESS projected to detect over one thousand transiting sub-Neptune-sized planets (Ricker et al, 2014), and JWST offering unprecedented spectroscopic capabilities. Sullivan et al (2015) used Monte Carlo simulations to predict the properties of the planets that TESS is likely to detect, and published a catalog of 962 simulated TESS planets. Prior to TESS launch, the re-scoped Kepler K2 mission and ground-based surveys such as MEarth continue to seek nearby Earth-like exoplanets orbiting M-dwarf host stars. The exoplanet community will undoubtedly employ JWST for atmospheric characterization follow-up studies of promising exoplanets, but the targeted planets for these studies must be chosen wisely to maximize JWST science return. The goal of this project is to estimate the capabilities of JWST’s Near InfraRed Imager and Slitless Spectrograph (NIRISS)—operating with the GR700XD grism in Single Object Slitless Spectrography (SOSS) mode—during observations of exoplanets transiting their host stars. We compare results obtained for the simulated TESS planets, confirmed K2-discovered super-Earths, and exoplanets discovered using ground-based surveys. By determining the target planet characteristics that result in the most favorable JWST observing conditions, we can optimize the choice of target planets in future JWST follow-on atmospheric characterization studies.

  7. {sup 1}H and {sup 23}Na MAS NMR spectroscopy of cationic species in CO{sub 2} selective alkaline earth metal porous silicoaluminophosphates prepared via liquid and solid state ion exchange

    Energy Technology Data Exchange (ETDEWEB)

    Arevalo-Hidalgo, Ana G. [Department of Chemical Engineering, University of Puerto Rico-Mayagueez Campus, Mayagueez, PR 00681-9000 (Puerto Rico); Dugar, Sneha; Fu, Riqiang [National High Magnetic Field Laboratory, Florida State University, Tallahassee, FL 32310 (United States); Hernandez-Maldonado, Arturo J., E-mail: arturoj.hernandez@upr.edu [Department of Chemical Engineering, University of Puerto Rico-Mayagueez Campus, Mayagueez, PR 00681-9000 (Puerto Rico)

    2012-07-15

    The location of extraframework cations in Sr{sup 2+} and Ba{sup 2+} ion-exchanged SAPO-34 was estimated by means of {sup 1}H and {sup 23}Na MAS NMR spectroscopy and spectral deconvolution. Incorporation of the alkaline earth metal cations onto the SAPO framework was achieved via liquid state ion exchange, coupled partial detemplation/solid-state ion exchange, and combination of both techniques. MAS NMR revealed that the level of ion exchange was limited by the presence of protons and sodium cations near hexagonal prisms (site SI), which are relatively difficult to exchange with the alkaline earth metal due to steric and charge repulsion criteria. In addition, the presence of ammonium cations in the supercages facilitated the exchange of otherwise tenacious hydrogen as corroborated by unit cell compositional data as well as enhanced CO{sub 2} adsorption at low partial pressures. The extraframework ammonium species were produced from partial detemplation of the structure-directing agent employed for the SAPO-34 synthesis, tetraethylammonium. - Graphical abstract: MAS NMR was used to elucidate the position the cationic species in alkaline earth metal exchanged silicoaluminophosphates. These species played a significant role during the ion exchange process and, therefore, the materials ultimate CO{sub 2} adsorption performance. Highlights: Black-Right-Pointing-Pointer Location of extraframework Sr{sup 2+} or Ba{sup 2+} cations was estimated by means of {sup 1}H and {sup 23}Na MAS NMR. Black-Right-Pointing-Pointer Level of Sr{sup 2+} or Ba{sup 2+} ion exchange was limited by the presence of protons and sodium cations. Black-Right-Pointing-Pointer Presence of ammonium cations in the supercages facilitated the exchange. Black-Right-Pointing-Pointer Sr{sup 2+} and Ba{sup 2+} ion exchanged SAPOs are outstanding CO{sub 2} adsorbents.

  8. High resolution rare-earth elements analyses of natural apatite and its application in geo-sciences: Combined micro-PIXE, quantitative CL spectroscopy and electron spin resonance analyses

    Energy Technology Data Exchange (ETDEWEB)

    Habermann, D. E-mail: haberman@physik.tu-freiberg.de; Goette, T.; Meijer, J.; Stephan, A.; Richter, D.K.; Niklas, J.R

    2000-03-01

    The rare-earth element (REE) distribution in natural apatite is analysed by micro-PIXE, cathodoluminescence (CL) microscopy and spectroscopy and electron spin resonance (ESR) spectroscopy. The micro-PIXE analyses of an apatite crystal from Cerro de Mercado (Mexico) and the summary of 20 analyses of six francolite (conodonts of Triassic age) samples indicate that most of the REEs are enriched in apatite and francolite comparative to average shale standard (NASC). The analyses of fossil francolite revealing the REE-distribution not to be in balance with the REE-distribution of seawater and fish bone debris. Strong inhomogenous lateral REE-distribution in fossil conodont material is shown by CL-mapping and most probably not being a vital effect. Therefore, the resulting REE-signal from fossil francolite is the sum of vital and post-mortem incorporation. The necessary charge compensation for the substitution of divalent Ca by trivalent REE being done by different kind of electron defects and defect ions.

  9. Moessbauer spectrometry and X-ray diffraction studies of the Fe sub 8 sub 7 Zr sub 6 B sub 6 Cu sub 1 nanocrystallization process

    CERN Document Server

    Bibicu, I; Plazaola, F; Apinaniz, E

    2001-01-01

    Fe sub 8 sub 7 Zr sub 6 B sub 6 Cu sub 1 amorphous ribbon were obtained by the melt spinning technique under a controlled atmosphere. One-hour isothermal treatments at different temperatures were performed in a differential thermal analyzer apparatus in an Ar atmosphere. The Conversion Electron Moessbauer Spectrometry (CEMS) and X-ray diffraction measurements of the Fe sub 8 sub 7 Zr sub 6 B sub 6 Cu sub 1 sample in different steps of the nanocrystallization process have been performed. The results have been compared with those obtained by means of Transmission Moessbauer Spectrometry (TMS) technique. The X-ray diffraction patterns and CEMS spectra of the studied samples present systematically higher crystallized fractions than those corresponding to spectra obtained by transmission geometry. As these techniques offer us information about different regions of the sample, the differences among the obtained results have been related to an inhomogenization of the crystallization process into the sample induced b...

  10. Exploring an Earth-sized neighbor: ground-based transmission spectroscopy of GJ1132b, a rocky planet transiting a small nearby M-dwarf

    Science.gov (United States)

    Diamond-Lowe, Hannah; Berta-Thompson, Zachory K.; Charbonneau, David; Irwin, Jonathan; Newton, Elisabeth R.; Dittmann, Jason

    2017-01-01

    The terrestrial planets of the Solar System are rocky worlds that did not accrete envelopes of hydrogen and helium, but instead possess thin secondary atmospheres, or no atmosphere at all. Until recently, most exoplanet atmospheric studies have centered around hot Jupiters, for which high planet-to-star radius ratios and short orbital periods allowed for observable transmission spectra. Now we have the opportunity to probe the atmosphere of a small, rocky exoplanet. GJ1132b has a radius of 1.2 Earth radii and a mass of 1.6 Earth masses, and orbits an M-dwarf 12 parsecs away. Determining the composition of GJ1132b's atmosphere is essential to understanding the nature of atmospheric evolution on terrestrial planets. We observed five transits of GJ1132b using the Magellan Clay telescope with the LDSS3C multi-object spectrograph. We compare the transit depth of GJ1132b in wavelength bins ranging from 0.65 -- 1.04 microns to infer whether or not GJ1132b has maintained its primordial hydrogen-dominated atmosphere. Should we find evidence of a hydrogen-dominated atmosphere, this would imply that a terrestrial planet is able to accrete and retain a low mean-molecular weight atmosphere from the planetary nebula. Coupled with recent UV spectra of the host star, our results can clarify the process of atmospheric escape on terrestrial worlds, with implications for formation histories of M-dwarf planets and the potential for habitability in these systems. If instead GJ1132b possesses a low mean-molecular weight atmosphere, we look to future observations with JWST and the ground-based extremely large telescopes to characterize its atmosphere.This material is based upon work supported by the National Science Foundation Graduate Research Fellowship Program. This work was made possible by a grant from the John Templeton Foundation.

  11. Expanding earth

    Energy Technology Data Exchange (ETDEWEB)

    Carey, S.W.

    1976-01-01

    Arguments in favor of an expanding earth are presented. The author believes that the theory of plate tectonics is a classic error in the history of geology. The case for the expanding earth is organized in the following way: introductory review - face of the earth, development of expanding earth concept, necessity for expansion, the subduction myth, and definitions; some principles - scale of tectonic phenomena, non-uniformitarianism, tectonic profile, paleomagnetism, asymmetry of the earth, rotation of the earth, and modes of crustal extension; regional studies - western North America, Central America, South-East Asia, and the rift oceans; tests and cause of expansion. 824 references, 197 figures, 11 tables. (RWR)

  12. VUV spectroscopy of nominally pure and rare-earth ions doped LiCaAIF6 single crystals as promising materials for 157 nm photolithography

    Science.gov (United States)

    Cefalas, Alkiviadis C.; Sarantopoulou, Evangelia; Kollia, Z.; Abdulsabirov, R. Y.; Korableva, S. L.; Naumov, A. K.; Semashko, V. V.; Kobe, S.; McGuiness, P. J.

    2002-07-01

    Recently it was found that birefringence is induced in CaF2 crystals when they are illuminated with laser light at 157 nm. Taking into consideration that CaF2 is the only optical material used in 157 nm photolithography today, the possibility to use new wide band gap fluoride crystals as optical elements for 157 nm photolithography, even those of non-cubic symmetry, should be considered. Additionally fluoride dielectric crystals with wide band gaps doped with trivalent rare-earth (RE) ions can be used as passive or active optical elements int eh VUV. For doped crystals, applications depend on the structure of the energy level pattern of the 4fn-15d electronic configuration and RE ion concentration. In this work we are exploiting the use of wide band gap fluoride dielectric crystals doped with RE ions. The laser induced fluorescence spectrum at 157 nm, and the absorption spectra of the LiCaAlF6 crystals, pure and doped with RE ions, were investigated in the VUV region of the spectrum. A new m4tehod for monitoring RE concentration in wide band gap fluoride crystals, that is based on vibrating sample magnetometer measurement is presented as well.

  13. X-Ray Absorption Spectroscopy Studies of the Atomic Structure of Zirconium-Doped Lithium Silicate Glasses and Glass-Ceramics, Zirconium-Doped Lithium Borate Glasses, and Vitreous Rare-Earth Phosphates

    Science.gov (United States)

    Yoo, Changhyeon

    In the first part of this work, the atomic-scale structure around rare-earth (RE = Pr, Nd, Eu, Dy, and Er) cations (RE3+) in rare-earth sodium ultraphosphate (REUP) glasses were investigated using RE LIII -edge (RE = Nd, Er, Dy, and Eu) and K-edge (RE = Pr and Dy) Extended X-ray Absorption Fine Structure (EXAFS) spectroscopy. (RE2O 3)x(Na2O)y(P2O5) 1-x-y glasses in the compositional range 0 ≤ x ≤ 0.14 and 0.3 ≤ x + y ≤ 0.4 were studied. For the nearest oxygen shell, the RE-oxygen (RE-O) coordination number decreases from 10.8 to 6.5 with increasing RE content for Pr-, Nd-, Dy-, and Er-doped sodium ultraphosphate glasses. For Eu-doped samples, the Eu-O coordination number was between 7.5 and 8.8. Also, the RE-O mean distance ranges were between 2.43-2.45 A, 2.40-2.43 A, 2.36-2.38 A, 2.30-2.35 A, and 2.28-2.30 A for Pr-, Nd-, Eu-, Dy-, and Er-doped samples, respectively. In the second part, a series of Zr-doped (3-10 mol%) lithium silicate (ZRLS) glass-ceramics and their parent glasses and a series of Zr-doped (2-6 mol% ZrO2) lithium borate (ZRLB) glasses were investigated using Zr K-edge EXAFS and X-ray Absorption Near Edge Structure (XANES) spectroscopy. Immediate coordination environments of all ZRLS glasses are remarkably similar for different compositions. For the nearest oxygen shell, the Zr-O coordination number ranges were between 6.1 and 6.3 for nucleated and crystallized samples, respectively. Also, the Zr-O mean distance remains similar around 2.10 A. For these glasses, the composition dependence of structural parameters was small. Small changes in the coordination environment were observed for ZRLS glass-ceramics after thermal treatments. In contrast, Zr coordination environment in ZRLB glasses appear to depend appreciably on the Zr concentration. For the nearest oxygen shell, the Zr-O coordination number increased from 6.1 to 6.8 and the Zr-O distance decreased from 2.18 A to 2.14 A with decreasing ZrO2 content.

  14. {sup 57}Fe Moessbauer probe of spin crossover thin films on a bio-membrane

    Energy Technology Data Exchange (ETDEWEB)

    Naik, Anil D.; Garcia, Yann, E-mail: yann.garcia@uclouvain.be [Universite Catholique de Louvain, Institute of Condensed Matter and Nanosciences (Belgium)

    2012-03-15

    An illustrious complex [Fe(ptz){sub 6}](BF{sub 4}){sub 2} (ptz = 1-propyl-tetrazole) (1) which was produced in the form of submicron crystals and thin film on Allium cepa membrane was probed by {sup 57}Fe Mossbauer spectroscopy in order to follow its intrinsic spin crossover. In addition to a weak signal that corresponds to neat SCO compound significant amount of other iron compounds are found that could have morphed from 1 due to specific host-guest interaction on the lipid-bilayer of bio-membrane. Further complimentary information about biogenic role of membrane, was obtained from variable temperature Mossbauer spectroscopy on a {approx}5% enriched [{sup 57}Fe(H{sub 2}O){sub 6}](BF{sub 4}){sub 2} salt on this membrane.

  15. Dispersion amplitudes in the Moessbauer lineshape of /sup 237/Np, /sup 182/W, and /sup 195/Pt

    Energy Technology Data Exchange (ETDEWEB)

    Potzel, W. (Technische Universitaet Muenchen, Garching, Ger.); Wagner, F.E.; Kalvius, G.M.; Asch, L.; Spirlet, J.C.; Mueller, W.

    1977-01-01

    Measurements of the dispersion amplitude for the Moessbauer resonances in /sup 237/Np (60 keV), /sup 182/W (100 keV) and /sup 195/Pt (99 keV) are reported. For the E1 transition in /sup 237/Np a value of xi = -(3.4 + 0.2) x 10/sup -2/ was found. Theoretical estimates of xi for this case are of limited accuracy and the comparison with experimental data is inaccurate because of the considerable line broadening. Computer simulations show the influence of xi on /sup 237/Np hyperfine spectra. For the E2 transition in /sup 182/W the dependence of the effective value of xi on absorber thickness was studied. Extrapolations to zero thickness yield xi = -(1.0 +- 0.1) x 10/sup -2/ in good agreement with theoretical calculations. For /sup 195/Pt we found xi = -(1.1 +- 0.3) x 10/sup -2/ for the dispersion amplitude at zero absorber thickness. This is the first pure M1 transition for which a dispersion term has been observed. For all three resonances the dispersion is large enough to affect the determination of isomer shifts.

  16. Moessbauer analysis of high-energy mechanical-milled sand fraction of a magnetic soil developing on basalt

    Energy Technology Data Exchange (ETDEWEB)

    Borges, Jose Flavio Marcelino; Hneda, Marlon Luiz; Brinatti, Andre Mauricio [State University of Ponta Grossa, Department of Physics (Brazil); Cunha, Joao Batista Marimon da [Federal University of Rio Grande do Sul, Institute of Physics (Brazil); Rosa, Jadir Aparecido [Polo Regional de Ponta Grossa, Agronomy Institute of Parana (Brazil); Fabris, Jose Domingos, E-mail: jdfabris@ufmg.br [Federal University of Jequitinhonha and Mucuri Valleys (UFVJM) (Brazil)

    2011-11-15

    A sample of the coarse sand fraction from the soil material of the A-horizon (0-0.2 m from the soil surface) of a dusky red magnetic Oxisol was submitted to high-energy mechanical milling for different times. This assay aimed mainly at (a) monitoring the individualization of strongly aggregated mineral particles, and (b) measuring the effect of the milling pressure on the mineralogy changes of the material. These data are also intended to experimentally subside any physical model describing the mechanical behavior of the superficial soil layer that is subjected to intensive machine management, in agriculture fields. Powder X-ray data reveal that some mineralogical phases, notably gibbsite, disappear soon after the first few hours milling. The 298 K-transmission Moessbauer spectrum for the non-milled sand sample shows a qualitatively typical pattern for the sand fraction of basalt derived soils, with magnetically ordered sextets, assignable mainly to hematite and maghemite, and an intense central (super)paramagnetic Fe{sup 3 + } doublet. For the milled samples, spectra revealed progressive spectral reduction of the magnetic hyperfine structure, with concomitant increase of relative subspectral areas due to (super)paramagnetic phases, as the milling time increased. This result is consistent with the reduction of measured saturation magnetization, from 4.96(8) J T{sup - 1} kg{sup - 1}, for the non-milled sample, to 3.26(7) J T{sup - 1} kg{sup - 1}, for the sample milled for 8 hours.

  17. Rayleigh Scattering of Moessbauer Radiation (RSMR) data, hydration effects and glass-like dynamical model of biopolymers

    Energy Technology Data Exchange (ETDEWEB)

    Gol' danskii, V.I.; Krupyanskii, Yu.F.; Fleurov, V.N.

    1986-06-01

    Specific features of the Rayleigh Scattering of Moessbauer Radiation (RSMR) technique in the study of biological systems are described. Experimental data show that the temperature and hydration degree are the principal parameters which influence intramolecular mobility in biopolymers. Data on temperature dependencies of elastic fraction, f, and spectrum line-shape do not fit neither Debye or Einstein models of solids nor the free diffusion in liquids and demand for their explanation a multimode approximation (i.e. a wide spectrum of correlation times, at T=293 K from 10/sup -6/s to 10/sup -12/-10/sup -13/s). On the basis of RSMR, low temperature specific heat and X-ray dynamic analysis data and from the general conditions that information macromolecule must be in a non-equilibrium state (an independent confirmation of this fact comes from the kinetic model of protein folding) a glass-like dynamical model of biopolymers is formulated. A possible interpretation of RSMR data shows that fluctuatively prepared tunneling between quasiequilibrium positions (QEP) can prevail activated transitions up to a room temperature.

  18. New transition metal-rich rare-earth palladium/platinum aluminides with RET{sub 5}Al{sub 2} composition. Structure, magnetism and {sup 27}Al NMR spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Benndorf, Christopher [Muenster Univ. (Germany). Inst. fuer Anorganische und Analytische Chemie; Muenster Univ. (Germany). Inst. fuer Physikalische Chemie; Stegemann, Frank; Janka, Oliver [Muenster Univ. (Germany). Inst. fuer Anorganische und Analytische Chemie; Eckert, Hellmut [Muenster Univ. (Germany). Inst. fuer Physikalische Chemie

    2015-06-01

    REPd{sub 5}Al{sub 2} compounds with RE = Ce-Gd as well as Y and Lu have been previously synthesized. Although some compounds with the small lanthanides also exist, the compounds with intermediate-sized rare-earth elements (RE = Tb-Yb) had not been prepared. We report on the missing members of the REPd{sub 5}Al{sub 2} (RE = Tb-Yb) series as well as on the new REPt{sub 5}Al{sub 2} (RE = Y, Gd-Tm, Lu) series, which we have synthesized and structurally as well as magnetically characterized. All members crystallize isostructurally in the ZrNi{sub 2}Al{sub 5} type with an anti-arrangement of the T = Pd/Pt and Al atoms. YPd{sub 5}Al{sub 2} and LuPd{sub 5}Al{sub 2}, as well as the respective platinum homologs, YPt{sub 5}Al{sub 2} and LuPt{sub 5}Al{sub 2}, have been characterized also by {sup 27}Al magic-angle spinning nuclear magnetic resonance spectroscopy. Consistent with the XRD analysis, the spectra indicate the existence of only one distinct Al site in the structure.

  19. Earth\\'s Mass Variability

    CERN Document Server

    Mawad, Ramy

    2014-01-01

    The perturbation of the Earth caused by variability of mass of Earth as additional reason with gravity of celestial bodies and shape of the Earth. The Earth eating and collecting matters from space and loss or eject matters to space through its flying in the space around the Sun. The source of the rising in the global sea level is not closed in global warming and icebergs, but the outer space is the additional important source for this rising. The Earth eats waters from space in unknown mechanism. The mass of the Earth become greater in November i.e. before transit apoapsis two months, and become latter in February i.e. after transit apoapsis to two months.

  20. Moessbauer and magnetic studies of the system Li{sub 0.35+0.5t} Zn{sub 03}Ti{sub t}Fe{sub 2.35-1.5t}O{sub 4}

    Energy Technology Data Exchange (ETDEWEB)

    Phanjoubam, Sumitra, E-mail: sumitra4@rediffmail.com [Manipur University, Department of Physics (India); Prakash, Chandra [DRDO Bhawan, Directorate of ER and IPR (India)

    2009-01-15

    Moessbauer and magnetic investigations were carried out on a series of Li-Zn-Ti ferrites with compositional formula Li{sub 035+0.5t} Zn{sub 03}Ti{sub t}Fe{sub 2.35-1.5t}O{sub 4}. Moessbauer spectra were taken at room temperature and analysed to yield information on hyperfine properties like isomer shift, quadrupole splitting and nuclear magnetic fields. Magnetic properties like Curie temperature and saturation magnetization have also been studied. The magnetic properties were observed to fall with increased values of 't'. The results obtained and the mechanisms involved are discussed.

  1. A {sup 119}Sn Moessbauer Study of Tin(IV) Complexes of 2- and 4-Benzoylpyridine Thiosemicarbazone and 4-Benzoylpyridine Semicarbazone

    Energy Technology Data Exchange (ETDEWEB)

    Perez-Rebolledo, Anayive [Universidade Federal de Minas Gerais, Departamento de Quimica (Brazil); Ardisson, Jose D., E-mail: jdr@cdtn.br [Centro de Desenvolvimento da Tecnologia Nuclear, Laboratorio de Fisica Aplicada (LFA/CDTN) (Brazil); Lima, Geraldo M. de [Universidade Federal de Minas Gerais, Departamento de Quimica (Brazil); Macedo, Waldemar A. A. [Centro de Desenvolvimento da Tecnologia Nuclear, Laboratorio de Fisica Aplicada (LFA/CDTN) (Brazil); Beraldo, Heloisa, E-mail: hberaldo@ufmg.br [Universidade Federal de Minas Gerais, Departamento de Quimica (Brazil)

    2005-06-15

    A {sup 119}Sn Moessbauer study was carried out of tin(IV) complexes with 2-benzoylpyridine thiosemicarbazone (H2Bz4DH) and its N(4)-methyl (H2Bz4M) and N(4)-phenyl (H2Bz4Ph) derivatives: [Sn(2Bz4DH)Cl{sub 3}] (1), [Sn(2Bz4DH)PhCl{sub 2}] (2), [Sn(2Bz4M)Cl{sub 3}] (3), [H{sub 2}2Bz4M]{sub 2}[Ph{sub 2}SnCl{sub 4}] (4), [Sn(2Bz4Ph)PhCl{sub 2}] (5), [Sn(2Bz4Ph)Ph{sub 2}Cl] (6), in which H2Bz4R stands for the neutral ligand and 2Bz4R stands for the anionic thiosemicarbazone. In addition, {sup 119}Sn Moessbauer studies of the tin(IV) complexes [Sn(H4Bz4DH){sub 2}Cl{sub 4}H{sub 2}O] (7), [Sn(H4BzPS){sub 2}Cl{sub 4}H{sub 2}O] (8) with 4-benzoylpyridine thiosemicarbazone (H4Bz4DH) and the correspondent semicarbazone (H4BzPS) were performed. The isomer shifts decrease upon coordination due to the variation in the percentage of s character as tin changes from approximately sp{sup 3} hybridization in the tin salts to sp{sup 3}d{sup 2} in the octahedral or sp{sup 3}d{sup 3} in the heptahedral complexes. The Moessbauer parameters of compound (4) showed the existence of two tin(IV) sites, which have been attributed to the presence of the cis and trans isomers.

  2. {sup 57}Fe Moessbauer effect in R{sub 2}Fe{sub 13.6}Si{sub 3.4} (R=U, Lu)

    Energy Technology Data Exchange (ETDEWEB)

    Andreev, A.V. [Institute of Physics, Academy of Sciences, Na Slovance 2, 18221 Prague (Czech Republic)]. E-mail: andreev@mag.mff.cuni.cz; Niznansky, D. [Department of Inorganic Chemistry, Faculty of Natural Sciences, Charles University, Albertov 6, 12843 Prague (Czech Republic); Joint Laboratory of Moessbauer Spectrometry, Faculty of Mathematics and Physics, Charles University, V Holesovickach 2, Prague (Czech Republic); Homma, Y. [Institute for Materials Research, Tohoku University, Katahira 2-1-1, Sendai 980-8578 (Japan); Onodera, H. [Institute for Materials Research, Tohoku University, Katahira 2-1-1, Sendai 980-8578 (Japan); Shiokawa, Y. [Institute for Materials Research, Tohoku University, Katahira 2-1-1, Sendai 980-8578 (Japan); Satoh, I. [Institute for Materials Research, Tohoku University, Katahira 2-1-1, Sendai 980-8578 (Japan)

    2005-12-01

    From a comparative analysis of {sup 57}Fe Moessbauer spectra of U{sub 2}Fe{sub 13.6}Si{sub 3.4} and Lu{sub 2}Fe{sub 13.6}Si{sub 3.4}, the contributions from the Fe and U sublattices to the total magnetic moment of U{sub 2}Fe{sub 13.6}Si{sub 3.4} are estimated to be M {sub Fe}=1.33{mu} {sub B} and M {sub U}=2.6{mu} {sub B}.

  3. Earth materials and earth dynamics

    Energy Technology Data Exchange (ETDEWEB)

    Bennett, K; Shankland, T. [and others

    2000-11-01

    In the project ''Earth Materials and Earth Dynamics'' we linked fundamental and exploratory, experimental, theoretical, and computational research programs to shed light on the current and past states of the dynamic Earth. Our objective was to combine different geological, geochemical, geophysical, and materials science analyses with numerical techniques to illuminate active processes in the Earth. These processes include fluid-rock interactions that form and modify the lithosphere, non-linear wave attenuations in rocks that drive plate tectonics and perturb the earth's surface, dynamic recrystallization of olivine that deforms the upper mantle, development of texture in high-pressure olivine polymorphs that create anisotropic velocity regions in the convecting upper mantle and transition zone, and the intense chemical reactions between the mantle and core. We measured physical properties such as texture and nonlinear elasticity, equation of states at simultaneous pressures and temperatures, magnetic spins and bonding, chemical permeability, and thermal-chemical feedback to better characterize earth materials. We artificially generated seismic waves, numerically modeled fluid flow and transport in rock systems and modified polycrystal plasticity theory to interpret measured physical properties and integrate them into our understanding of the Earth. This is the final report of a three-year, Laboratory-Directed Research and Development (LDRD) project at the Los Alamos National Laboratory (LANL).

  4. Synthesis of Iron-Nitride Phases by Reactive Sputtering: Magnetic and Moessbauer Characterization.

    Science.gov (United States)

    Lo, Cary Chia-Chiung

    This dissertation is concerned with the synthesis of discrete Fe-N phases by the reactive rf-sputtering technique, and their characterization by x-ray diffraction, Mossbauer spectroscopy, magnetic susceptibility and magnetization measurements, and SEM (scanning electron microscopy) to elucidate the growth, the structure, and the magnetic properties of the Fe-N system. Since discrete Fe-N phases are difficult to synthesize by conventional chemical methods as was tried by several researchers, resource was taken to prepare these phases by rf-sputtering, which is a relatively new and attractive technique. Single Fe-N phases (e.g., Fe(,4)N, Fe(,3)N, Fe(,2)N, etc.) were obtained by a careful control of various sputtering conditions, such as the total gas pressure (Ar + N(,2)), partial pressure of N(,2) (p(,N(,2))), substrate temperature, and the applied power. A detailed Mossbauer study of the Fe-N system was carried out as a function of temperature. The low -temperature (300-80 K) spectra of Fe(,3)N and Fe(,4)N showed a superparamagnetic behavior. The blocking temperature (T(,B)) for Fe(,4)N was found to be (TURN)80 K, whereas the T(,B) for Fe(,3)N appeared to be well below 80 K. The high-temperature (300-553 K) spectra were recorded in order to investigate the chemical stability of the nitride films and obtain the temperature at which the magnetic ordering disappeared. It was found that the Curie temperatures of Fe(,3)N and Fe(,4)N were lower than those of the bulk phases, arising from the canted spins at the surface of the film accompanied by thermal fluctuations. Furthermore, on the basis of the Mossbauer parameters, such as the isomer shift, quadrupole splitting and hyperfine field, as well as the magnetic moment per Fe atom, a coherent electronic structure for Fe(,4)N has been proposed. The microstructure of the Fe-N system was investigated by using SEM. These films showed a micro-columnar structure with the columns perpendicular to the plane of the film in most

  5. Snowball Earth

    OpenAIRE

    2016-01-01

    In the ongoing quest to better understand where life may exist elsewhere in the Universe, important lessons may be gained from our own planet. In particular, much can be learned from planetary glaciation events that Earth suffered ∼600 million years ago, so-called `Snowball Earth' episodes. I begin with an overview of how the climate works. This helps to explain how the ice-albedo feedback effect can destabilise a planet's climate. The process relies on lower temperatures causing more ice to ...

  6. Digital Earth - A sustainable Earth

    Science.gov (United States)

    Mahavir

    2014-02-01

    All life, particularly human, cannot be sustainable, unless complimented with shelter, poverty reduction, provision of basic infrastructure and services, equal opportunities and social justice. Yet, in the context of cities, it is believed that they can accommodate more and more people, endlessly, regardless to their carrying capacity and increasing ecological footprint. The 'inclusion', for bringing more and more people in the purview of development is often limited to social and economic inclusion rather than spatial and ecological inclusion. Economic investment decisions are also not always supported with spatial planning decisions. Most planning for a sustainable Earth, be at a level of rural settlement, city, region, national or Global, fail on the capacity and capability fronts. In India, for example, out of some 8,000 towns and cities, Master Plans exist for only about 1,800. A chapter on sustainability or environment is neither statutorily compulsory nor a norm for these Master Plans. Geospatial technologies including Remote Sensing, GIS, Indian National Spatial Data Infrastructure (NSDI), Indian National Urban Information Systems (NUIS), Indian Environmental Information System (ENVIS), and Indian National GIS (NGIS), etc. have potential to map, analyse, visualize and take sustainable developmental decisions based on participatory social, economic and social inclusion. Sustainable Earth, at all scales, is a logical and natural outcome of a digitally mapped, conceived and planned Earth. Digital Earth, in fact, itself offers a platform to dovetail the ecological, social and economic considerations in transforming it into a sustainable Earth.

  7. Moessbauer and X-ray diffraction study of Co{sup 2+}-Si{sup 4+} substituted M-type barium hexaferrite BaFe{sub 12-2x}So{sub x}Si{sub x}O{sub 19{+-}{gamma}}

    Energy Technology Data Exchange (ETDEWEB)

    Solovyova, E.D., E-mail: solovyovak@mail.ru [V.I. Vernadskii Institute of General and Inorganic Chemistry, 32/34 Prospect Palladina, Kyiv-142 03680 (Ukraine); Pashkova, E.V., E-mail: pashelena@ukr.net [V.I. Vernadskii Institute of General and Inorganic Chemistry, 32/34 Prospect Palladina, Kyiv-142 03680 (Ukraine); Ivanitski, V.P. [Institute of Geochemistry, Mineralogy and Ore Formation, 34 Prospect Palladina, Kyiv-164 03680 (Ukraine); V' yunov, O.I., E-mail: vyunov@ionc.kiev.ua [V.I. Vernadskii Institute of General and Inorganic Chemistry, 32/34 Prospect Palladina, Kyiv-142 03680 (Ukraine); Belous, A.G., E-mail: belous@ionc.kiev.ua [V.I. Vernadskii Institute of General and Inorganic Chemistry, 32/34 Prospect Palladina, Kyiv-142 03680 (Ukraine)

    2013-03-15

    Using X-ray powder diffractions, Moessbauer spectroscopy, and magnetic measurements, the effect of dopants (Co{sup 2+}+Si{sup 4+}) on the fine structure and magnetic properties of M-type barium hexaferrite prepared by hydroxide and carbonate precipitations has been studied. It has been shown that the magnetic properties of M-type barium hexaferrite can be controlled by heterovalent substitution 2Fe{sup 3+}{yields}So{sup 2+}+Si{sup 4+}. - Highlights: Black-Right-Pointing-Pointer In the range x=0-0.3, homogeneous solid solutions BaFe{sub 12-2x}Co{sub x}Si{sub x}O{sub 19{+-}{gamma}} are formed. Black-Right-Pointing-Pointer Only Fe{sup 3+}ions in the high-spin state present in the homogeneous region. Black-Right-Pointing-Pointer So{sup 2+}, Si{sup 4+} ions prefer to occupy crystallographic positions 12k, 4f{sub 1} respectively. Black-Right-Pointing-Pointer Substitution 2Fe{sup 3+}{yields}So{sup 2+}+Si{sup 4+} decreases particle size and coercivity.

  8. Moessbauer effect and X-ray distribution function analysis in complex Na{sub 2}O-CaO-ZnO-Fe{sub 2}O{sub 3}-Al{sub 2}O{sub 3}-SiO{sub 2} glasses and glass-ceramics

    Energy Technology Data Exchange (ETDEWEB)

    Romero, M.; Rincon, J.M.; Musik, S.; Kozhukharov, V.

    1999-05-01

    Moessbauer spectroscopy at room temperature was carried out to determine the state of iron ions in complex glasses and glass-ceramics in the SiO{sub 2}-CaO-ZnO-Na{sub 2}O-Fe{sub 2}O{sub 3}-Al{sub 2}O{sub 3} system. Isomer shift values of the glasses suggest that Fe{sup 3+} and Fe{sup 2+} are in tetrahedral and octahedral coordination, respectively. The spectrum of the glass-ceramic shows that about 60 wt% total iron is in the magnetite phase. The Fe{sup +3}/Fe{sup +2} ratio varies with the total iron oxide content of the glasses, indicating that the vitreous network is more distorted when the iron content is greater. X-ray diffraction measurements were carried out to obtain the radial distribution function (RDF). The interatomic distances for Si-Si and Si-O have been determined. The complex composition of these glasses does not allow the estimation of Al-O and Fe-O distances.

  9. Magnetic nanoparticles based on iron coated carbon produced from the reaction of Fe{sub 2}O{sub 3} with CH{sub 4}: a Moessbauer study

    Energy Technology Data Exchange (ETDEWEB)

    Tristao, Juliana C.; Silva, Aline A. [Universidade Federal de Minas Gerais, Departamento de Quimica-ICEx (Brazil); Ardisson, Jose D. [Centro de Desenvolvimento de Tecnologia Nuclear, CDTN, Laboratorio de Fisica Aplicada (Brazil); Lago, Rochel M., E-mail: rochel@ufmg.br [Universidade Federal de Minas Gerais, Departamento de Quimica-ICEx (Brazil)

    2010-01-15

    In this work, it was investigated the production of magnetic nanoparticles encapsulated with carbon by the reaction of hematite and methane by Temperature Programmed Reaction up to 950 deg. C. XRD and Moessbauer analyses showed that the materials prepared at 600 deg. C and 700 deg. C are mainly composed of magnetite and small amounts of hematite {alpha} -Fe{sub 2}O{sub 3} with particle size of 30-40 nm. At higher temperatures, the spectra also display two central doublets corresponding to wuestite phase (Fe{sub 1-x}O). The materials were also characterized by magnetization measurements, BET surface area, thermal analysis (TG) and SEM. These materials can be prepared by a simple and low cost process and show great potential to be used as adsorbents and catalyst support.

  10. Vibrational spectroscopy

    Science.gov (United States)

    Umesh P. Agarwal; Rajai Atalla

    2010-01-01

    Vibrational spectroscopy is an important tool in modern chemistry. In the past two decades, thanks to significant improvements in instrumentation and the development of new interpretive tools, it has become increasingly important for studies of lignin. This chapter presents the three important instrumental methods-Raman spectroscopy, infrared (IR) spectroscopy, and...

  11. Explicit expression for the intensity tensor for 3/2-1/2 transitions and solution of the ambiguity problem in Moessbauer spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Szymanski, K. [Institute of Experimental Physics, University of Bialystok, Lipowa 41, 15-424 Bialystok (Poland)

    2000-08-21

    Analytical expressions for the intensity tensor in the case of 3/2-1/2 nuclear transitions are obtained and the properties of the trace, symmetric and antisymmetric parts of the intensity tensor for a single transition are discussed. It is shown that in the principal axis system of the symmetric part of the intensity tensor the angular dependence of absorption of the circularly polarized resonant radiation depends essentially on only one parameter - the maximal degree of circular polarization. The latter parameter is directly connected with the antisymmetric part of the intensity tensor. It is shown that the so-called ambiguity problem, including the sign of the hyperfine magnetic field, can be solved by measuring the antisymmetric part using circularly polarized radiation. Some values typical in circular polarimetry can be measured in a standard experiment and vice versa. Explicit expressions for the line intensities of the powdered absorber are given in the general case of mixed transitions. The symmetry of the shape of the spectra with different signs of the electric field is explained. An experiment is proposed in which all parameters of the I=3/2 spin Hamiltonian can be unambiguously determined. (author)

  12. Terahertz spectroscopy

    DEFF Research Database (Denmark)

    Jepsen, Peter Uhd

    2009-01-01

    In this presentation I will review methods for spectroscopy in the THz range, with special emphasis on the practical implementation of the technique known ad THz time-domain spectroscopy (THz-TDS). THz-TDS has revived the old field of far-infrared spectroscopy, and enabled a wealth of new...... activities that promise commercial potential for spectroscopic applications in the THz range. This will be illustrated with examples of spectroscopy of liquids inside their bottles as well as sensitive, quantitative spectroscopy in waveguides....

  13. Sulfur Earth

    Science.gov (United States)

    de Jong, B. H.

    2007-12-01

    Variations in surface tension affect the buoyancy of objects floating in a liquid. Thus an object floating in water will sink deeper in the presence of dishwater fluid. This is a very minor but measurable effect. It causes for instance ducks to drown in aqueous solutions with added surfactant. The surface tension of liquid iron is very strongly affected by the presence of sulfur which acts as a surfactant in this system varying between 1.9 and 0.4 N/m at 10 mass percent Sulfur (Lee & Morita (2002), This last value is inferred to be the maximum value for Sulfur inferred to be present in the liquid outer core. Venting of Sulfur from the liquid core manifests itself on the Earth surface by the 105 to 106 ton of sulfur vented into the atmosphere annually (Wedepohl, 1984). Inspection of surface Sulfur emission indicates that venting is non-homogeneously distributed over the Earth's surface. The implication of such large variation in surface tension in the liquid outer core are that at locally low Sulfur concentration, the liquid outer core does not wet the predominantly MgSiO3 matrix with which it is in contact. However at a local high in Sulfur, the liquid outer core wets this matrix which in the fluid state has a surface tension of 0.4 N/m (Bansal & Doremus, 1986), couples with it, and causes it to sink. This differential and diapiric movement is transmitted through the essentially brittle mantle (1024 Pa.s, Lambeck & Johnson, 1998; the maximum value for ice being about 1030 Pa.s at 0 K, in all likely hood representing an upper bound of viscosity for all materials) and manifests itself on the surface by the roughly 20 km differentiation, about 0.1 % of the total mantle thickness, between topographical heights and lows with concomitant lateral movement in the crust and upper mantle resulting in thin skin tectonics. The brittle nature of the medium though which this movement is transmitted suggests that the extremes in topography of the D" layer are similar in range to

  14. Spectroscopy from Space

    Science.gov (United States)

    Clark, R. N.; Swayze, G. A.; Carlson, R.; Grundy, W.; Noll, K.

    2014-01-01

    This chapter reviews detection of materials on solid and liquid (lakes and ocean) surfaces in the solar system using ultraviolet to infrared spectroscopy from space, or near space (high altitude aircraft on the Earth), or in the case of remote objects, earth-based and earth-orbiting telescopes. Point spectrometers and imaging spectrometers have been probing the surfaces of our solar system for decades. Spacecraft carrying imaging spectrometers are currently in orbit around Mercury, Venus, Earth, Mars, and Saturn, and systems have recently visited Jupiter, comets, asteroids, and one spectrometer-carrying spacecraft is on its way to Pluto. Together these systems are providing a wealth of data that will enable a better understanding of the composition of condensed matter bodies in the solar system. Minerals, ices, liquids, and other materials have been detected and mapped on the Earth and all planets and/or their satellites where the surface can be observed from space, with the exception of Venus whose thick atmosphere limits surface observation. Basaltic minerals (e.g., pyroxene and olivine) have been detected with spectroscopy on the Earth, Moon, Mars and some asteroids. The greatest mineralogic diversity seen from space is observed on the Earth and Mars. The Earth, with oceans, active tectonic and hydrologic cycles, and biological processes, displays the greatest material diversity including the detection of amorphous and crystalline inorganic materials, organic compounds, water and water ice. Water ice is a very common mineral throughout the Solar System and has been unambiguously detected or inferred in every planet and/or their moon(s) where good spectroscopic data has been obtained. In addition to water ice, other molecular solids have been observed in the solar system using spectroscopic methods. Solid carbon dioxide is found on all systems beyond the Earth except Pluto, although CO2 sometimes appears to be trapped in other solids rather than as an ice on some

  15. Dynamics of ferrocene in molecular sieves probed by Mossbauer spectroscopy and nuclear resonant scattering

    Energy Technology Data Exchange (ETDEWEB)

    Asthalter, T [Institut fuer Physikalische Chemie, Universitat Stuttgart, D-70569 Stuttgart (Germany); Sergueev, I [European Synchrotron Radiation Facility, F-38043 Grenoble (France); Buerck, U van; Wagner, F E [Experimentalphysik E13, Technische Universitaet Muenchen, D-85747 Garching (Germany); Haerter, P [Anorganische Chemie, Technische Universitaet Muenchen, D-85747 Garching (Germany); Kornatowski, J [Max-Planck-Institut fuer Kohlenforschung, D-45470 Muelheim (Germany); Klingelhoefer, S; Behrens, P, E-mail: t.asthalter@ipc.uni-stuttgart.d [Anorganische Chemie, Leibniz-Universitaet Hannover, D-30167 Hannover (Germany)

    2010-03-01

    A detailed study on the slow dynamics of ferrocene in the unidimensional channels of the molecular sieves SSZ-24 and AlPO{sub 4}-5 has been carried out, using Moessbauer spectroscopy (MS), nuclear forward scattering (NFS) and synchrotron radiation-based perturbed angular correlations (SRPAC). In both host systems, anisotropic rotational dynamics is observed above 100 K. For SSZ-24, this anisotropy persists even above the bulk melting temperature of ferrocene. Various theoretical models are exploited for the study of anisotropic discrete jump rotations for the first time. The experimental data can be described fairly well by a jump model that involves reorientations of the molecular axis on a cone mantle with an opening angle dependant on temperature.

  16. Spectroscopy of neutral radium

    Energy Technology Data Exchange (ETDEWEB)

    Mol, Aran; De, Subhadeep; Jungmann, Klaus; Wilschut, Hans; Willmann, Lorenz [KVI, University of Groningen, Groningen (Netherlands)

    2008-07-01

    The heavy alkaline earth atoms radium is uniquely sensitive towards parity and time reversal symmetry violations due to a large enhancement of an intrinsic permanent electric dipole moment of the nucleous or the electron. Furthermore, radium is sensitive to atomic parity violation and the nuclear anapole moment. To prepare such experiments spectroscopy of relevant atomic states need to be done. At a later stage we will build a neutral atom trap for radium. We have built an atomic beam of the short lived isotope {sup 225}Ra with a flux of several 10{sup 4} atoms/sec. We are preparing the laser spectroscopy using this beam setup. In the preparation for efficient laser cooling and trapping we have successfully trapped barium, which is similar in it's requirements for laser cooling. The techniques which we have developed with barium can be used to trap rare radium isotopes. We report on the progress of the experiments.

  17. Electronic spectroscopies

    NARCIS (Netherlands)

    Weckhuysen, B.M.; Schoonheydt, R.A.

    2000-01-01

    Diffuse reflectance spectroscopy (DRS) in the ultraviolet, visible and near-infrared region is a versatile spectroscopic technique, as both d-d and charge transfer transitions of supported TMI can be probed. One of the advantages of electronic spectroscopy is that the obtained information is

  18. Optical Spectroscopy

    DEFF Research Database (Denmark)

    Thyrhaug, Erling

    The work presented in this thesis is broadly concerned with how complexation reactions and molecular motion can be characterized with the standard techniques in optical spectroscopy. The thesis aims to show a relatively broad range of methods for probing physico-chemical properties in fluorophore...... containing systems and are characterized using techniques in optical spectroscopy. Of the standard techniques in optical spectroscopy, particular attention has been paid to those based on time-resolved measurements and polarization, which is reflected in the experiment design in the projects. Not all...... reactions by optical spectroscopy. In project 1 simple steady-state absorption and fluorescence spectroscopy is used to determine the stoichiometries and equilibrium constants in the inclusion complex formation between cyclodextrins and derivatives of the water-insoluble oligo(phenylene vinylene) in aqueous...

  19. X-ray diffraction and Mössbauer spectroscopy study of fcc iron hydride FeH at high pressures and implications for the composition of the Earth's core

    Science.gov (United States)

    Narygina, Olga; Dubrovinsky, Leonid S.; McCammon, Catherine A.; Kurnosov, Alexander; Kantor, Innokenty Yu.; Prakapenka, Vitali B.; Dubrovinskaia, Natalia A.

    2011-07-01

    The phase fcc FeH x (x ~ 1) was synthesized at pressures over 30 GPa and temperatures over 1600(50) K. At room temperature this iron hydride is stable at pressures from 19(1) GPa up to at least 68(2) GPa (the highest pressure achieved in this study). A fit of the PV data collected for fcc FeH x at room temperature gives the following parameters for the equation of state: V 0 = 53.8(3) Å 3, K 0 = 99(5) GPa, K' = 11.7(5). Using this data the amount of H required to match the density of the Earth's core was estimated to be 0.5-1 wt.% hydrogen in the outer core and 0.08-0.16 wt.% hydrogen in the inner core. Our results also suggest that hydrogen and carbon do not occur together in the Earth's core.

  20. Rare Earth Market Review

    Institute of Scientific and Technical Information of China (English)

    2008-01-01

    @@ Oversupply of rare earths led to the significant price drop of rare earth mineral products and separated products in Chinese domestic market. To stabilize the price, prevent waste of resources, further improve regulation capability on domestic rare earth market and rare earth price and maintain sustaining and healthy development of rare earth industry, partial rare earth producers in Baotou and Jiangxi province projected to cease the production for one month.

  1. Note: Portable rare-earth element analyzer using pyroelectric crystal

    Energy Technology Data Exchange (ETDEWEB)

    Imashuku, Susumu, E-mail: imashuku.susumu.2m@kyoto-u.ac.jp; Fuyuno, Naoto; Hanasaki, Kohei; Kawai, Jun [Department of Materials Science and Engineering, Kyoto University, Sakyo, Kyoto 606-8501 (Japan)

    2013-12-15

    We report a portable rare-earth element analyzer with a palm-top size chamber including the electron source of a pyroelectric crystal and the sample stage utilizing cathodoluminescence (CL) phenomenon. The portable rare-earth element analyzer utilizing CL phenomenon is the smallest reported so far. The portable rare-earth element analyzer detected the rare-earth elements Dy, Tb, Er, and Sm of ppm order in zircon, which were not detected by scanning electron microscopy-energy dispersive X-ray spectroscopy analysis. We also performed an elemental mapping of rare-earth elements by capturing a CL image using CCD camera.

  2. Laser spectroscopy

    CERN Document Server

    Demtröder, Wolfgang

    Keeping abreast of the latest techniques and applications, this new edition of the standard reference and graduate text on laser spectroscopy has been completely revised and expanded. While the general concept is unchanged, the new edition features a broad array of new material, e.g., ultrafast lasers (atto- and femto-second lasers) and parametric oscillators, coherent matter waves, Doppler-free Fourier spectroscopy with optical frequency combs, interference spectroscopy, quantum optics, the interferometric detection of gravitational waves and still more applications in chemical analysis, medical diagnostics, and engineering.

  3. Moessbauer effect and full-potential linearized augmented plane wave band structure studies on Ho(Fe{sub 1-x}Co{sub x}){sub 2} intermetallics

    Energy Technology Data Exchange (ETDEWEB)

    Bednarski, M; Pszczola, J; Bodnar, W [Faculty of Physics and Applied Computer Science, AGH University of Science and Technology, A Mickiewicza Avenue 30, 30-059 Krakow (Poland); Stoch, P; Zachariasz, P; Suwalski, J, E-mail: pszczola@agh.edu.pl [Institute of Atomic Energy, 05-400 Swierk-Otwock (Poland)

    2011-05-01

    {sup 57}Fe Moessbauer effect spectra were collected at 4.2 K for the Ho(Fe{sub 1-x}Co{sub x}){sub 2} C15 Laves phases. The hyperfine interaction parameters, i.e. isomer shift, the magnetic hyperfine field and the quadrupole interaction parameter, were determined for the individual Fe/Co nearest neighbourhoods of iron atoms and also as average values for the sample as bulk. As a result of Fe/Co substitution, Slater-Pauling-type dependences for magnetic hyperfine fields corresponding to both the local area and the sample as bulk were observed, and a linear correlation between the local magnetic hyperfine field and the average magnetic hyperfine field was observed. Magnetic moments of atoms were obtained from band structure calculations using the full-potential linearized augmented plane wave method. The magnetic hyperfine field obtained from the experiment correlates linearly (but separately for weak and strong ferromagnetic areas) with the magnetic moment calculated per transition metal atom.

  4. Moessbauer studies of single crystal Pr sub 1 sub / sub 3 Sr sub 2 sub / sub 3 FeO sub 3

    CERN Document Server

    Uhm, Y R; Kim, C S; Tomioka, Y; Tokura, Y

    2000-01-01

    Single crystal Pr sub 1 sub / sub 3 Sr sub 2 sub / sub 3 FeO sub 3 was synthesized by using the floating zone method and the relation of magnetic properties and charge ordering transition with lattice dynamics was systematically investigated. Moessbauer spectra of Pr sub 1 sub / sub 3 sub S r sub 2 sub / sub 3 FeO sub 3 were taken at various temperatures ranging from 20 K to room temperature. The charge disproportionation, in which iron with valence states Fe sup 3 sup + and Fe sup 5 sup + was found in a ratio of 2:1, was detected in Pr sub 1 sub / sub 3 Sr sub 2 sub / sub 3 FeO sub 3 below 190+-3 K. Iron with valence state Fe sup 4 sup + coexisted in Pr sub 1 sub / sub 3 sub S r sub 2 sub / sub 3 FeO sub 3 at and above 150 K, and its ratio increased from 13 to 66 % with increasing temperature. This result means that charge-ordered and -disordered phases co-exist in Pr sub 1 sub / sub 3 Sr sub 2 sub / sub 3 FeO sub 3.

  5. Fluorescence spectroscopy

    DEFF Research Database (Denmark)

    Bagatolli, Luis

    2016-01-01

    Fluorescence spectroscopy is a powerful experimental tool used by scientists from many disciplines. During the last decades there have been important developments on distinct fluorescence methods, particularly those related to the study of biological phenomena. This chapter discusses...

  6. Characterization of the near-Earth Asteroid 2002NY40

    OpenAIRE

    Roberts, Jr., Lewis C.; Hall, Doyle T.; Lambert, John V.; Africano, John L.; Knox, Keith T.; Barros, Jacob K.; Hamada, Kris M.; Liang, Dennis; Sydney, Paul F.; Kervin, Paul

    2007-01-01

    In August 2002, the near-Earth asteroid 2002 NY40, made its closest approach to the Earth. This provided an opportunity to study a near-Earth asteroid with a variety of instruments. Several of the telescopes at the Maui Space Surveillance System were trained at the asteroid and collected adaptive optics images, photometry and spectroscopy. Analysis of the imagery reveals the asteroid is triangular shaped with significant self-shadowing. The photometry reveals a 20-hour period and the spectros...

  7. Moessbauer and magnetic studies of the ternary compound FeIn{sub 2}Se{sub 4}

    Energy Technology Data Exchange (ETDEWEB)

    Bodnar, I. V., E-mail: chemzav@bsuir.by; Pauliukavets, S. A. [Belarussian State University of Informatics and Radioelectronics (Belarus); Trukhanov, S. V. [National Academy of Sciences of Belarus, Scientific-Practical Materials Research Center (Belarus); Fedotova, Yu. A. [Belarus State University (Belarus)

    2012-05-15

    Single crystals of the ternary compound FeIn{sub 2}Se{sub 4} are grown by directional crystallization of the melt. The composition and structure of the single crystals are determined. The local states of iron ions in this compound are studied by nuclear {gamma}-resonance spectroscopy in transmission configuration. The temperature and field dependences of a specific magnetic moment for the ternary compound FeIn{sub 2}Se{sub 4} are measured in the temperature range 4-310 K in magnetic fields of 0-140 kOe. The reasons and mechanisms for magnetic state formation in single crystals of the obtained compound are discussed.

  8. Syntheses, Vibrational Spectroscopy, and Crystal Structure Determination from X-Ray Powder Diffraction Data of Alkaline Earth Dicyanamides M[N(CN) 2] 2 with M=Mg, Ca, Sr, and Ba

    Science.gov (United States)

    Jürgens, Barbara; Irran, Elisabeth; Schnick, Wolfgang

    2001-03-01

    The alkaline earth dicyanamides Mg[N(CN)2]2, Ca[N(CN)2]2, Sr[N(CN)2]2, and Ba[N(CN)2]2 were synthesized by ion exchange using Na[N(CN)2] and the respective nitrates or bromides as starting materials. The crystal structures were determined from X-ray powder diffractometry: Mg[N(CN)2]2, Pnnm, Z=2, a=617.14(3), b=716.97(3), and c=740.35(5) pm; Ca[N(CN)2]2 and Sr[N(CN)2]2, C2/c, Z=4; Ca[N(CN)2]2, a=1244.55(3), b=607.97(1), and c=789.81(1) pm, β=98.864(2)°; Sr[N(CN)2]2, a=1279.63(2), b=624.756(8), and c=817.56(1) pm, β=99.787(1)°; Ba[N(CN)2]2, Pnma, Z=4, a=1368.68(7), b=429.07(7), and c=1226.26(2) pm. The dicyanamides consist of the respective alkaline earth cations and bent planar [N(CN)2]- ions. The structural features were correlated with vibrational spectroscopic data. The thermal behavior was studied by thermoanalytical experiments.

  9. Earth from Above

    Science.gov (United States)

    Stahley, Tom

    2006-01-01

    Google Earth is a free online software that provides a virtual view of Earth. Using Google Earth, students can view Earth by hovering over features and locations they preselect or by serendipitously exploring locations that catch their fascination. Going beyond hovering, they can swoop forward and even tilt images to make more detailed…

  10. Rare Earth Resolution

    Institute of Scientific and Technical Information of China (English)

    Mei Xinyu

    2012-01-01

    BEFORE the early 1970s, China had no rare earth exports, and the world rare earth market was dominated by the United States, Europe and Japan. In the 1970s, China began to enter the world rare earth market and its share has picked up sharply in the following decades. Today, having the monopoly over global rare earth production, China must improve the benefits from rare earth production, not only from producing individual rare earth products, but also from mastering the intensive processing of rare earth products.

  11. Electron Spectroscopy

    Science.gov (United States)

    Siegbahn, Kai

    Wilhelm Conrad Röntgen's discovery of X radiation in 1895 in Wörzburg resulted in an immediate break-through not only in physics but also in Society, the latter mainly because of its sensational radiological applications. Within a short time it furthermore indirectly led to the discovery of radioactivity by Henri Becquerel. The discovery of X radiation opened the gate to modern atomic physics, and radioactivity to nuclear physics. Later on, the discovery of X-ray diffraction by Laue, Friedrich and Knipping in 1912 initiated the field of X-ray spectroscopy with its fundamental contributions to atomic and crystal structures. Secondary electrons were early observed in the scattered radiation when X-rays were hitting a sample. The development of the corresponding electron spectroscopy had to wait a much longer time for its maturity. A survey of electron spectroscopy is presented.

  12. Moessbauer and magnetoelastic investigations of the surface effects in Fe{sub 72}Cu{sub 1.5}Nb{sub 4}Si{sub 13.5}B{sub 9} nanocrystalline alloy

    Energy Technology Data Exchange (ETDEWEB)

    Szumiata, T. E-mail: szumiatt@inetia.plszumiatt@kiux.man.radom.pl; Brzozka, K.; Gawronski, M.; Gorka, B.; Blazquez-Gamez, J.S.; Kulik, T.; Zuberek, R.; Slawska-Waniewska, A

    2004-05-01

    An existence of effects connected with the surface of grains in nanocrystalline FINEMET-like Fe{sub 72}Cu{sub 1.5}Nb{sub 4}Si{sub 13.5}B{sub 9} alloy was verified by investigation of hyperfine and magnetoelastic properties. In the Moessbauer spectra (collected both at room temperature and close to T{sub c} of amorphous matrix) a broad, high field component was found, which could be attributed to the grains surface and interface region. Such interpretation is confirmed in magnetostrictive experiment pointing to a high value of surface magnetostriction constant.

  13. Dimeric Fe (II, III) complex of quinoneoxime as functional model of PAP enzyme: Moessbauer, magneto-structural and DNA cleavage studies

    Energy Technology Data Exchange (ETDEWEB)

    Salunke-Gawali, Sunita; Ahmed, Khursheed [University of Pune, Department of Chemistry (India); Varret, Francois; Linares, Jorge [Universite de Versailles, Laboratoire de Magnetisme et d' Optique, CNRS, UMR 8634 (France); Zaware, Santosh [University of Pune, Department of Chemistry (India); Date, Sadgopal [University of Pune, Department of Physics (India); Rane, Sandhya, E-mail: syrane@chem.unipune.ernet.in [University of Pune, Department of Chemistry (India)

    2008-07-15

    Purple acid phosphatase, (PAP), is known to contain dinuclear Fe{sub 2}{sup +2,+3} site with characteristic Fe{sup +3} <- Tyr ligand to metal charge transfer in coordination. Phthiocoloxime (3-methyl-2-hydroxy-1,4-naphthoquinone-1-oxime) ligand L, mimics (His/Tyr) ligation with controlled and unique charge transfers resulting in valence tautomeric coordination with mixed valent diiron site in model compound Fe-1: [{mu}-OH-Fe{sub 2}{sup +2,+3} (o-NQ{sub CH3ox}) (o-NSQ{sub CH3ox}){sub 2} (CAT) H{sub 2}O]. Fe-2: [Fe{sup +3}(o-NQ{sub CH3ox}) (p-NQ{sub CH3ox}){sub 2}]{sub 2} a molecularly associated dimer of phthiocoloxime synthesized for comparison of charge transfer. {sup 57}Fe Moessbauer studies was used to quantitize unusual valences due to ligand in dimeric Fe-1 and Fe-2 complexes which are supported by EPR and SQUID studies. {sup 57}Fe Moessbauer spectra for Fe-1 at 300 K indicates the presence of two quadrupole split asymmetric doublets due to the differences in local coordination geometries of [Fe{sup +3}]{sub A} and [Fe{sup +2}]{sub B} sites. The hyperfine interaction parameters are {delta}{sub A} = 0.152, ({Delta}E{sub Q}){sub A} 0.598 mm/s with overlapping doublet at {delta}{sub B} = 0.410 and ({Delta}E{sub Q}){sub B} 0.468 mm/s. Due to molecular association tendency of ligand, dimer Fe-2 possesses 100% Fe{sup +3}(h.s.) hexacoordinated configuration with isomer shift {delta} = 0.408 mm/s. Slightly distorted octahedral symmetry created by NQ{sub CH3ox} ligand surrounding Fe{sup +3}(h.s.) state generates small field gradient indicated by quadrupole split {Delta}E{sub Q} = 0.213 mm/s. Decrease of isomer shifts together with variation of quadrupole splits with temperature in Fe-1 dimer compared to Fe-2 is result of charge transfers in [Fe{sub 2}{sup +2,+3} SQ] complexes. EPR spectrum of Fe-1 shows two strong signals at g{sub 1} = 4.17 and g{sub 2} = 2.01 indicative of S = 3/2 spin state with an intermediate spin of Fe{sup +3}(h.s.) configuration. SQUID data of

  14. The Lifeworld Earth and a Modelled Earth

    Science.gov (United States)

    Juuti, Kalle

    2014-01-01

    The goal of this paper is to study the question of whether a phenomenological view of the Earth could be empirically endorsed. The phenomenological way of thinking considers the Earth as a material entity, but not as an object as viewed in science. In the learning science tradition, tracking the process of the conceptual change of the shape of the…

  15. The Lifeworld Earth and a Modelled Earth

    Science.gov (United States)

    Juuti, Kalle

    2014-01-01

    The goal of this paper is to study the question of whether a phenomenological view of the Earth could be empirically endorsed. The phenomenological way of thinking considers the Earth as a material entity, but not as an object as viewed in science. In the learning science tradition, tracking the process of the conceptual change of the shape of the…

  16. Raman spectroscopy

    Science.gov (United States)

    Raman spectroscopy has gained increased use and importance in recent years for accurate and precise detection of physical and chemical properties of food materials, due to the greater specificity and sensitivity of Raman techniques over other analytical techniques. This book chapter presents Raman s...

  17. Modern Spectroscopy

    Science.gov (United States)

    Barrow, Gordon M.

    1970-01-01

    Presents the basic ideas of modern spectroscopy. Both the angular momenta and wave-nature approaches to the determination of energy level patterns for atomic and molecular systems are discussed. The interpretation of spectra, based on atomic and molecular models, is considered. (LC)

  18. EarthKAM

    Data.gov (United States)

    National Aeronautics and Space Administration — Sponsored by NASA, EarthKAM (Earth Knowledge Acquired by Middle School Students) is an educational outreach program allowing middle school students to take pictures...

  19. Earth on the Move.

    Science.gov (United States)

    Naturescope, 1987

    1987-01-01

    Provides background information on the layers of the earth, the relationship between changes on the surface of the earth and its insides, and plate tectonics. Teaching activities are included, with some containing reproducible worksheets and handouts to accompany them. (TW)

  20. NASA Earth Exchange (NEX)

    Data.gov (United States)

    National Aeronautics and Space Administration — The NASA Earth Exchange (NEX) represents a new platform for the Earth science community that provides a mechanism for scientific collaboration and knowledge sharing....

  1. Astronomical Spectroscopy

    CERN Document Server

    Massey, Philip

    2010-01-01

    Spectroscopy is one of the most important tools that an astronomer has for studying the universe. This chapter begins by discussing the basics, including the different types of optical spectrographs, with extension to the ultraviolet and the near-infrared. Emphasis is given to the fundamentals of how spectrographs are used, and the trade-offs involved in designing an observational experiment. It then covers observing and reduction techniques, noting that some of the standard practices of flat-fielding often actually degrade the quality of the data rather than improve it. Although the focus is on point sources, spatially resolved spectroscopy of extended sources is also briefly discussed. Discussion of differential extinction, the impact of crowding, multi-object techniques, optimal extractions, flat-fielding considerations, and determining radial velocities and velocity dispersions provide the spectroscopist with the fundamentals needed to obtain the best data. Finally the chapter combines the previous materi...

  2. Grain Spectroscopy

    Science.gov (United States)

    Allamandola, L. J.

    1992-01-01

    Our fundamental knowledge of interstellar grain composition has grown substantially during the past two decades thanks to significant advances in two areas: astronomical infrared spectroscopy and laboratory astrophysics. The opening of the mid-infrared, the spectral range from 4000-400 cm(sup -1) (2.5-25 microns), to spectroscopic study has been critical to this progress because spectroscopy in this region reveals more about a materials molecular composition and structure than any other physical property. Infrared spectra which are diagnostic of interstellar grain composition fall into two categories: absorption spectra of the dense and diffuse interstellar media, and emission spectra from UV-Vis rich dusty regions. The former will be presented in some detail, with the latter only very briefly mentioned. This paper summarized what we have learned from these spectra and presents 'doorway' references into the literature. Detailed reviews of many aspects of interstellar dust are given.

  3. Capturing Near Earth Objects

    OpenAIRE

    Baoyin, Hexi; CHEN Yang; Li, Junfeng

    2011-01-01

    Recently, Near Earth Objects (NEOs) have been attracting great attention, and thousands of NEOs have been found to date. This paper examines the NEOs' orbital dynamics using the framework of an accurate solar system model and a Sun-Earth-NEO three-body system when the NEOs are close to Earth to search for NEOs with low-energy orbits. It is possible for such an NEO to be temporarily captured by Earth; its orbit would thereby be changed and it would become an Earth-orbiting object after a small...

  4. Transits of Earth-Like Planets

    CERN Document Server

    Kaltenegger, L

    2009-01-01

    Transmission spectroscopy of Earth-like exoplanets is a potential tool for habitability screening. Transiting planets are present-day "Rosetta Stones" for understanding extrasolar planets because they offer the possibility to characterize giant planet atmospheres and should provide an access to biomarkers in the atmospheres of Earth-like exoplanets, once they are detected. Using the Earth itself as a proxy we show the potential and limits of the transiting technique to detect biomarkers on an Earth-analog exoplanet in transit. We quantify the Earths cross section as a function of wavelength, and show the effect of each atmospheric species, aerosol, and Rayleigh scattering. Clouds do not significantly affect this picture because the opacity of the lower atmosphere from aerosol and Rayleigh losses dominates over cloud losses. We calculate the optimum signal-to-noise ratio for spectral features in the primary eclipse spectrum of an Earth-like exoplanet around a Sun-like star and also M stars, for a 6.5-m telesco...

  5. Synthesis, properties and Moessbauer study of ZrFe{sub 2-x}Ni{sub x} hydrides (x = 0.2-0.8)

    Energy Technology Data Exchange (ETDEWEB)

    Sivov, Roman B., E-mail: rsivov@mail.ru [Department of Material Science, Lomonosov Moscow State University, Leninskie Gory 3, Moscow 119991 (Russian Federation); Zotov, Timur A., E-mail: tim.zotov@gmail.com [Chemistry Department, Lomonosov Moscow State University, Leninskie Gory 3, Moscow 119991 (Russian Federation); Verbetsky, Victor N.; Filimonov, Dmitry S.; Pokholok, Konstantin V. [Chemistry Department, Lomonosov Moscow State University, Leninskie Gory 3, Moscow 119991 (Russian Federation)

    2011-09-15

    Research highlights: > ZrFe{sub 2-x}Ni{sub x} (x = 0.2, 0.4, 0.6, and 0.8) can accumulate up to 1.7-1.8 wt.% H{sub 2} at 295 K. > H{sub 2} desorption pressures at 295 K decreased from 325 (x = 0) to 115 atm (x = 0.8). > Isomer shifts (IS) remain constant with Ni content. > Absorption of H{sub 2} results in increase in IS and hyperfine fields for all samples. > Hydride decomposition process involves formation of intermediate hydride phase. - Abstract: Interaction of ZrFe{sub 2-x}Ni{sub x} (x = 0.2, 0.4, 0.6, and 0.8) pseudobinary intermetallic compounds with hydrogen was studied. It was found that these compounds can accumulate up to 1.7-1.8 wt.% H{sub 2} at room temperature. For all investigated ZrFe{sub 2-x}Ni{sub x}-H{sub 2} systems, thermodynamic functions of the {beta}-hydride {yields} {alpha}-solution phase transition and changes of metal matrix volume during formation of hydrides were calculated. It was shown that increase in Ni content leads to reduction of both desorption pressures and starting pressures of reaction with hydrogen in the first hydrogenation cycle compared to ZrFe{sub 2}. Moessbauer investigations, which have been carried out for all alloys as well as hydrides, revealed that Curie temperatures (T{sub c}) and average hyperfine fields (HF{sub av}) of initial alloys decrease with Ni content increase, while isomer shifts (IS) remain constant. Absorption of H{sub 2} results in significant increase in IS together with some increase in T{sub c} and HF{sub av} for all samples. The decomposition of the hydride phases to intermetallic phases while heating from 78 K to room temperature was found to be a two-step process involving formation of the hydride phases with intermediate hydrogen content.

  6. Nuclear spectroscopy

    CERN Document Server

    Ajzenberg-Selove, Fay

    1960-01-01

    Nuclear Spectroscopy, Part B focuses on the ways in which experimental data may be analyzed to furnish information about nuclear parameters and nuclear models in terms of which the data are interpreted.This book discusses the elastic and inelastic potential scattering amplitudes, role of beta decay in nuclear physics, and general selection rules for electromagnetic transitions. The nuclear shell model, fundamental coupling procedure, vibrational spectra, and empirical determination of the complex potential are also covered. This publication is suitable for graduate students preparing for exper

  7. Laser spectroscopy

    CERN Document Server

    Demtröder, Wolfgang

    2008-01-01

    Keeping abreast of the latest techniques and applications, this new edition of the standard reference and graduate text on laser spectroscopy has been completely revised and expanded. While the general concept is unchanged, the new edition features a broad array of new material, e.g., frequency doubling in external cavities, reliable cw-parametric oscillators, tunable narrow-band UV sources, more sensitive detection techniques, tunable femtosecond and sub-femtosecond lasers (X-ray region and the attosecond range), control of atomic and molecular excitations, frequency combs able to synchronize independent femtosecond lasers, coherent matter waves, and still more applications in chemical analysis, medical diagnostics, and engineering.

  8. The Earth's Magnetic Field

    OpenAIRE

    Edda Lína Gunnarsdóttir 1988

    2012-01-01

    The Earth's magnetic field is essential for life on Earth, as we know it, to exist. It forms a magnetic shield around the planet, protecting it from high energy particles and radiation from the Sun, which can cause damage to life, power systems, orbiting satellites, astronauts and spacecrafts. This report contains a general overview of the Earth's magnetic field. The different sources that contribute to the total magnetic field are presented and the diverse variations in the field are describ...

  9. Uderstanding Snowball Earth Deglaciation

    Science.gov (United States)

    Abbot, D. S.

    2012-12-01

    Earth, a normally clement planet comfortably in its star's habitable zone, suffered global or nearly global glaciation at least twice during the Neoproterozoic era (at about 635 and 710 million years ago). Viewed in the context of planetary evolution, these pan-global glaciations (Snowball Earth events) were extremely rapid, lasting only a few million years. The dramatic effect of the Snowball Earth events on the development of the planet can be seen through their link to rises in atmospheric oxygen and evolutionary innovations. These potential catastrophes on an otherwise clement planet can be used to gain insight into planetary habitability more generally. Since Earth is not currently a Snowball, a sound deglaciation mechanism is crucial for the viability of the Snowball Earth hypothesis. The traditional deglaciation mechanism is a massive build up of CO2 due to reduced weathering during Snowball Earth events until tropical surface temperatures reach the melting point. Once initiated, such a deglaciation might happen on a timescale of only dozens of thousands of years and would thrust Earth from the coldest climate in its history to the warmest. Therefore embedded in Snowball Earth events is an even more rapid and dramatic environmental change. Early global climate model simulations raised doubt about whether Snowball Earth deglaciation could be achieved at a CO2 concentration low enough to be consistent with geochemical data, which represented a potential challenge to the Snowball Earth hypothesis. Over the past few years dust and clouds have emerged as the essential missing additional processes that would allow Snowball Earth deglaciation at a low enough CO2 concentration. I will discuss the dust and cloud mechanisms and the modeling behind these ideas. This effort is critical for the broader implications of Snowball Earth events because understanding the specific deglaciation mechanism determines whether similar processes could happen on other planets.

  10. The Earth's early evolution.

    Science.gov (United States)

    Bowring, S A; Housh, T

    1995-09-15

    The Archean crust contains direct geochemical information of the Earth's early planetary differentiation. A major outstanding question in the Earth sciences is whether the volume of continental crust today represents nearly all that formed over Earth's history or whether its rates of creation and destruction have been approximately balanced since the Archean. Analysis of neodymium isotopic data from the oldest remnants of Archean crust suggests that crustal recycling is important and that preserved continental crust comprises fragments of crust that escaped recycling. Furthermore, the data suggest that the isotopic evolution of Earth's mantle reflects progressive eradication of primordial heterogeneities related to early differentiation.

  11. Near Earth Objects

    DEFF Research Database (Denmark)

    Wolff, Stefan

    2006-01-01

    , Near Earth Objects: Asteroids and comets following paths that bring them near the Earth. NEOs have collided with the Earth since its formation, some causing local devastation, some causing global climate changes, yet the threat from a collision with a near Earth object has only recently been recognised...... of starlight by the Sun, and therefore directly observe the structure of space-time. This thesis explores several aspects of the observation of NEOs with Gaia, emphasising detection of NEOs and the quality of orbits computed from Gaia observations. The main contribution is the work on motion detection...

  12. Capturing near-Earth asteroids around Earth

    Science.gov (United States)

    Hasnain, Zaki; Lamb, Christopher A.; Ross, Shane D.

    2012-12-01

    The list of detected near-Earth asteroids (NEAs) is constantly growing. NEAs are likely targets for resources to support space industrialization, as they may be the least expensive source of certain needed raw materials. The limited supply of precious metals and semiconducting elements on Earth may be supplemented or even replaced by the reserves floating in the form of asteroids around the solar system. Precious metals make up a significant fraction NEAs by mass, and even one metallic asteroid of ˜1km size and fair enrichment in platinum-group metals would contain twice the tonnage of such metals already harvested on Earth. There are ˜1000 NEAs with a diameter of greater than 1 km. Capturing these asteroids around the Earth would expand the mining industry into an entirely new dimension. Having such resources within easy reach in Earth's orbit could provide an off-world environmentally friendly remedy for impending terrestrial shortages, especially given the need for raw materials in developing nations. In this paper, we develop and implement a conceptually simple algorithm to determine trajectory characteristics necessary to move NEAs into capture orbits around the Earth. Altered trajectories of asteroids are calculated using an ephemeris model. Only asteroids of eccentricity less than 0.1 have been studied and the model is restricted to the ecliptic plane for simplicity. We constrain the time of retrieval to be 10 years or less, based on considerations of the time to return on investment. For the heliocentric phase, constant acceleration is assumed. The acceleration required for transporting these asteroids from their undisturbed orbits to the sphere of influence of the Earth is the primary output, along with the impulse or acceleration necessary to effect capture to a bound orbit once the Earth's sphere of influence is reached. The initial guess for the constant acceleration is provided by a new estimation method, similar in spirit to Edelbaum's. Based on the

  13. Raman Spectroscopy at High Pressures

    Directory of Open Access Journals (Sweden)

    Alexander F. Goncharov

    2012-01-01

    Full Text Available Raman spectroscopy is one of the most informative probes for studies of material properties under extreme conditions of high pressure. The Raman techniques have become more versatile over the last decades as a new generation of optical filters and multichannel detectors become available. Here, recent progress in the Raman techniques for high-pressure research and its applications in numerous scientific disciplines including physics and chemistry of materials under extremes, earth and planetary science, new materials synthesis, and high-pressure metrology will be discussed.

  14. Introducing Earth's Orbital Eccentricity

    Science.gov (United States)

    Oostra, Benjamin

    2015-01-01

    Most students know that planetary orbits, including Earth's, are elliptical; that is Kepler's first law, and it is found in many science textbooks. But quite a few are mistaken about the details, thinking that the orbit is very eccentric, or that this effect is somehow responsible for the seasons. In fact, the Earth's orbital eccentricity is…

  15. The Earth's Core.

    Science.gov (United States)

    Jeanloz, Raymond

    1983-01-01

    The nature of the earth's core is described. Indirect evidence (such as that determined from seismological data) indicates that it is an iron alloy, solid toward its center but otherwise liquid. Evidence also suggests that it is the turbulent flow of the liquid that generates the earth's magnetic field. (JN)

  16. Solid Earth: Introduction

    Science.gov (United States)

    Rummel, R.

    1991-10-01

    The principles of the solid Earth program are introduced. When considering the study of solid Earth from space, satellites are used as beacons, inertial references, free fall probes and carrying platforms. The phenomenon measured by these satellites and the processes which can be studied as a result of these measurements are tabulated. The NASA solid Earth program focusses on research into surface kinematics, Earth rotation, land, ice, and ocean monitoring. The ESA solid Earth program identifies as its priority the Aristoteles mission for determining the gravity and magnetic field globally, with high spatial resolution and high accuracy. The Aristoteles mission characteristics and goals are listed. The benefits of the improved gravity information that will be provided by this mission are highlighted. This information will help in the following research: geodesy, orbit mechanics, geodynamics, oceanography, climate sea level, and the atmosphere.

  17. Low-temperature Sn-119-Moessbauer study of superconducting Bi4Sr(3.5)Ca(2.5)Cu4Sn(0.015)O(16-y) ceramic (2212 phase)

    Science.gov (United States)

    Nishida, Tetsuaki; Katada, Motomi; Miura, Norio; Deshimaru, Yuichi; Yamazoe, Noboru; Matsumoto, Yasukuni; Takashima, Yoshimasa

    1992-04-01

    The Sn-119-Moessbauer spectra of superconducting Bi4Sr(3.5)Ca(2.5)Cu4Sn(0.015)O(16-y) ceramic (2212 phase, Tc, 77 K), measured between 298 K and 7 K, consist of singlet peaks of Sn(4+) with the deltas and Gammas of -0.01-0.07 and 1.05-1.27 mm/s, respectively. The ln A (absorption area)-vs.-T plot shows that the recoil-free fraction f increases with decreasing temperature, and that the Debye and Einstein temperatures are 340 and 185 K, respectively. The Theta(D) of 340 K suggests that the Sn(4+) is in the BiO5 pyramids. The ln A shows a 'normal' lattice vibration, probably because of the long Cu-O(3) distance and the displacement of O(3).

  18. Mixed alkaline earth effect in sodium aluminosilicate glasses

    DEFF Research Database (Denmark)

    Kjeldsen, Jonas; Smedskjær, Morten Mattrup; Mauro, John C.

    2013-01-01

    While the mixed alkali effect has received significant attention in the glass literature, the mixed alkaline earth effect has not been thoroughly studied. Here, we investigate the latter effect by partial substitution of magnesium for calcium in sodium aluminosilicate glasses. We use Raman and NMR...... spectroscopies to obtain insights into the structural and topological features of these glasses, and hence into the mixed alkaline earth effect. We demonstrate that the mixed alkaline earth effect manifests itself as a maximum in the amount of bonded tetrahedral units and as a minimum in liquid fragility index...

  19. Electrical resistivity and Moessbauer effect investigations on Tb{sub 0.27}Dy{sub 0.73}(Mn{sub 1-x}Fe{sub x}){sub 2} intermetallics

    Energy Technology Data Exchange (ETDEWEB)

    Bodnar, W. [Faculty of Physics and Applied Computer Science, AGH, Al. Mickiewicza 30, 30-059 Krakow (Poland); Stoch, P. [Institute of Atomic Energy, 05-400 Swierk-Otwock (Poland); Faculty of Materials Science and Ceramics, AGH, Al. Mickiewicza 30, 30-059 Krakow (Poland); Chmist, J. [Faculty of Physics and Applied Computer Science, AGH, Al. Mickiewicza 30, 30-059 Krakow (Poland); Pszczola, J., E-mail: pszczola@agh.edu.p [Faculty of Physics and Applied Computer Science, AGH, Al. Mickiewicza 30, 30-059 Krakow (Poland); Zachariasz, P.; Suwalski, J. [Institute of Atomic Energy, 05-400 Swierk-Otwock (Poland)

    2010-09-03

    This paper concerns synthesis, X-ray analysis (300 K), electrical resistivity and {sup 57}Fe Moessbauer effect studies (4.2 K) of complete Tb{sub 0.27}Dy{sub 0.73}(Mn{sub 1-x}Fe{sub x}){sub 2} intermetallic series, with a borderline compound Tb{sub 0.27}Dy{sub 0.73}Fe{sub 2} known as Terfenol-D. A cubic Laves phase Fd3m of the MgCu{sub 2}-type is observed across the series. The lattice parameter decreases parabolically with x. Electrical resistivity was measured in a wide temperature region across the Tb{sub 0.27}Dy{sub 0.73}(Mn{sub 1-x}Fe{sub x}){sub 2} series and the parameters which characterize resistivity dependence on temperature, including Debye temperature, were determined. Residual, phonon and magnetic contributions were separated from electrical resistivity. The magnetic contribution to electrical resistivity was applied to estimate Curie temperatures. The Curie temperature increases significantly with x. {sup 57}Fe Moessbauer effect measurements for the Tb{sub 0.27}Dy{sub 0.73}(Mn{sub 1-x}Fe{sub x}){sub 2} intermetallic system evidence an [1 0 0] easy axis of magnetization. Mn/Fe substitution introduces a local area, at sub-nanoscale, with different Mn/Fe neighbourhoods of the tested {sup 57}Fe atoms. Hyperfine interaction parameters, an isomer shift, a magnetic hyperfine field and a quadrupole interaction parameter were determined from the spectra both for the local neighbourhood area and, as averaged values, for the sample as bulk. The average magnetic hyperfine field increases parabolically with x. The correlation between Curie temperatures and magnetic hyperfine fields is discussed.

  20. SIMP spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    Hochberg, Yonit [Ernest Orlando Lawrence Berkeley National Laboratory, University of California,Berkeley, CA 94720 (United States); Department of Physics, University of California,Berkeley, CA 94720 (United States); Kuflik, Eric [Department of Physics, LEPP, Cornell University,Ithaca NY 14853 (United States); Murayama, Hitoshi [Ernest Orlando Lawrence Berkeley National Laboratory, University of California,Berkeley, CA 94720 (United States); Department of Physics, University of California,Berkeley, CA 94720 (United States); Kavli Institute for the Physics and Mathematics of the Universe (WPI),University of Tokyo Institutes for Advanced Study, University of Tokyo,Kashiwa 277-8583 (Japan); Center for Japanese Studies, University of California,Berkeley, CA 94720 (United States)

    2016-05-16

    We study the interactions between strongly interacting massive particle dark matter and the Standard Model via a massive vector boson that is kinetically mixed with the hypercharge gauge boson. The relic abundance is set by 3→2 self-interactions of the dark matter, while the interactions with the vector mediator enable kinetic equilibrium between the dark and visible sectors. We show that a wide range of parameters is phenomenologically viable and can be probed in various ways. Astrophysical and cosmological constraints are evaded due to the p-wave nature of dark matter annihilation into visible particles, while direct detection methods using electron recoils can be sensitive to parts of the parameter space. In addition, we propose performing spectroscopy of the strongly coupled dark sector at e{sup +}e{sup −} colliders, where the energy of a mono-photon can track the resonance structure of the dark sector. Alternatively, some resonances may decay back into Standard Model leptons or jets, realizing ‘hidden valley’ phenomenology at the LHC and ILC in a concrete fashion.

  1. Earth as art three

    Science.gov (United States)

    ,

    2010-01-01

    For most of us, deserts, mountains, river valleys, coastlines even dry lakebeds are relatively familiar features of the Earth's terrestrial environment. For earth scientists, they are the focus of considerable scientific research. Viewed from a unique and unconventional perspective, Earth's geographic attributes can also be a surprising source of awe-inspiring art. That unique perspective is space. The artists for the Earth as Art Three exhibit are the Landsat 5 and Landsat 7 satellites, which orbit approximately 705 kilometers (438 miles) above the Earth's surface. While studying the images these satellites beam down daily, researchers are often struck by the sheer beauty of the scenes. Such images inspire the imagination and go beyond scientific value to remind us how stunning, intricate, and simply amazing our planet's features can be. Instead of paint, the medium for these works of art is light. But Landsat satellite sensors don't see light as human eyes do; instead, they see radiant energy reflected from Earth's surface in certain wavelengths, or bands, of red, green, blue, and infrared light. When these different bands are combined into a single image, remarkable patterns, colors, and shapes emerge. The Earth as Art Three exhibit provides fresh and inspiring glimpses of different parts of our planet's complex surface. The images in this collection were chosen solely based on their aesthetic appeal. Many of the images have been manipulated to enhance color variations or details. They are not intended for scientific interpretation only for your viewing pleasure. Enjoy!

  2. Sun-Earth Days

    Science.gov (United States)

    Thieman, J.; Ng, C.; Lewis, E.; Cline, T.

    2010-08-01

    Sun-Earth Day is a well-coordinated series of programs, resources and events under a unique yearly theme highlighting the fundamentals of heliophysics research and missions. A menu of activities, conducted throughout the year, inspire and educate participants. Sun-Earth Day itself can vary in date, but usually is identified by a celebration on or near the spring equinox. Through the Sun-Earth Day framework we have been able to offer a series of coordinated events that promote and highlight the Sun, its connection to Earth and the other planets. Sun-Earth Day events are hosted by educators, museums, amateur astronomers and scientists and occur at schools, community groups, parks, planetaria and science centers around the globe. Sun-Earth Day raises the awareness and knowledge of formal and informal education audiences concerning space weather and heliophysics. By building on the success of Sun-Earth Day yearly celebrations, we seek to affect people of all backgrounds and ages with the wonders of heliophysics science, discovery, and exploration in ways that are both tangible and meaningful to their lives.

  3. Accretion of the Earth.

    Science.gov (United States)

    Canup, Robin M

    2008-11-28

    The origin of the Earth and its Moon has been the focus of an enormous body of research. In this paper I review some of the current models of terrestrial planet accretion, and discuss assumptions common to most works that may require re-examination. Density-wave interactions between growing planets and the gas nebula may help to explain the current near-circular orbits of the Earth and Venus, and may result in large-scale radial migration of proto-planetary embryos. Migration would weaken the link between the present locations of the planets and the original provenance of the material that formed them. Fragmentation can potentially lead to faster accretion and could also damp final planet orbital eccentricities. The Moon-forming impact is believed to be the final major event in the Earth's accretion. Successful simulations of lunar-forming impacts involve a differentiated impactor containing between 0.1 and 0.2 Earth masses, an impact angle near 45 degrees and an impact speed within 10 per cent of the Earth's escape velocity. All successful impacts-with or without pre-impact rotation-imply that the Moon formed primarily from material originating from the impactor rather than from the proto-Earth. This must ultimately be reconciled with compositional similarities between the Earth and the Moon.

  4. Spectroscopy and dynamics of rare earth doped fluorides

    NARCIS (Netherlands)

    Ebens, Willem Omco

    1995-01-01

    The defect structure of RE doped Fluorides has been studied along with the conductivity properties, using a variety of techniques, both experimental and theoretical. Two systems have been studied in detail, which represent two kinds of defect states for RE doped SrFr. The system SrFr:CeF, has been t

  5. Earth Science Informatics - Overview

    Science.gov (United States)

    Ramapriyan, H. K.

    2017-01-01

    Over the last 10-15 years, significant advances have been made in information management, there are an increasing number of individuals entering the field of information management as it applies to Geoscience and Remote Sensing data, and the field of informatics has come to its own. Informatics is the science and technology of applying computers and computational methods to the systematic analysis, management, interchange, and representation of science data, information, and knowledge. Informatics also includes the use of computers and computational methods to support decision making and applications. Earth Science Informatics (ESI, a.k.a. geoinformatics) is the application of informatics in the Earth science domain. ESI is a rapidly developing discipline integrating computer science, information science, and Earth science. Major national and international research and infrastructure projects in ESI have been carried out or are on-going. Notable among these are: the Global Earth Observation System of Systems (GEOSS), the European Commissions INSPIRE, the U.S. NSDI and Geospatial One-Stop, the NASA EOSDIS, and the NSF DataONE, EarthCube and Cyberinfrastructure for Geoinformatics. More than 18 departments and agencies in the U.S. federal government have been active in Earth science informatics. All major space agencies in the world, have been involved in ESI research and application activities. In the United States, the Federation of Earth Science Information Partners (ESIP), whose membership includes over 180 organizations (government, academic and commercial) dedicated to managing, delivering and applying Earth science data, has been working on many ESI topics since 1998. The Committee on Earth Observation Satellites (CEOS)s Working Group on Information Systems and Services (WGISS) has been actively coordinating the ESI activities among the space agencies.

  6. Earth Science Informatics - Overview

    Science.gov (United States)

    Ramapriyan, H. K.

    2017-01-01

    Over the last 10-15 years, significant advances have been made in information management, there are an increasing number of individuals entering the field of information management as it applies to Geoscience and Remote Sensing data, and the field of informatics has come to its own. Informatics is the science and technology of applying computers and computational methods to the systematic analysis, management, interchange, and representation of science data, information, and knowledge. Informatics also includes the use of computers and computational methods to support decision making and applications. Earth Science Informatics (ESI, a.k.a. geoinformatics) is the application of informatics in the Earth science domain. ESI is a rapidly developing discipline integrating computer science, information science, and Earth science. Major national and international research and infrastructure projects in ESI have been carried out or are on-going. Notable among these are: the Global Earth Observation System of Systems (GEOSS), the European Commissions INSPIRE, the U.S. NSDI and Geospatial One-Stop, the NASA EOSDIS, and the NSF DataONE, EarthCube and Cyberinfrastructure for Geoinformatics. More than 18 departments and agencies in the U.S. federal government have been active in Earth science informatics. All major space agencies in the world, have been involved in ESI research and application activities. In the United States, the Federation of Earth Science Information Partners (ESIP), whose membership includes over 180 organizations (government, academic and commercial) dedicated to managing, delivering and applying Earth science data, has been working on many ESI topics since 1998. The Committee on Earth Observation Satellites (CEOS)s Working Group on Information Systems and Services (WGISS) has been actively coordinating the ESI activities among the space agencies.The talk will present an overview of current efforts in ESI, the role members of IEEE GRSS play, and discuss

  7. Earth before life.

    Science.gov (United States)

    Marzban, Caren; Viswanathan, Raju; Yurtsever, Ulvi

    2014-01-09

    A recent study argued, based on data on functional genome size of major phyla, that there is evidence life may have originated significantly prior to the formation of the Earth. Here a more refined regression analysis is performed in which 1) measurement error is systematically taken into account, and 2) interval estimates (e.g., confidence or prediction intervals) are produced. It is shown that such models for which the interval estimate for the time origin of the genome includes the age of the Earth are consistent with observed data. The appearance of life after the formation of the Earth is consistent with the data set under examination.

  8. Whole-Earth Decompression Dynamics

    OpenAIRE

    Herndon, J. Marvin

    2005-01-01

    The principles of Whole-Earth Decompression Dynamics are disclosed leading to a new way to interpret whole-Earth dynamics. Whole-Earth Decompression Dynamics incorporates elements of and unifies the two seemingly divergent dominant theories of continential displacement, plate tectonics theory and Earth expansion theory. Whole-Earth decompression is the consequence of Earth formation from within a Jupiter-like protoplanet with subsequent loss of gases and ices and concomitant rebounding. The i...

  9. Earth rotation and geodynamics

    Science.gov (United States)

    Bogusz, Janusz; Brzezinski, Aleksander; Kosek, Wieslaw; Nastula, Jolanta

    2015-12-01

    This paper presents the summary of research activities carried out in Poland in 2011-2014 in the field of Earth rotation and geodynamics by several Polish research institutions. It contains a summary of works on Earth rotation, including evaluation and prediction of its parameters and analysis of the related excitation data as well as research on associated geodynamic phenomena such as geocentre motion, global sea level change and hydrological processes. The second part of the paper deals with monitoring of geodynamic phenomena. It contains analysis of geodynamic networks of local, and regional scale using space (GNSS and SLR) techniques, Earth tides monitoring with gravimeters and water-tube hydrostatic clinometer, and the determination of secular variation of the Earth' magnetic field.

  10. Earth science: Extraordinary world

    Science.gov (United States)

    Day, James M. D.

    2016-09-01

    The isotopic compositions of objects that formed early in the evolution of the Solar System have been found to be similar to Earth's composition -- overturning notions of our planet's chemical distinctiveness. See Letters p.394 & p.399

  11. Gambling with the earth

    CERN Multimedia

    Muir, H

    2000-01-01

    The probability that dangerous Earth-devouring particles will be born at a new accelerator in the US may be tiny, but scientists have played down the devastating potential costs in their risk assessments according to a physicist (1 page).

  12. Astronomy: Earth's seven sisters

    Science.gov (United States)

    Snellen, Ignas A. G.

    2017-02-01

    Seven small planets whose surfaces could harbour liquid water have been spotted around a nearby dwarf star. If such a configuration is common in planetary systems, our Galaxy could be teeming with Earth-like planets. See Letter p.456

  13. Rare Earth Market Review

    Institute of Scientific and Technical Information of China (English)

    2008-01-01

    @@ July 20~31 Rare earth market still went downward, which was mainly led by sluggish demand for didymium products. Weak demand by domestic NdFeB market was attributed to continuous price falling of didymium mischmetal.

  14. Analyzing earth's surface data

    Science.gov (United States)

    Barr, D. J.; Elifrits, C. D.

    1979-01-01

    Manual discusses simple inexpensive image analysis technique used to interpret photographs and scanner of data of Earth's surface. Manual is designed for those who have no need for sophisticated computer-automated analysis procedures.

  15. Managing Planet Earth.

    Science.gov (United States)

    Clark, William C.

    1989-01-01

    Discusses the human use of the planet earth. Describes the global patterns and the regional aspects of change. Four requirements for the cultivation of leadership and institutional competence are suggested. Lists five references for further reading. (YP)

  16. Earliest life on earth

    CERN Document Server

    Golding, Suzanne D

    2010-01-01

    This volume integrates the latest findings on earliest life forms, identified and characterized in some of the oldest rocks on Earth. It places emphasis on the integration of analytical methods with observational techniques and experimental simulations.

  17. Earth/Lands

    OpenAIRE

    2011-01-01

    Earth is an essentially original and misunderstood raw material with great potential, from the positive environmental and energy ratio, to its admirable capacity to integrate other materials such as stone, wood, brick, lime, vegetable fibres, etc., capable also of constituting the sole material for whole buildings in climactical and geographically extreme situations. Earth offers a great capacity to respond to the housing needs of millions of human beings, not only quantitative needs compa...

  18. Earth rotation and geodynamics

    OpenAIRE

    Bogusz Janusz; Brzezinski Aleksander; Kosek Wieslaw; Nastula Jolanta

    2015-01-01

    This paper presents the summary of research activities carried out in Poland in 2011-2014 in the field of Earth rotation and geodynamics by several Polish research institutions. It contains a summary of works on Earth rotation, including evaluation and prediction of its parameters and analysis of the related excitation data as well as research on associated geodynamic phenomena such as geocentre motion, global sea level change and hydrological processes. The second part of the paper deals wit...

  19. Laser spectroscopy of radium

    Energy Technology Data Exchange (ETDEWEB)

    Santra, Bodhaditya; Dammalapati, Umakanth; Jungmann, Klaus; Willmann, Lorenz [KVI, University of Groningen (Netherlands)

    2011-07-01

    Searches for permanent electric dipole moments (EDMs) of fundamental particles are sensitive probes of physics beyond the Standard Model. Fundamental EDMs can experience enhancements in atomic and molecular systems. In particular, isotopes of the heavy alkaline earth element radium exhibit the largest known enhancement factors for any atomic systems due to their atomic and nuclear structure. A sensitive search for EDMs will require an efficient use of the rare isotopes, which are available from radioactive sources or at rare isotope facilities like TRI{mu}P at KVI. Here, laser cooling and trapping methods play a crucial role. The main transitions from the ground state have been identified by laser spectroscopy. Nevertheless, the strongest cooling transitions 7s{sup 2} {sup 1}S{sub 0}-7s7p {sup 1}P{sub 1} suffers from strong leakage to metastable states, similar to the case of barium. We describe the experimental approach to determine the wavelength of the three needed repump transitions, which then will permit an efficient capture of radium atoms into a magneto optical trap.

  20. Toward other Earths

    Science.gov (United States)

    Hatzes, Artie P.

    2016-04-01

    How common are habitable Earth-like planets? This is a key question that drives much of current research in exoplanets. To date, we have discovered over one thousand exoplanets, mostly through the transit method. Among these are Earth-size planets, but these orbit very close to the star (semi-major axis approximately 0.01 Astronomical Units). Potentially rocky planets have also been discovered in a star's habitable zone, but these have approximately twice the radius of the Earth. These certainly do not qualify as Earth "twins". Several hundreds of multi-planet systems have also been discovered, but these are mostly ultra-compact systems with up to seven planets all with orbital distances less than that of Mercury in our solar system. The detection of a planetary system that is the direct analog of our solar system still eludes us. After an overview of the current status of exoplanet discoveries I will discuss the prospects and challenges of finding such Earth analogs from the ground and from future space missions like PLATO. After over two decades of searching, we may well be on the brink of finding other Earths.

  1. Photoelectron spectroscopy and Auger electron spectroscopy of solids and surfaces

    Energy Technology Data Exchange (ETDEWEB)

    Kowalczyk, S.P.

    1976-01-01

    The use of photoelectron spectroscopy, primarily x-ray photoelectron spectroscopy, to obtain information on the electronic structure of a wide variety of solids (especially the bulk electronic structure of solids) is covered. Both valence band and core-level spectra, as well as a few cases of photon excited Auger electron spectroscopy, are employed in the investigations to derive information on N(E). The effect of several modulations inherent in the measured I(E)'s, such as final state band structure, cross section, and relaxation, is discussed. Examples of many-electron interactions in PES are given. Some experimental aspects of PES and AES studies are given with emphasis on sample preparation techniques. Multiple splitting of core levels is examined using the Mn levels in MnF/sub 2/ as a detailed case study. Core level splittings in transition metals, rare earth metals, transition metal halides and several alloys are also reported. The application of PES to the study of the chemical bond in some crystalline semiconductors and insulators, A/sup N/B/sup 8-N/ and A/sup N/B/sup 10-N/ compounds is treated, and a spectroscopic scale of ionicity for these compounds is developed from the measured ''s-band'' splitting in the valence band density of states. (GHT)

  2. Colors of extreme exo-Earth environments.

    Science.gov (United States)

    Hegde, Siddharth; Kaltenegger, Lisa

    2013-01-01

    The search for extrasolar planets has already detected rocky planets and several planetary candidates with minimum masses that are consistent with rocky planets in the habitable zone of their host stars. A low-resolution spectrum in the form of a color-color diagram of an exoplanet is likely to be one of the first post-detection quantities to be measured for the case of direct detection. In this paper, we explore potentially detectable surface features on rocky exoplanets and their connection to, and importance as, a habitat for extremophiles, as known on Earth. Extremophiles provide us with the minimum known envelope of environmental limits for life on our planet. The color of a planet reveals information on its properties, especially for surface features of rocky planets with clear atmospheres. We use filter photometry in the visible as a first step in the characterization of rocky exoplanets to prioritize targets for follow-up spectroscopy. Many surface environments on Earth have characteristic albedos and occupy a different color space in the visible waveband (0.4-0.9 μm) that can be distinguished remotely. These detectable surface features can be linked to the extreme niches that support extremophiles on Earth and provide a link between geomicrobiology and observational astronomy. This paper explores how filter photometry can serve as a first step in characterizing Earth-like exoplanets for an aerobic as well as an anaerobic atmosphere, thereby prioritizing targets to search for atmospheric biosignatures.

  3. Physical Characterization of Warm Spitzer-observed Near-Earth Objects

    NARCIS (Netherlands)

    Thomas, Cristina A.; Emery, Joshua P.; Trilling, David E.; Delbo, Marco; Hora, Joseph L.; Mueller, Michael

    2014-01-01

    Near-infrared spectroscopy of Near-Earth Objects (NEOs) connects diagnostic spectral features to specific surface mineralogies. The combination of spectroscopy with albedos and diameters derived from thermal infrared observations can increase the scientific return beyond that of the individual datas

  4. Chiroptical Spectroscopy

    Science.gov (United States)

    Gurst, Jerome E.

    1995-09-01

    A brief review of the literature, and Chemical and Engineering News in particular, reveals that the determination and use of optical activity is of increasing importance in today's commercial and research laboratories. The classical technique is to measure [alpha]D using a manual or recording polarimeter to provide a single value, the specific rotation at 589 nm. A spectropolarimeter can be used to determine optical activity through the UV-Visible spectrum (Optical Rotatory Dispersion [ORD]). At wavelengths far removed from electronic absorption bands, optical activity arises from circular birefringence, or the difference in the refractive index for left- and right-circularly polarized light; i.e., nL - nR does not equal zero for chiral materials. If the optical activity is measured through an absorption band, complex behavior is observed (a Cotton Effect curve). At an absorption band, chiral materials exhibit circular dichroism (CD), or a difference in the absorption of left- and right-circularly polarized light; epsilon L minus epsilon R does not equal zero. If the spectropolarimeter is set for the measurement of CD spectra, one observes what appears to be a UV-Vis spectrum except that some absorption bands are positive while others may be negative. Just as enantiomers have specific rotations that are equal and opposite at 589 nm (sodium D line), rotations are equal and opposite at all wavelengths, and CD measurements are equal and opposite at all wavelengths. Figure 1 shows the ORD curves for the enantiomeric carvones while Figure 2 contains the CD curves. The enantiomer of carvone that has the positive [alpha]D is obtained from caraway seeds and is known to have the S-configuration while the R-enantiomer is found in spearmint oil. Figure 1. ORD of S-(+)- and R-(-)-carvones Figure 2. CD of S-(+)- and R-(-)-carvones While little can be done to correlate stereochemistry with [alpha]D values, chiroptical spectroscopy (ORD and/or CD) often can be used to assign

  5. The earth's hydrological cycle

    CERN Document Server

    Bonnet, R-M; Calisto, M; Destouni, G; Gurney, R; Johannessen, J; Kerr, Y; Lahoz, WA; Rast, M

    2014-01-01

    This book gives a comprehensive presentation of our present understanding of the Earth's Hydrological cycle and the problems, consequences and impacts that go with this topic. Water is a central component in the Earth's system. It is indispensable for life on Earth in its present form and influences virtually every aspect of our planet's life support system. On relatively short time scales, atmospheric water vapor interacts with the atmospheric circulation and is crucial in forming the Earth's climate zones. Water vapor is the most powerful of the greenhouse gases and serves to enhance the tropospheric temperature. The dominant part of available water on Earth resides in the oceans. Parts are locked up in the land ice on Greenland and Antarctica and a smaller part is estimated to exist as groundwater. If all the ice over the land and all the glaciers were to melt, the sea level would rise by some 80 m. In comparison, the total amount of water vapor in the atmosphere is small; it amounts to ~ 25 kg/m2, or the ...

  6. The Sun and Earth

    Science.gov (United States)

    Gopalswamy, Natchimuthuk

    2012-01-01

    Thus the Sun forms the basis for life on Earth via the black body radiation it emits. The Sun also emits mass in the form of the solar wind and the coronal mass ejections (CMEs). Mass emission also occurs in the form of solar energetic particles (SEPs), which happens during CMEs and solar flares. Both the mass and electromagnetic energy output of the Sun vary over a wide range of time scales, thus introducing disturbances on the space environment that extends from the Sun through the entire heliosphere including the magnetospheres and ionospheres of planets and moons of the solar system. Although our habitat is located in the neutral atmosphere of Earth, we are intimately connected to the non-neutral space environment starting from the ionosphere to the magnetosphere and to the vast interplanetary space. The variability of the solar mass emissions results in the interaction between the solar wind plasma and the magnetospheric plasma leading to huge disturbances in the geospace. The Sun ionizes our atmosphere and creates the ionosphere. The ionosphere can be severely disturbed by the transient energy input from solar flares and the solar wind during geomagnetic storms. The complex interplay between Earth's magnetic field and the solar magnetic field carried by the solar wind presents varying conditions that are both beneficial and hazardous to life on earth. This seminar presents some of the key aspects of this Sun-Earth connection that we have learned since the birth of space science as a scientific discipline some half a century ago.

  7. Modeling the earth system

    Energy Technology Data Exchange (ETDEWEB)

    Ojima, D. [ed.

    1992-12-31

    The 1990 Global Change Institute (GCI) on Earth System Modeling is the third of a series organized by the Office for Interdisciplinary Earth Studies to look in depth at particular issues critical to developing a better understanding of the earth system. The 1990 GCI on Earth System Modeling was organized around three themes: defining critical gaps in the knowledge of the earth system, developing simplified working models, and validating comprehensive system models. This book is divided into three sections that reflect these themes. Each section begins with a set of background papers offering a brief tutorial on the subject, followed by working group reports developed during the institute. These reports summarize the joint ideas and recommendations of the participants and bring to bear the interdisciplinary perspective that imbued the institute. Since the conclusion of the 1990 Global Change Institute, research programs, nationally and internationally, have moved forward to implement a number of the recommendations made at the institute, and many of the participants have maintained collegial interactions to develop research projects addressing the needs identified during the two weeks in Snowmass.

  8. Better Than Earth

    CERN Document Server

    Heller, René

    2015-01-01

    Do We Inhabit The Best O All Possible Worlds? German mathematician Gottfried Leibniz thought so, writing in 1710 that our planet, warts and all, must be the most optimal one imaginable. Leibniz's idea was roundly scorned as unscientific wishful thinking, most notably by French author Voltaire in his magnum opus, Candide. Yet Leibniz might find sympathy from at least one group of scientists - the astronomers who have for decades treated Earth as a golden standard as they search for worlds beyond our own solar system. Because earthlings still know of just one living world - our own - it makes some sense to use Earth as a template in the search for life elsewhere, such as in the most Earth-like regions of Mars or Jupiter's watery moon Europa. Now, however, discoveries of potentially habitable planets orbiting stars other than our sun - exoplanets, that is - are challenging that geocentric approach.

  9. Better Than Earth

    Science.gov (United States)

    Heller, René

    2015-01-01

    Do we inhabit the best of all possible worlds? German mathematician Gottfried Leibniz thought so, writing in 1710 that our planet, warts and all, must be the most optimal one imaginable. Leibniz's idea was roundly scorned as unscientific wishful thinking, most notably by French author Voltaire in his magnum opus, Candide. Yet Leibniz might find sympathy from at least one group of scientists - the astronomers who have for decades treated Earth as a golden standard as they search for worlds beyond our own solar system. Because earthlings still know of just one living world - our own - it makes some sense to use Earth as a template in the search for life elsewhere, such as in the most Earth-like regions of Mars or Jupiter's watery moon Europa. Now, however, discoveries of potentially habitable planets orbiting stars other than our sun - exoplanets, that is - are challenging that geocentric approach.

  10. Geoneutrino and Hydridic Earth model

    CERN Document Server

    Bezrukov, Leonid

    2013-01-01

    Uranium, Thorium and Potassium-40 abundances in the Earth were calculated in the frame of Hydridic Earth model. Terrestrial heat producton from U, Th and K40 decays was calculated also. We must admit the existance of Earth expansion process to understand the obtained large value of terrestrial heat producton. The geoneutrino detector with volume more than 5 kT (LENA type) must be constructed to definitely separate between Bulk Silicat Earth model and Hydridic Earth model.

  11. How Big is Earth?

    Science.gov (United States)

    Thurber, Bonnie B.

    2015-08-01

    How Big is Earth celebrates the Year of Light. Using only the sunlight striking the Earth and a wooden dowel, students meet each other and then measure the circumference of the earth. Eratosthenes did it over 2,000 years ago. In Cosmos, Carl Sagan shared the process by which Eratosthenes measured the angle of the shadow cast at local noon when sunlight strikes a stick positioned perpendicular to the ground. By comparing his measurement to another made a distance away, Eratosthenes was able to calculate the circumference of the earth. How Big is Earth provides an online learning environment where students do science the same way Eratosthenes did. A notable project in which this was done was The Eratosthenes Project, conducted in 2005 as part of the World Year of Physics; in fact, we will be drawing on the teacher's guide developed by that project.How Big Is Earth? expands on the Eratosthenes project by providing an online learning environment provided by the iCollaboratory, www.icollaboratory.org, where teachers and students from Sweden, China, Nepal, Russia, Morocco, and the United States collaborate, share data, and reflect on their learning of science and astronomy. They are sharing their information and discussing their ideas/brainstorming the solutions in a discussion forum. There is an ongoing database of student measurements and another database to collect data on both teacher and student learning from surveys, discussions, and self-reflection done online.We will share our research about the kinds of learning that takes place only in global collaborations.The entrance address for the iCollaboratory is http://www.icollaboratory.org.

  12. Alkaline earth metal thioindates

    Energy Technology Data Exchange (ETDEWEB)

    Ivanov-Ehmin, B.N.; Ivlieva, V.I.; Filatenko, L.A.; Zajtsev, B.E.; Kaziev, G.Z.; Sarabiya, M.G.

    1984-08-01

    Alkaline earth metal thioindates of MIn/sub 2/S/sub 4/ composition were synthesized by interaction of alkaline earth metal oxoindates with hydrogen sulfide during heating. Investigation into the compounds by X-ray analysis showed that calcium compound crystallizes in cubic crystal system and strontium and barium compounds in rhombic crystal system. Lattice parameters and the number of formula units were determined. Thioindates of M/sub 3/In/sub 2/S/sub 6/ composition were synthesized, their individuality was shown.

  13. Rare (Earth Elements [score

    Directory of Open Access Journals (Sweden)

    Camilo Méndez

    2014-12-01

    Full Text Available Rare (Earth Elements is a cycle of works for solo piano. The cycle was inspired by James Dillon’s Book of Elements (Vol. I-V. The complete cycle will consist of 14 pieces; one for each selected rare (earth element. The chosen elements are Neodymium, Erbium, Tellurium, Hafnium, Tantalum, Technetium, Indium, Dysprosium, Lanthanium, Cerium, Europium, Terbium, Yttrium and Darmstadtium. These elements were selected due to their special atomic properties that in many cases make them extremely valuable for the development of new technologies, and also because of their scarcity. To date, only 4 works have been completed Yttrium, Technetium, Indium and Tellurium.

  14. Teaching earth science

    Science.gov (United States)

    Alpha, Tau Rho; Diggles, M.F.

    1998-01-01

    This CD-ROM contains 17 teaching tools: 16 interactive HyperCard 'stacks' and a printable model. They are separated into the following categories: Geologic Processes, Earthquakes and Faulting, and Map Projections and Globes. A 'navigation' stack, Earth Science, is provided as a 'launching' place from which to access all of the other stacks. You can also open the HyperCard Stacks folder and launch any of the 16 stacks yourself. In addition, a 17th tool, Earth and Tectonic Globes, is provided as a printable document. Each of the tools can be copied onto a 1.4-MB floppy disk and distributed freely.

  15. Quantizing Earth surface deformations

    Directory of Open Access Journals (Sweden)

    C. O. Bowin

    2015-03-01

    Full Text Available The global analysis of Bowin (2010 used the global 14 absolute Euler pole set (62 Myr history from Gripp and Gordon (1990 and demonstrated that plate tectonics conserves angular momentum. We herein extend that analysis using the more detailed Bird (2003 52 present-day Euler pole set (relative to a fixed Pacific plate for the Earth's surface, after conversion to absolute Euler poles. Additionally, new analytical results now provide new details on upper mantle mass anomalies in the outer 200 km of the Earth, as well as an initial quantizing of surface deformations.

  16. IR and the Earth

    DEFF Research Database (Denmark)

    Corry, Olaf; Stevenson, Hayley

    2017-01-01

    , in the end, one finite interconnected space. Together these two starting points make for the basic conundrum of Inter- national Relations and the Earth: how does a divided world live on a single globe? This introduction first provides an overview of the recent rise of ‘the environment’ in international......, ‘what has the environment ever done for IR?’, before the plan for the rest of the book sketches the content and direction of the ensuing chapters that explore the problematique of International Relations and the Earth....

  17. Synthesis of Polyketone STCO Promoted by Rare Earth Catalyst

    Institute of Scientific and Technical Information of China (English)

    GUO Jintang; ZHENG Yonghui; WANG Bo; TIAN Jing

    2006-01-01

    To lower the cost of polyketone synthesis, rare earth coordinate catalyst was introduced to the copolymerization of carbon monoxide (CO) and styrene (ST) to synthesize aliphatic polyketone STCO.The catalytic system was composed of rare earth neodymium acetate, yttrium acetate,2,2'-bipyridine, p-toluensulfonic acid, cupric p-toluensulfonate, and 1,4-benzoquinone.The catalyst and the copolymer were characterized by infrared spectrum and X-ray photoelectron spectroscopy respectively.The effects of each component of catalytic system and the kinds of rare earth acetates on catalytic activity of copolymerization were investigated.The results show that the proposed rare earth has distinct catalytic activity in the copolymerization of CO and ST and the maximum activity can reach 303.3 gSTCO/(mol·h).

  18. Bones of the Earth

    Science.gov (United States)

    Correa, Jose Miguel

    2014-01-01

    The film "Bones of the Earth" (Riglin, Cunninham & Correa, 2014) is an experience in collective inquiry and visual creation based on arts-based research. Starting from the meeting of different subjectivities and through dialogue, planning, shooting and editing, an audiovisual text that reconstructs a reflexive process of collective…

  19. Earth as art 4

    Science.gov (United States)

    ,

    2016-03-29

    Landsat 8 is the latest addition to the long-running series of Earth-observing satellites in the Landsat program that began in 1972. The images featured in this fourth installment of the Earth As Art collection were all acquired by Landsat 8. They show our planet’s diverse landscapes with remarkable clarity.Landsat satellites see the Earth as no human can. Not only do they acquire images from the vantage point of space, but their sensors record infrared as well as visible wavelengths of light. The resulting images often reveal “hidden” details of the Earth’s land surface, making them invaluable for scientific research.As with previous Earth As Art exhibits, these Landsat images were selected solely for their aesthetic appeal. Many of the images have been manipulated to enhance color variations or details. They are not intended for scientific interpretation—only for your viewing pleasure. What do you see in these unique glimpses of the Earth’s continents, islands, and coastlines?

  20. DIORAMA Earth Terrain Model

    Energy Technology Data Exchange (ETDEWEB)

    Werley, Kenneth Alan [Los Alamos National Lab. (LANL), Los Alamos, NM (United States)

    2015-03-10

    When simulating near-surface nuclear detonations, the terrain of the Earth can have an effect on the observed outputs. The critical parameter is called the “height of burst”. In order to model the effect of terrain on the simulations we have incorporated data from multiple sources to give 9 km resolution data with global coverage.

  1. Magnetic rare earth superlattices

    DEFF Research Database (Denmark)

    Majkrzak, C.F.; Kwo, J.; Hong, M.;

    1991-01-01

    Advances in molecular beam epitaxy deposition techniques have recently made it possible to grow, an atomic plane at a time, single crystalline superlattices composed of alternating layers of a magnetic rare earth, such as Gd, Dy, Ho, or Er, and metallic Y, which has an identical chemical structure...

  2. Google Earth Science

    Science.gov (United States)

    Baird, William H.; Padgett, Clifford W.; Secrest, Jeffery A.

    2015-01-01

    Google Earth has made a wealth of aerial imagery available online at no cost to users. We examine some of the potential uses of that data in illustrating basic physics and astronomy, such as finding the local magnetic declination, using landmarks such as the Washington Monument and Luxor Obelisk as gnomons, and showing how airport runways get…

  3. Understanding Earth's Albedo Effect

    Science.gov (United States)

    Fidler, Chuck

    2012-01-01

    Earth and space science in the middle school classroom are composed of intricately intertwined sets of conceptual systems (AAAS 1993; NRC 1996). Some systems of study, such as the water and rock cycles, are quite explicit and often found as stand-alone middle school science units. Other phenomena are not so apparent, yet they play an extremely…

  4. Olympus and Earth Day

    Institute of Scientific and Technical Information of China (English)

    2009-01-01

    Let your gaze rest upon the poster for Earth Day on April 22. A small polar bear clings tightly to the stem of an aero-vane. Staring at the vanishing floating ice on the wild sea, his eyes are full of panic and fear.

  5. Google Earth Science

    Science.gov (United States)

    Baird, William H.; Padgett, Clifford W.; Secrest, Jeffery A.

    2015-01-01

    Google Earth has made a wealth of aerial imagery available online at no cost to users. We examine some of the potential uses of that data in illustrating basic physics and astronomy, such as finding the local magnetic declination, using landmarks such as the Washington Monument and Luxor Obelisk as gnomons, and showing how airport runways get…

  6. Rare Earth Market Review

    Institute of Scientific and Technical Information of China (English)

    2009-01-01

    @@ Rare earth market continued drop tendency.There was not much transaction of didymium oxide and the alloy. Affected by reduced order of NdFeB magnetic materials and inactive dealings of didymium mischmetal,price of didymium mischmetal had dropped from RMB ¥95,000~98,000/ton to RMBY 93,000~95,000/ton currently.

  7. Cosmic rays on earth

    Energy Technology Data Exchange (ETDEWEB)

    Allkofer, O.C.; Grieder, P.K.F.

    1984-01-01

    A data collection is presented that covers cosmic rays on earth. Included are all relevant data on flux and intensity measurements, energy spectra, and related data of all primary and secondary components of the cosmic radiation at all levels in the atmosphere, at sea level and underground. In those cases where no useful experimental data have been available, theoretical predictions were substituted.

  8. "Galileo Calling Earth..."

    Science.gov (United States)

    National Aeronautics and Space Administration, Washington, DC.

    This guide presents an activity for helping students understand how data from the Galileo spacecraft is sent to scientists on earth. Students are asked to learn about the concepts of bit-rate and resolution and apply them to the interpretation of images from the Galileo Orbiter. (WRM)

  9. Earth flyby anomalies

    Energy Technology Data Exchange (ETDEWEB)

    Nieto, Michael Martin [Los Alamos National Laboratory; Anderson, John D [PROPULSION LAB.

    2009-01-01

    In the planet-centric system, a spacecraft should have the same initial and final energies, even though its energy and angular momentum will change in the barycenter of the solar system. However, without explanation, a number of earth flybys have yielded small energy changes.

  10. Protect the Earth

    Institute of Scientific and Technical Information of China (English)

    张永兴

    2011-01-01

    The earth, a blue globe, is very beautiful. It is the home to all the living things. But the environment around us is becoming worse and worse. People cut down trees to build houses and throw about litter. The air pollution is almost everywhere in the world!

  11. Citizens of Planet Earth

    DEFF Research Database (Denmark)

    Frisk, Kristian

    2015-01-01

    The inability of the nation-state system to handle contemporary environmental issues comprehensively has spurred greater cooperation between religious and secular civil society actors. An empirical analysis of the Alliance of Religions and Conservation (ARC) contributes to knowledge about this pr...... (2010a) have termed Terrapolitan Earth Religion....

  12. Whole-Earth Decompression Dynamics

    CERN Document Server

    Herndon, J M

    2005-01-01

    The principles of Whole-Earth Decompression Dynamics are disclosed leading to a new way to interpret whole-Earth dynamics. Whole-Earth Decompression Dynamics incorporates elements of and unifies the two seemingly divergent dominant theories of continential displacement, plate tectonics theory and Earth expansion theory. Whole-Earth decompression is the consequence of Earth formation from within a Jupiter-like protoplanet with subsequent loss of gases and ices and concomitant rebounding. The initial whole-Earth decompression is expected to result in a global system of major primary decompression cracks appearing in the rigid crust which persist as the basalt feeders for the global, mid-oceanic ridge system. As the Earth subsequently decompresses, the area of the Earth's surface increases by the formation of secondary decompression cracks, often located near the continental margins, presently identified as oceanic trenches. These secondary decompression cracks are subsequently in-filled with basalt, extruded fr...

  13. The Earth's Biosphere

    Science.gov (United States)

    2002-01-01

    In the last five years, scientists have been able to monitor our changing planet in ways never before possible. The Sea-viewing Wide Field-of-View Sensor (SeaWiFS), aboard the OrbView-2 satellite, has given researchers an unprecedented view of the biological engine that drives life on Earth-the countless forms of plants that cover the land and fill the oceans. 'There is no question the Earth is changing. SeaWiFS has enabled us, for the first time, to monitor the biological consequences of that change-to see how the things we do, as well as natural variability, affect the Earth's ability to support life,' said Gene Carl Feldman, SeaWiFS project manager at NASA's Goddard Space Flight Center, Greenbelt, Md. SeaWiFS data, based on continuous daily global observations, have helped scientists make a more accurate assessment of the oceans' role in the global carbon cycle. The data provide a key parameter in a number of ecological and environmental studies as well as global climate-change modeling. The images of the Earth's changing land, ocean and atmosphere from SeaWiFS have documented many previously unrecognized phenomena. The image above shows the global biosphere from June 2002 measured by SeaWiFS. Data in the oceans is chlorophyll concentration, a measure of the amount of phytoplankton (microscopic plants) living in the ocean. On land SeaWiFS measures Normalized Difference Vegetation Index, an indication of the density of plant growth. For more information and images, read: SeaWiFS Sensor Marks Five Years Documenting Earth'S Dynamic Biosphere Image courtesy SeaWiFS project and copyright Orbimage.

  14. Advances in atomic spectroscopy

    CERN Document Server

    Sneddon, J

    1997-01-01

    This series describes selected advances in the area of atomic spectroscopy. It is primarily intended for the reader who has a background in atmoic spectroscopy; suitable to the novice and expert. Although a widely used and accepted method for metal and non-metal analysis in a variety of complex samples, Advances in Atomic Spectroscopy covers a wide range of materials. Each Chapter will completely cover an area of atomic spectroscopy where rapid development has occurred.

  15. Basic molecular spectroscopy

    CERN Document Server

    Gorry, PA

    1985-01-01

    BASIC Molecular Spectroscopy discusses the utilization of the Beginner's All-purpose Symbolic Instruction Code (BASIC) programming language in molecular spectroscopy. The book is comprised of five chapters that provide an introduction to molecular spectroscopy through programs written in BASIC. The coverage of the text includes rotational spectra, vibrational spectra, and Raman and electronic spectra. The book will be of great use to students who are currently taking a course in molecular spectroscopy.

  16. Advances in atomic spectroscopy

    CERN Document Server

    Sneddon, J

    1995-01-01

    This series describes selected advances in the area of atomic spectroscopy. It is promarily intended for the reader who has a background in atmoic spectroscopy; suitable to the novice and expert. Although a widely used and accepted method for metal and non-metal analysis in a variety of complex samples, Advances in Atomic Spectroscopy covers a wide range of materials. Each Chapter will completely cover an area of atomic spectroscopy where rapid development has occurred.

  17. Earth: A Ringed Planet?

    Science.gov (United States)

    Hancock, L. O.; Povenmire, H.

    2010-12-01

    Among the most beautiful findings of the Space Age have been the discoveries of planetary rings. Not only Saturn but also Jupiter, Uranus and Neptune have rings; Saturn’s ring system has structures newly discovered; even Saturn's moon Rhea itself has a ring. All these are apparently supplied by material from the planetary moons (Rhea's ring by Rhea itself). The question naturally arises, why should the Earth not have a ring, and on the other hand, if it does, why has it not been observed? No rings have yet been observed in the inner solar system, but after all, rings in the inner solar system might simply tend to be fainter and more transient than those of the outer solar system: the inner solar system is more affected by the solar wind, and the Sun’s perturbing gravitational influence is greater. J.A. O’Keefe first suggested (1980) that Earth might have a ring system of its own. An Earth ring could account for some climate events. O’Keefe remarked that formation or thickening of a ring system in Earth’s equatorial plane could drive glaciation by deepening the chill of the winter hemisphere. (It is very well established that volcanic dust is an effective agent for the extinction of sunlight; this factor can be overwhelmingly apparent in eclipse observations.) O’Keefe died in 2000 and the speculation was not pursued, but the idea of an Earth ring has a prima facie reasonableness that calls for its renewed consideration. The program of this note is to hypothesize that, as O’Keefe proposed: (a) an Earth ring system exists; (b) it affects Earth's weather and climate; (c) the tektite strewn fields comprise filaments of the ring fallen to Earth's surface on various occasions of disturbance by comets or asteroids. On this basis, and drawing on the world's weather records, together with the Twentieth Century Reanalysis by NCEP/CIRES covering the period 1870-2010 and the geology of the tektite strewn fields, we herein propose the hypothesized Earth ring

  18. Symposium on atomic spectroscopy

    Energy Technology Data Exchange (ETDEWEB)

    1979-01-01

    Topics covered by the conference include: fast beam spectroscopy; astrophysical and other spectra; highly ionized spectroscopy; complex spectra; rydberg levels; fine structure, hyperfine structure and isotope shift; lineshapes; lifetimes, oscillator strengths and Einstein coefficients; and spectroscopy with lasers. Abstracts of the conference papers are presented. (GHT)

  19. Rotation and magnetism of Earth`s inner core

    Energy Technology Data Exchange (ETDEWEB)

    Glatzmaier, G.A. [Los Alamos National Lab., NM (United States); Roberts, P.H. [Univ. of California, Los Angeles, CA (United States)

    1996-12-13

    Three-dimensional numerical simulations of the geodynamo suggest that a super-rotation of Earth`s solid inner core relative to the mantle is maintained by magnetic coupling between the inner core and an eastward thermal wind in the fluid outer core. This mechanism, which is analogous to a synchronous motor, also plays a fundamental role in the generation of Earth`s magnetic field. 18 refs., 6 figs.

  20. Earth Science Multimedia Theater

    Science.gov (United States)

    Hasler, A. F.

    1998-01-01

    The presentation will begin with the latest 1998 NASA Earth Science Vision for the next 25 years. A compilation of the 10 days of animations of Hurricane Georges which were supplied daily on NASA to Network television will be shown. NASA's visualizations of Hurricane Bonnie which appeared in the Sept 7 1998 issue of TIME magazine. Highlights will be shown from the NASA hurricane visualization resource video tape that has been used repeatedly this season on network TV. Results will be presented from a new paper on automatic wind measurements in Hurricane Luis from 1 -min GOES images that will appear in the October BAMS. The visualizations are produced by the Goddard Visualization & Analysis Laboratory, and Scientific Visualization Studio, as well as other Goddard and NASA groups using NASA, NOAA, ESA, and NASDA Earth science datasets. Visualizations will be shown from the "Digital-HyperRes-Panorama" Earth Science ETheater'98 recently presented in Tokyo, Paris and Phoenix. The presentation in Paris used a SGI/CRAY Onyx Infinite Reality Super Graphics Workstation at 2560 X 1024 resolution with dual synchronized video Epson 71 00 projectors on a 20ft wide screen. Earth Science Electronic Theater '999 is being prepared for a December 1 st showing at NASA HQ in Washington and January presentation at the AMS meetings in Dallas. The 1999 version of the Etheater will be triple wide with at resolution of 3840 X 1024 on a 60 ft wide screen. Visualizations will also be featured from the new Earth Today Exhibit which was opened by Vice President Gore on July 2, 1998 at the Smithsonian Air & Space Museum in Washington, as well as those presented for possible use at the American Museum of Natural History (NYC), Disney EPCOT, and other venues. New methods are demonstrated for visualizing, interpreting, comparing, organizing and analyzing immense Hyperimage remote sensing datasets and three dimensional numerical model results. We call the data from many new Earth sensing satellites

  1. Visualizing Earth Materials

    Science.gov (United States)

    Cashman, K. V.; Rust, A.; Stibbon, E.; Harris, R.

    2016-12-01

    Earth materials are fundamental to art. They are pigments, they are clay, they provide form and color. Earth scientists, however, rarely attempt to make the physical properties of Earth materials visible through art, and similarly many artists use Earth materials without fully understanding their physical and chemical properties. Here we explore the intersection between art and science through study of the physical properties of Earth materials as characterized in the laboratory, and as transferred to paper using different techniques and suspending media. One focus of this collaboration is volcanic ash. Ash is interesting scientifically because its form provides information on the fundamental processes that drive volcanic eruptions, and determines its transport properties, and thus its potential to affect populations far downwind of the volcano. Ash properties also affect its behavior as an art material. From an aesthetic point of view, ash lends a granular surface to the image; it is also uncontrollable, and thus requires engagement between artist and medium. More fundamentally, using ash in art creates an exchange between the medium and the subject matter, and imparts something of the physical, visceral experience of volcanic landscapes to the viewer. Another component of this work uses powdered rock as a printing medium for geologic maps. Because different types of rock create powders with different properties (grain size distributions and shapes), the geology is communicated not only as color, but also by the physical characteristics of the material as it interacts with the paper. More importantly, the use of actual rocks samples as printing material for geologic maps not only makes a direct connection between the map and the material it represents, but also provides an emotional connection between the map, the viewer and the landscape, its colors, textures and geological juxtapositions. Both case studies provide examples not only of ways in which artists can

  2. Towards earth AntineutRino TomograpHy (EARTH)

    NARCIS (Netherlands)

    De Meijer, R. J.; Smit, F. D.; Brooks, F. D.; Fearick, R. W.; Wortche, H. J.; Mantovani, F.

    2006-01-01

    The programme Earth AntineutRino TomograpHy (EARTH) proposes to build ten underground facilities each hosting a telescope. Each telescope consists of many detector modules, to map the radiogenic heat sources deep in the interior of the Earth by utilising direction sensitive geoneutrino detection.

  3. sup 119 Sn-Moessbauer study on the normal lattice vibration of superconducting Bi(Pb) sub 2 Sr sub 2 Ca sub 2 Cu sub 3 Sn sub 0. 015 O sub 10-y

    Energy Technology Data Exchange (ETDEWEB)

    Nishida, Tetsuaki; Takashima, Yoshimasa (Kyushu Univ., Fukuoka (Japan). Faculty of Science); Katada, Motomi; Miura, Norio; Deshimaru, Yuichi; Otani, Tetsuya; Yamazoe, Noboru; Matsumoto, Yasukuni

    1991-04-01

    The {sup 119}Sn-Moessbauer spectrum of superconducting Bi(Pb){sub 2}Sr{sub 2}Ca{sub 2}Cu{sub 3}Sn{sub 0.015}O{sub 10-y} ceramic, having the T{sub c} of 108 K, consists of an intense doublet peak with the {delta} of 0.18 mmcenter dots{sup -1} and the {Delta} of 1.01 mmcenter dot s{sup -1} at room temperature. The {delta} and {Delta} indicate that the Sn{sup 4+} is substituted for the copper ion in the triangular CuO{sub 3} site of the CuO{sub 4} layer. The {delta} and the absorption area increase gradually with decreasing temperature and become saturated at about 30 K, being consistent with the theoretical curves obtained from the 'combined Debye and Einstein model'. Only the normal vibration without the softening is observed in the CuO{sub 4} layer. (author).

  4. China Rare Earth Market Review

    Institute of Scientific and Technical Information of China (English)

    2010-01-01

    @@ February, 2010 Rare earth separation plants and downstream producers like NdFeB magnetic materials and phosphor materials successively ceased production due to Spring Festival, Chinese New Year. Transactions in rare earth market were few affected by public holidays.

  5. Mirador - Earth Surface and Interior

    Data.gov (United States)

    National Aeronautics and Space Administration — Earth Science data access made simple. The goal of the Earth Surface and Interior focus area is to assess, mitigate and forecast the natural hazards that affect...

  6. China Rare Earth Market Review

    Institute of Scientific and Technical Information of China (English)

    2010-01-01

    @@ Active demands from downstream industry drove the price rise of rare earth products in Chinese domestic marketrecently, particularly didymium and dysprosium products. Prices of other rare earth products remained stable.

  7. China rare earth market review

    Institute of Scientific and Technical Information of China (English)

    2011-01-01

    Rare earth market fluctuated slightly recently and the transactions remained sluggish. Environment control was strengthened in southern China and many rare earth plants had gone out of production. Some traders were considering selling commodities at low p

  8. NASA Benefits Earth

    Science.gov (United States)

    Robinson, Julie A.

    2009-01-01

    This slide presentation reviews several ways in which NASA research has benefited Earth and made life on Earth better. These innovations include: solar panels, recycled pavement, thermometer pill, invisible braces for straightening teeth, LASIK, aerodynamic helmets and tires for bicycles, cataract detection, technology that was used to remove Anthrax spores from mail handling facilities, study of atomic oxygen erosion of materials has informed the restoration of artwork, macroencapsulation (a potential mechanism to deliver anti cancer drugs to specific sites), and research on a salmonella vaccine. With research on the International Space Station just beginning, there will be opportunities for entrepreneurs and other government agencies to access space for their research and development. As well as NASA continuing its own research on human health and technology development.

  9. Life Before Earth

    CERN Document Server

    Sharov, Alexei A

    2013-01-01

    An extrapolation of the genetic complexity of organisms to earlier times suggests that life began before the Earth was formed. Life may have started from systems with single heritable elements that are functionally equivalent to a nucleotide. The genetic complexity, roughly measured by the number of non-redundant functional nucleotides, is expected to have grown exponentially due to several positive feedback factors: gene cooperation, duplication of genes with their subsequent specialization, and emergence of novel functional niches associated with existing genes. Linear regression of genetic complexity on a log scale extrapolated back to just one base pair suggests the time of the origin of life 9.7 billion years ago. This cosmic time scale for the evolution of life has important consequences: life took ca. 5 billion years to reach the complexity of bacteria; the environments in which life originated and evolved to the prokaryote stage may have been quite different from those envisaged on Earth; there was no...

  10. Heat-pipe Earth.

    Science.gov (United States)

    Moore, William B; Webb, A Alexander G

    2013-09-26

    The heat transport and lithospheric dynamics of early Earth are currently explained by plate tectonic and vertical tectonic models, but these do not offer a global synthesis consistent with the geologic record. Here we use numerical simulations and comparison with the geologic record to explore a heat-pipe model in which volcanism dominates surface heat transport. These simulations indicate that a cold and thick lithosphere developed as a result of frequent volcanic eruptions that advected surface materials downwards. Declining heat sources over time led to an abrupt transition to plate tectonics. Consistent with model predictions, the geologic record shows rapid volcanic resurfacing, contractional deformation, a low geothermal gradient across the bulk of the lithosphere and a rapid decrease in heat-pipe volcanism after initiation of plate tectonics. The heat-pipe Earth model therefore offers a coherent geodynamic framework in which to explore the evolution of our planet before the onset of plate tectonics.

  11. Coherent Raman spectroscopy

    CERN Document Server

    Eesley, G L

    1981-01-01

    Coherent Raman Spectroscopy provides a unified and general account of the fundamental aspects of nonlinear Raman spectroscopy, also known as coherent Raman spectroscopy. The theoretical basis from which coherent Raman spectroscopy developed is described, along with its applications, utility, and implementation as well as advantages and disadvantages. Experimental data which typifies each technique is presented. This book is comprised of four chapters and opens with an overview of nonlinear optics and coherent Raman spectroscopy, followed by a discussion on nonlinear transfer function of matter

  12. Testing MOND on Earth

    CERN Document Server

    Ignatiev, A Yu

    2014-01-01

    MOND is one of the most popular alternatives to Dark Matter (DM). While efforts to directly detect DM in laboratories have been steadily pursued over the years, the proposed Earth-based tests of MOND are still in their infancy. Some proposals recently appeared in the literature are briefly reviewed, and it is argued that collaborative efforts of theorists and experimenters are needed to move forward in this exciting new area. Possible future directions are outlined.

  13. Superhydrophobic diatomaceous earth

    Science.gov (United States)

    Simpson, John T [Clinton, TN; D& #x27; Urso, Brian R [Clinton, TN

    2012-07-10

    A superhydrophobic powder is prepared by coating diatomaceous earth (DE) with a hydrophobic coating on the particle surface such that the coating conforms to the topography of the DE particles. The hydrophobic coating can be a self assembly monolayer of a perfluorinated silane coupling agent. The DE is preferably natural-grade DE where organic impurities have been removed. The superhydrophobic powder can be applied as a suspension in a binder solution to a substrate to produce a superhydrophobic surface on the substrate.

  14. Why Earth aurorae shine?

    Institute of Scientific and Technical Information of China (English)

    2006-01-01

    @@ By using the data obtained from three satellites of the Cluster mission launched by the European Space Agency (ESA), CAO Jinbin from the CAS Center for Space Science and Applied Research (CSSAR) and his US and European co-workers have clarified why Earth's aurorae shine.Their work entitled Joint Observations by Cluster Satellites of Bursty Bulk Flows in the Magnetotail was published in a recent issue of Journal of Geophysical Research.

  15. Life Before Earth

    OpenAIRE

    Sharov, Alexei A; Gordon, Richard

    2013-01-01

    An extrapolation of the genetic complexity of organisms to earlier times suggests that life began before the Earth was formed. Life may have started from systems with single heritable elements that are functionally equivalent to a nucleotide. The genetic complexity, roughly measured by the number of non-redundant functional nucleotides, is expected to have grown exponentially due to several positive feedback factors: gene cooperation, duplication of genes with their subsequent specialization,...

  16. Mission to Planet Earth

    Science.gov (United States)

    Tilford, Shelby G.; Wilson, Gregory S.; Backlund, Peter W.

    1991-01-01

    The NASA program described is an international study to predict changes in the earth's environment by means of multidisciplinary remote sensing from satellites. An international consortium dedicates satellites with advanced sensors to data collection, and a data processing system is described to collect and analyze a large amount of terrestrial data. The program requires international multidisciplinary involvement to collect and interpret the data and thereby manage and preserve the global environment.

  17. Earth Abides Arsenic Biotransformations

    OpenAIRE

    Zhu, Yong-Guan; Yoshinaga, Masafumi; Zhao, Fang-Jie; Rosen, Barry P.

    2014-01-01

    Arsenic is the most prevalent environmental toxic element and causes health problems throughout the world. The toxicity, mobility, and fate of arsenic in the environment are largely determined by its speciation, and arsenic speciation changes are driven, at least to some extent, by biological processes. In this article, biotransformation of arsenic is reviewed from the perspective of the formation of Earth and the evolution of life, and the connection between arsenic geochemistry and biology ...

  18. Earth before life

    OpenAIRE

    Marzban, Caren; Viswanathan, Raju; Yurtsever, Ulvi

    2014-01-01

    Background A recent study argued, based on data on functional genome size of major phyla, that there is evidence life may have originated significantly prior to the formation of the Earth. Results Here a more refined regression analysis is performed in which 1) measurement error is systematically taken into account, and 2) interval estimates (e.g., confidence or prediction intervals) are produced. It is shown that such models for which the interval estimate for the time origin of the genome i...

  19. Hunan Rare Earth Group Approved

    Institute of Scientific and Technical Information of China (English)

    2012-01-01

    <正>Following Guangdong,Guangxi,Fujian and Jiangxi,Hunan announced that it would consolidate its rare earth resources-the consolidation plan of Hunan Rare Earth Group has been approved. Consolidation of the rare earth industry of south China is in full swing.According to "Several Opinions of the State Council on Promoting the Sustainable and Healthy Development of Rare Earth Industry"(hereinafter referred to as "Several Opinions")released in 2011,

  20. China Rare Earth Market Review

    Institute of Scientific and Technical Information of China (English)

    2011-01-01

    September 20-30, 2011 Rare earth market remained steady recently. Quoted prices of didymium products by separation and smelting plants kept stable. Some rare earth industrial zones in Baotou, Sichuan and Ganzhou had suspended production with the intensified environmental protection control and consolidation of rare earth industry. Persons in the industry hold a positive attitude toward the rare earth market after the National Day' s holiday in China. The market will develop healthily and orderly in the future.