Onesnaženost okolja s težkimi kovinami in reševanje te problematike na učinkovit in hkrati stroškovno sprejemljiv način postaja v današnjem času velik izziv za družbo in njene znanstvenike. Namen diplomske naloge je preučiti adsorpcijo ionov svinca in kadmija na biooglju, pridelanemu iz celuloze in olivnih tropin. Teoretska in praktična znanja v zvezi s to tematiko so črpana tudi iz v zadnjem času objavljenih znanstvenih člankih, ki so nastali zaradi vse večjega problema onesnaževanja oko...
, major and trace element and isotope compositions of fertile lherzolites and thus cannot provide viable alternatives to the concept of melt extraction from pristine mantle as the major mechanism of CLM formation. Published data on xenoliths from andesitic volcanoes and on supra-subduction oceanic peridotites  show that the most common rocks in mantle wedge lithosphere are highly refractory harzburgites characterized by a combination of variable but generally high modal opx (18-30%) with very low modal cpx (1.5-3%). At a given olivine (or MgO) content, they have higher opx and silica, and lower cpx, Al and Ca contents than normal refractory peridotite xenoliths in continental basalts; the Mg-Si and Al-Si trends in those rocks resemble those in cratonic peridotites. These features may indicate either fluid fluxing during melting in the mantle wedge or selective post-melting metasomatic enrichments in silica to transform some olivine to opx. High oxygen fugacities and radiogenic Os-isotope compositions in those rocks may be related to enrichments by slab-derived fluids, but these features are not always coupled with trace element enrichments or patterns commonly attributed to "subduction zone metasomatism" deduced from studies of arc volcanic rocks and experiments. The valuable insights provided by experimental work and xenolith case studies are difficult to apply to many natural peridotite series because late-stage processes commonly overlap the evidence for initial melting. References:  Herzberg C., J. Petrol. 45: 2507 (2004).  Ionov D. & Sobolev A., GCA 72 (S1): A410 (2008).  Ionov D., Contrib. Miner. Petrol. (2007)  Ionov D., J. Petrol. doi: 10.1093/petrology/egp090 (2010)
data are compared with data on opx2 in mantle xenoliths, mostly observed in the mantle wedge above active or inactive subduction zones ( and references therein), as well as experimental data [5, 6]. These metasomatic opx2 are characterized by lower Al, Ca and Cr than opx1, as observed in Mont Coupet. Together with the presence of pores and of chloroapatite, the compositional characteristics of our samples are interpreted as the signature of Si-rich and Cl-bearing metasomatic fluids. They are similar to slab-derived fluids and may be in relation to the subduction event occurring during the Variscan orogeny, a possibility envisaged by  from recent Li isotopic studies.  Wagner, Goldschmidt Conf., 2015;  Wagner & Deloule, EGU, 2016;  Gu, PhD Thesis, Nancy, France, 2016;  Benard & Ionov, J. Petrol., 2013;  Perchuk & Yapaskurt, Geoch. Intern., 2013;  Grant et al, Am. Mineral., 2016.
Reworking of Archean mantle in the NE Siberian craton by carbonatite and silicate melt metasomatism: Evidence from a carbonate-bearing, dunite-to-websterite xenolith suite from the Obnazhennaya kimberlite
Ionov, Dmitri A.; Doucet, Luc S.; Xu, Yigang; Golovin, Alexander V.; Oleinikov, Oleg B.
The Obnazhennaya kimberlite in the NE Siberian craton hosts a most unusual cratonic xenolith suite, with common rocks rich in pyroxenes and garnet, and no sheared peridotites. We report petrographic and chemical data for whole rocks (WR) and minerals of 20 spinel and garnet peridotites from Obnazhennaya with Re-depletion Os isotope ages of 1.8-2.9 Ga (Ionov et al., 2015a) as well as 2 pyroxenites. The garnet-bearing rocks equilibrated at 1.6-2.8 GPa and 710-1050 °C. Some xenoliths contain vermicular spinel-pyroxene aggregates with REE patterns in clinopyroxene mimicking those of garnet. The peridotites show significant scatter of Mg# (0.888-0.924), Cr2O3 (0.2-1.4 wt.%) and high NiO (0.3-0.4 wt.%). None are pristine melting residues. Low-CaO-Al2O3 (≤0.9 wt.%) dunites and harzburgites are melt-channel materials. Peridotites with low to moderate Al2O3 (0.4-1.8 wt.%) usually have CaO > Al2O3, and some have pockets of calcite texturally equilibrated with olivine and garnet. Such carbonates, exceptional in mantle xenoliths and reported here for the first time for the Siberian mantle, provide direct evidence for modal makeover and Ca and LREE enrichments by ephemeral carbonate-rich melts. Peridotites rich in CaO and Al2O3 (2.7-8.0 wt.%) formed by reaction with silicate melts. We infer that the mantle lithosphere beneath Obnazhennaya, initially formed in the Mesoarchean, has been profoundly modified. Pervasive inter-granular percolation of highly mobile and reactive carbonate-rich liquids may have reduced the strength of the mantle lithosphere leading the way for reworking by silicate melts. The latest events before the kimberlite eruption were the formation of the carbonate-phlogopite pockets, fine-grained pyroxenite veins and spinel-pyroxene symplectites. The reworked lithospheric sections are preserved at Obnazhennaya, but similar processes could erode lithospheric roots in the SE Siberian craton (Tok) and the North China craton, where ancient melting residues and
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Full Text Available Selected Abstracts of the 2nd Congress of joint European Neonatal Societies (jENS 2017; Venice (Italy; October 31-November 4, 201758th ESPR Annual Meeting, 7th International Congress of UENPS, 3rd International Congress of EFCNIORGANIZING INSTITUTIONSEuropean Society for Paediatric Research (ESPR, European Society for Neonatology (ESN, Union of European Neonatal & Perinatal Societies (UENPS, European Foundation for the Care of Newborn Infants (EFCNIORGANIZING COMMITTEELuc Zimmermann (President of ESPR, Morten Breindahl (President of ESN, Manuel Sánchez Luna (President of UENPS, Silke Mader (Chairwoman of the Executive Board and Co-Founder of EFCNISCIENTIFIC COMMITTEEVirgilio P. Carnielli (Congress President Chair, Pierre Gressens (Past Scientific President, Umberto Simeoni, Manon Benders, Neil Marlow, Ola D. Saugstad, Petra Hüppi, Agnes van den HoogenSession "Circulation, Macro- and Microcirculation"ABS 1. MOLECULAR AND GENETIC MARKERS FOR PREDICTION OF RESISTANCE TO INOTROPIC THERAPY IN NEWBORNS WITH ARTERIAL HYPOTENSION • D. Kryuchko, A. Donnikov, E. Baibarina, I. Nikitina, O. Ionov, D. DegtyarevABS 2. GUT AND CEREBRAL OXYGENATION FROM BIRTH TO SIX WEEKS OF LIFE IN PRETERM INFANTS: WHAT IS NORMAL? • C. Howarth, T. Leung, J. Banerjee, J. Morris, N. AladangadyABS 3. CHANGES OF NT-PROBNP CONCENTRATION WITHIN THE FIRST WEEK OF LIFE IN PRETERM NEWBORNS WITH BIRTH WEIGHT ≤ 1,200 G • T. Talar, E. Gulczyńska, B. Cyranowicz, J. MollABS 4. RESISTANCE INDEX (RI OF ARTERIA CEREBRI ANTERIOR AND CEREBRAL OXYGENATION IN PRETERM INFANTS • N. Baik-Schneditz, B. Urlesberger, B. Schwaberger, L. Mileder, N. Höller, G. PichlerABS 5. THE INFLUENCE OF MATERNAL MEDICATION ON CLOSURE OF THE DUCTUS ARTERIOSUS IN THE PREMATURE NEWBORN • W.P. de Boode, J. van Drongelen, M.J.A. RaaymakersABS 6. INFLUENCE OF GLOBAL HYPOXIA AND REMOTE ISCHEMIC POSTCONDITIONING ON NATRIURETIC PEPTIDE EXPRESSION IN NEWBORN PIGLET HEART CHAMBERS • H. Kierkegaard, K.J. Kyng, B