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Sample records for nojima danso shuhen

  1. Evaluation for characteristics of around the Nojima fault; Butsuri tansa ni yoru `Nojima jishin danso` shuhen no jiban bussei ni kansuru ichihyoka

    Energy Technology Data Exchange (ETDEWEB)

    Shimizu, K.; Tsuji, T. [Newjec Inc., Osaka (Japan); Tsuji, M. [OYO Corp., Tokyo (Japan)

    1996-05-01

    Various surveys were conducted for the area around the Nojima fault, including ground surface, two-dimensional electrical and boring surveys and elastic wave tomography, in order to grasp properties of the ground around the `Nojima earthquake fault.` The resistivity image method as one of the two-dimensional electrical methods was used to grasp fault shapes over a wide range of the 1.6km long section extending between Esaki and Hirabayashi. The courses of traverse were set in the direction almost perpendicular to the fault. Boreholes were excavated and elastic wave tomography was conducted between the boreholes on the 9th and 17th courses of traverse, to confirm ground/mountain conditions and to compare the results with observed elastic wave velocities. Very low resistivities are observed at places where granite is distributed, suggesting that the fault-induced changes are not limited to the area around the fault. The zone in which elastic wave velocity decreases is narrow, 10m at the longest, at a velocity of 2.4km/s or lower, which is a low velocity for that propagating in granite. 5 refs., 4 figs.

  2. Polarimetric borehole radar measurement near Nojima fault and its application to subsurface crack characterization; Polarimetric borehole radar ni yoru Nojima danso shuhen no chika kiretsu keisoku jikken

    Energy Technology Data Exchange (ETDEWEB)

    Sato, M.; Taniguchi, Y.; Miwa, T.; Niitsuma, H. [Tohoku University, Sendai (Japan); Ikeda, R. [National Research Institute for Disaster Prevention, Tsukuba (Japan); Makino, K. [Geophysical Surveying and Consulting Co. Ltd., Tokyo (Japan)

    1997-05-27

    Practical application of subsurface crack characterization by the borehole radar measurement to which the radar polarimetric method was introduced was attempted to measuring objects for which the borehole radar has not been much used, for example, the inside of low loss rock mass or fracture zone where cracks tightly exist. A system was trially manufactured which makes the radar polarimetric measurement possible in the borehole at a 1000m depth and with a about 10cm diameter, and a field experiment was conducted for realizing the subsurface crack characterization near the Nojima fault. For the measuring experiment by the polarimetric borehole radar, used were Iwaya borehole and Hirabayashi borehole drilled in the north of Awaji-shima, Hyogo-ken. In a comparison of both polarization systems of Hirabayashi borehole, reflected waves at depths of 1038m and 1047m are relatively stronger in both polarization systems than those with the same polarization form and at different depths, whereas reflected waves around a 1017m depth are strong only as to the parallel polarization system. Characteristics of the polarization in this experiment indirectly reflect crack structures. 6 refs., 6 figs., 1 tab.

  3. Velocity structure of Nojima-fault by VSP method; VSP ho ni yoru Nojima danso no sokudo kozo

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    Kuwahara, Y.; Ito, H.; Kiguchi, T.; Miyazaki, T. [Geological Survey of Japan, Tsukuba (Japan)

    1996-05-01

    In order to investigate in detail structures of the fractured fault band, the VSP tests were conducted using a 750m deep borehole penetrating the Nojima fault in Awaji Island. The borehole penetrates the fault clay band at a depth of 624m in the Hirabayashi area. The offset VSP survey, conducted by the aid of hydrophone through the naked borehole, detects many characteristic phenomena resulting from the fault fracture. Largely fractured lithofacies are found by the core observation at a depth in a range from 557 to 673m. P-waves propagate at 4.6 and 5.1km/s above and below the fractured band, respectively. The fractured band is subdivided into 2 sections, both being of low speed of 4.5 and 3.1km/s. The X1 and X2 phases resulting from the fault fracture are also observed, above and below the fractured band. The causes for these wave phases are now under investigation. 4 figs.

  4. Evaluation of permeability of Nojima fault by hydrophone VSP; Hydrophone VSP ni yoru Nojima danso no tosuisei hyoka

    Energy Technology Data Exchange (ETDEWEB)

    Kiguchi, T.; Ito, H.; Kuwahara, Y.; Miyazaki, T. [Geological Survey of Japan, Tsukuba (Japan)

    1996-05-01

    The multi-offset hydrophone VSP experiments were carried out using a 750m deep borehole as the oscillation receiver, which penetrates the Nojima fault, to detect water-permeable cracks and evaluate their characteristics. Soil around the borehole is of granodiorite, and fault clay is found at a depth in a range from 623 to 624m. A total of 4 dynamite tunnels were provided around the borehole as the focus. The VSP results show that the tube waves are generated at 22 depths, including the depth at which fault clay is found. However, these waves are generated at only 6 depths in an approximately 150m long fracture zone, suggesting that the cracks in the zone are not necessarily permeable. It is also found that crack angle determined by the analysis of tube waves almost coincides with that of fault clay determined by the core, BHTV and FMI, and that permeability is of the order of 100md at a depth of fault clay or shallower. 3 refs., 2 figs., 2 tabs.

  5. Fault fracture zone evaluation using borehole geophysical logs; case study at Nojima fault, Awaji island; Kosei butsuri kenso ni yoru danso hasaitai no hyoka

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    Ikeda, R.; Omura, K. [National Research Institute for Disaster Prevention, Tsukuba (Japan); Yamamoto, T. [Geophysical Surveying and Consulting Co. Ltd., Tokyo (Japan)

    1997-10-22

    Ikeda, et al., in their examination of log data obtained from a borehole (2000m deep) drilled at Ashio, Tochigi Prefecture, where micro-earthquakes swarm at very shallow levels, pay special attention to porosity. Using correlationship between the porosity and elastic wave velocity/resistivity, the authors endeavor to find the presence of secondary pores, dimensions of faults, composition of water in strata in faults, and difference in matrix between rocks, all these for the classification and evaluation of fault fracture zones. In the present report, log data from a borehole (1800m deep) drilled to penetrate the Nojima fault (Nojima-Hirabayashi, Awaji island) that emerged during the Great Hanshin-Himeji Earthquake are analyzed in the same way as the above-named Ashio data, and the results are compared with the Ashio results. Immediately below the Nojima-Hirabayashi fault fractured zone, stress is found remarkably reduced and the difference stress quite small in size. This is interpreted as indicating a state in which clay has already developed well in the fault fractured zone ready to allow the occurrence of shear fracture or a state in which such has already occurred for the release of stress. 4 refs., 5 figs.

  6. 3D electrical method and step continuous wave radar method for Nojima site. Results of measurement of resistivity at trench site; Nojima danso ni okeru sanjigenhi teikoho to step shiki renzokuha chika radar ho tansa. Trench chosa chiten deno hiteiko sokutei kekka

    Energy Technology Data Exchange (ETDEWEB)

    Suzuki, K.; Oda, Y.; Tank, K. [Central Research Institute of Electric Power Industry, Tokyo (Japan); Hayashi, H. [Kawasaki Geological Engineering Co. Ltd., Tokyo (Japan); Jomori, A. [Japan Crust Research, Tokyo (Japan)

    1996-05-01

    Several surveys were carried out near the Nojima fault, including three-dimensional resistivity measurement and underground radar survey at the Ogura area, underground radar survey at the Hirabayashi area, and resistivity measurement in the vicinity of the trench at the Nashinomoto area, in order to investigate in detail the underground structures at a depth up to several tens meters from the ground surface. Resistivity was measured by an automatic analyzer capable of simultaneously measuring potential levels at 14 channels which can cover 112 measuring points at the largest. At the Ogura area, the boundary planes of the resistivity structures are continuously detected in the direction of the fault moving during the earthquake period. The underground radar measurement results suggest accumulated displacement of strata at a depth of around 25m in the Osaka Strata and flexible structures. At the Hirabayashi area, the underground radar analysis detects discrete sections in the reflection planes at the fault position, but no reflection planes of high continuity. At the Nashinomoto area, the clay stratum detected in the fault by excavating the trenches are found to be low in resistivity by the resistivity measurement. 4 refs., 11 figs., 2 tabs.

  7. Consideration on characteristics of faults distributed at around Fujigawa river mouth; Fujigawa kako shuhen ni okeru danso kaiseki

    Energy Technology Data Exchange (ETDEWEB)

    Iwashita, A.; Misawa, Y. [Tokai University, Tokyo (Japan)

    1997-10-22

    From the sonic prospecting on the ground, it was confirmed that faults distributed in the inner part of Suruga Bay extend near the Fujigawa river mouth. While, faults in the sea bottom were found by the sonic prospecting using a single air-gun. However, continuity of faults running from the land to the sea has not been reported. This paper describes the continuity of Fujigawa fault system running from the land to the sea around Fujigawa river mouth along the subduction zone of Philippine Sea Plate using single air-gun seismic reflection records. Locations of the faults can be expressed as fracture information of linearment obtained from the satellite remote sensing images, which agreed well with those found by the Active Fault Research Association. As a result of the image processing, they agreed distinctly with the topography of Fujigawa fault system. Thus, much more accurate analysis can be performed by comparing the regional information by the remote sensing with the sonic seismic reflection profiles. 3 refs., 2 figs.

  8. Airborne gamma-ray survey around the Negoro fault. 1; Negoro danso shuhen chiiki ni okeru kuchu {gamma} sen tansa. 1

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    Nakayama, E.; Kasuya, Y.; Hasegawa, H. [Aero Asahi Corp., Tokyo (Japan); Tsukuda, E. [Geological Survey of Japan, Tsukuba (Japan)

    1997-05-27

    An airborne gamma-ray survey was carried out to investigate the active fault system in the central structure line in the peripheral area of the city of Wakayama. At the same time, with an objective to enhance applicability of the airborne gamma-ray survey to active fault investigation, fundamental data were acquired and discussed. The measurement data were processed according to the standard method specified by IAEA. An ID-FFT filter and a nonlinear filter were employed to extract anomalous gamma-ray intensity values. The gamma-ray intensity distribution chart shows a noticeable positive anomalous area extending from the central part of the western edge to the north-east direction. This area agrees nearly well with the Negoro fault, but its peak portion is positioned slightly more to south than the position of the Negoro fault shown in existing data. The Sakuraike fault and the vicinity of the central structure line also show positive anomaly as a whole, particularly remarkably in the vicinity of their converging portion. However, differing from the vicinity of the Negoro fault, the areas are not extracted as an anomalous area which has directionality and extends in a line form. One of the factors for this would be that it is a fault in unsolidified deposits with low opening trend, differing from the one in solidified rocks. 1 fig., 3 tabs.

  9. Radioactivity depth distribution of 500 m borehole samples through the Nojima fault zone in Awaji Island

    International Nuclear Information System (INIS)

    Sakama, M.; Yamashita, S.; Koori, N.; Nakayama, S.; Fushimi, K.; Murata, A.

    2003-01-01

    The movements of the Nojima Fault in the northwest region of the island of Awaji, southwest Japan, were caused by the 17 January 1995 Hanshin-Kobe-Awaji Earthquake. The earthquake epicentered on about 14 km underground point below Akashi Strait (N 34deg 36' and E 135deg 03') and the magnitude was record as Ms=7.2 on the epicenter. Many cities in the Hanshin area and the northern part of Awaji Island were devastated by the earthquake and the death toll reached more than about 6400 people. Immediately after the earthquake, in order to elucidate the displacement on the Nojima fault, three drillings were in 1995 and 1996 carried out at Ogura, Hokudan-cho in Awaji Island by the Disaster Prevention Research Institute, Kyoto University. In the drilling project, two 500 m boreholes in one of them were successfully drilled through the fault zone at a depth of 389.4 m. The 500 m borehole samples were collected in the regions of 0 to 455.3 m and 193.0 to 550.7 m, respectively. They were divided into about 80 core samples on the basis of lithology and the radioactive concentrations of naturally occurring radionuclides included into those core samples were analyzed by a gamma-ray spectrometry. In this work, we report the relationship between the radioactivity depth distribution of naturally occurring radionuclides and the some strata including the fault zone up to the depth of 500 m underground. (author)

  10. Development of direct dating methods of fault gouges: Deep drilling into Nojima Fault, Japan

    Science.gov (United States)

    Miyawaki, M.; Uchida, J. I.; Satsukawa, T.

    2017-12-01

    It is crucial to develop a direct dating method of fault gouges for the assessment of recent fault activity in terms of site evaluation for nuclear power plants. This method would be useful in regions without Late Pleistocene overlying sediments. In order to estimate the age of the latest fault slip event, it is necessary to use fault gouges which have experienced high frictional heating sufficient for age resetting. It is said that frictional heating is higher in deeper depths, because frictional heating generated by fault movement is determined depending on the shear stress. Therefore, we should determine the reliable depth of age resetting, as it is likely that fault gouges from the ground surface have been dated to be older than the actual age of the latest fault movement due to incomplete resetting. In this project, we target the Nojima fault which triggered the 1995 Kobe earthquake in Japan. Samples are collected from various depths (300-1,500m) by trenching and drilling to investigate age resetting conditions and depth using several methods including electron spin resonance (ESR) and optical stimulated luminescence (OSL), which are applicable to ages later than the Late Pleistocene. The preliminary results by the ESR method show approx. 1.1 Ma1) at the ground surface and 0.15-0.28 Ma2) at 388 m depth, respectively. These results indicate that samples from deeper depths preserve a younger age. In contrast, the OSL method dated approx. 2,200 yr1) at the ground surface. Although further consideration is still needed as there is a large margin of error, this result indicates that the age resetting depth of OSL is relatively shallow due to the high thermosensitivity of OSL compare to ESR. In the future, we plan to carry out further investigation for dating fault gouges from various depths up to approx. 1,500 m to verify the use of these direct dating methods.1) Kyoto University, 2017. FY27 Commissioned for the disaster presentation on nuclear facilities (Drilling

  11. Sealing process with calcite in the Nojima active fault zone revealed from isotope analysis of calcite

    International Nuclear Information System (INIS)

    Arai, Takashi; Tsukahara, Hiroaki; Morikiyo, Toshiro

    2003-01-01

    The Nojima fault appeared on the surface in the northern part of Awaji Island, central Japan as a result of the Hyogo-ken Nanbu earthquake (1995, M=7.2). Active fault drilling was performed by the Disaster Prevention Research Institute (DPRI), Kyoto University, and core samples were retrieved from 1410 to 1710 m, which were composed of intact and fractured granodiorites. We obtained calcite samples and gas samples from the vein in marginal fracture and non-fracture zones. We analyzed the carbon and oxygen isotope ratios of calcite and carbon dioxide to investigate the characteristic isotope ratios of fluids in the active fault zone, to estimate the origins of fluids, and to determine the sealing process of fractures. The analyzed values of carbon and oxygen isotope ratios of calcite were -10.3 to -7.2 per mille, 18 to 23 per mille, respectively, and carbon isotope ratios of CO 2 were -21 to -17 per mille. If carbon isotope ratios of calcite were at equilibrium with those of CO 2 , the precipitation temperature of calcite is calculated to be 30 to 50 deg C. This temperature is consistent with the present temperature of the depth where drilling cores were retrieved. Oxygen isotope ratios of H 2 O that, precipitated calcite were calculated to be -1.8 to -5.5 per mille. These values indicate calcite were precipitated from mixed fluids of sea water and meteoric water. Therefore, the marginal fracture zone of the Nojima fault was sealed with calcite, which was generated from mixing of sea water and meteoric water in situ. (author)

  12. Thermoluminescence of quartz collected from Nojima Fault Trench excavated in 2015

    Science.gov (United States)

    Hasebe, N.; Miura, K.; Ganzawa, Y.; Tagami, T.; Lin, A.

    2017-12-01

    The Southern Hyogo prefecture earthquake occurred in 1995, which is known as Kobe Earthquake or Great Hanshin-Awaji Earthquake, was caused by the activity of the Nojima fault. The research project on the Nojima fault is currently going on and new trench was excavated in 2015. We investigate the effect of fault activity on surrounding rocks by thermoluminescence (TL) dating method. First, quartz were extracted from samples collected from the trench wall with different distance from the fault. A block of nearby basement rock is also collected and analyzed. Next, the luminescence sites and their emission temperatures were determined by T-Tmax method (McKeever, 1980) perfomed by 10 ° C interval for selected samples (the basement rock collected from Rokko granite, the granite sample collected about 5 m away from the fault in the trench, and the gouge sample adjacent to the fault). As a result, the peak emission temperatures were 200-220 ° C, 270 ° C and 320-350 ° C for granite quartz. These values were concordant for UV-TL and Blue TL. The activation energy and frequency factors were determined for signals emitted at different temperatures by peak shift methods (Aitken, 1985). On the other hand, the TL emission curves for the sample adjacent to the fault do not show discrete luminescence sites, different from granite samples. Natural TL emission show variety of TL profile. The accumulated doses of each sample were estimated for identified signal peaks after peak separation. Signals from different peak temperatures show different dose values in all the samples. The dose estimated by signals at 200 ° showed the minimum value for all samples. The same sample show different accumulated dose for Blue TL and UV-TL. The variety of accumulated doses in a sample may be reflective of complex thermal history of samples, and/or partly caused by the ineffective peak separation. Even the host rock collected away from the fault show a low accumulated dose in 200°C singnal, far

  13. Subsurface structure of the Nojima fault from dipole shear velocity/anisotropy and borehole Stoneley wave

    Energy Technology Data Exchange (ETDEWEB)

    Ito, H. [Geological Survey of Japan, Tsukuba (Japan); Yamamoto, H.; Brie, A.

    1996-10-01

    Fracture and permeability in the fault zone of the active fault drilling at the Nojima fault were evaluated from acoustic waveforms. There were several permeable intervals in the fault zone. There was strong Stoneley wave attenuation, very large S-Se below the fault and in the interval above the fault. In the fault zone, there were also several short intervals where S-Se was very large; 667 m-674 m and 706 m-710 m. In these intervals, the Stoneley attenuation was large, but there was no Stoneley reflection from within the interval. Reflections were observed at the upper and lower boundaries, going away from the bed up above, and down below. In this well, the shear wave was very strongly attenuated at and below the fault zone. The fast shear azimuth changed at the fault. The slowness anisotropy was fairly strong above the fault from 602 m to 612 m, but smaller below the fault. The changes in fast shear azimuth were much more pronounced near the fault, which suggested a strong influence of the fault. 6 refs., 5 figs.

  14. Fracture structures of active Nojima fault, Japan, revealed by borehole televiewer imaging

    Science.gov (United States)

    Nishiwaki, T.; Lin, A.

    2017-12-01

    Most large intraplate earthquakes occur as slip on mature active faults, any investigation of the seismic faulting process and assessment of seismic hazards require an understanding of the nature of active fault damage zones as seismogenic source. In this study, we focus on the fracture structures of the Nojima Fault (NF) that triggered the 1995 Kobe Mw 7.2 earthquake using ultrasonic borehole televiewer (BHTV) images from a borehole wall. The borehole used in this study was drilled throughout the NF at 1000 m in depth by a science project of Drilling into Fault Damage Zone(DFDZ) in 2016 (Lin, 2016; Miyawaki et al., 2016). In the depth of consolidated sandstone and conglomerate of the Plio-Pleistocene Osaka-Group and mudstone and sandstone of the Miocene Kobe Group. The basement rock in the depth of >230 m consist of pre-Neogene granitic rock. Based on the observations of cores and analysis of the BHTV images, the main fault plane was identified at a depth of 529.3 m with a 15 cm thick fault gouge zone and a damage zone of 100 m wide developed in the both sides of the main fault plane. Analysis of the BHTV images shows that the fractures are concentrated in two groups: N45°E (Group-1), parallel to the general trend of the NF, and another strikes N70°E (Group-2), oblique to the fault with an angle of 20°. It is well known that Riedel shear structures are common within strike-slip fault zones. Previous studies show that the NF is a right-lateral strike-slip fault with a minor thrust component, and that the fault damage zone is characterized by Riedel shear structures dominated by Y shears (main faults), R shears and P foliations (Lin, 2001). We interpret that the fractures of Group (1) correspond to Y Riedel fault shears, and those of Group (2) are R shears. Such Riedel shear structures indicate that the NF is a right-lateral strike-slip fault which is activated under a regional stress field oriented to the direction close to east-west, coincident with that

  15. Characterization of earthquake fault by borehole experiments; Koseinai sokutei ni yoru jishin danso no kenshutsu

    Energy Technology Data Exchange (ETDEWEB)

    Ito, H.; Miyazaki, T.; Nishizawa, O.; Kuwahara, Y.; Kiguchi, T. [Geological Survey of Japan, Tsukuba (Japan)

    1996-05-01

    A borehole was excavated to penetrate the Nojima fault at the Hirabayashi area, to investigate the underground structures of the fault by observation of the cores and well logging. The borehole was excavated from 74.6m east of the fault surface. Soil is of granodiorite from the surface, and fault clay at a depth in a range from 624.1 to 625.1m. Observation of the cores, collected almost continuously, indicates that the fault fracture zone expands in a depth range from 557 to 713.05m. The well logging experiments are natural potential, resistivity, density, gamma ray, neutron, borehole diameter, microresistivity and temperature. They are also for DSI- and FMI-observation, after expansion of the borehole. The well logging results indicate that resistivity, density and elastic wave velocity decrease as distance from fault clay increases, which well corresponds to the soil conditions. The BHTV and FMI analyses clearly detect the fault clay demarcations, and show that elastic wave velocity and BHTV results differ at above and below the fault. 3 refs., 3 figs.

  16. Preliminaries on core image analysis using fault drilling samples; Core image kaiseki kotohajime (danso kussaku core kaisekirei)

    Energy Technology Data Exchange (ETDEWEB)

    Miyazaki, T.; Ito, H. [Geological Survey of Japan, Tsukuba (Japan)

    1996-05-01

    This paper introduces examples of image data analysis on fault drilling samples. The paper describes the following matters: core samples used in the analysis are those obtained from wells drilled piercing the Nojima fault which has moved in the Hygoken-Nanbu Earthquake; the CORESCAN system made by DMT Corporation, Germany, used in acquiring the image data consists of a CCD camera, a light source and core rotation mechanism, and a personal computer, its resolution being about 5 pixels/mm in both axial and circumferential directions, and 24-bit full color; with respect to the opening fractures in core samples collected by using a constant azimuth coring, it was possible to derive values of the opening width, inclination angle, and travel from the image data by using a commercially available software for the personal computer; and comparison of this core image with the BHTV record and the hydrophone VSP record (travel and inclination obtained from the BHTV record agree well with those obtained from the core image). 4 refs., 4 figs.

  17. Structural analysis of cataclastic rock of active fault damage zones: An example from Nojima and Arima-Takatsuki fault zones (SW Japan)

    Science.gov (United States)

    Satsukawa, T.; Lin, A.

    2016-12-01

    Most of the large intraplate earthquakes which occur as slip on mature active faults induce serious damages, in spite of their relatively small magnitudes comparing to subduction-zone earthquakes. After 1995 Kobe Mw7.2 earthquake, a number of studies have been done to understand the structure, physical properties and dynamic phenomenon of active faults. However, the deformation mechanics and related earthquake generating mechanism in the intraplate active fault zone are still poorly understood. The detailed, multi-scalar structural analysis of faults and of fault rocks has to be the starting point for reconstructing the complex framework of brittle deformation. Here, we present two examples of active fault damage zones: Nojima fault and Arima-Takatsuki active fault zone in the southwest Japan. We perform field investigations, combined with meso-and micro-structural analyses of fault-related rocks, which provide the important information in reconstructing the long-term seismic faulting behavior and tectonic environment. Our study shows that in both sites, damage zone is observed in over 10m, which is composed by the host rocks, foliated and non-foliated cataclasites, fault gouge and fault breccia. The slickenside striations in Asano fault, the splay fault of Nojima fault, indicate a dextral movement sense with some normal components. Whereas, those of Arima-Takatsuki active fault shows a dextral strike-slip fault with minor vertical component. Fault gouges consist of brown-gray matrix of fine grains and composed by several layers from few millimeters to a few decimeters. It implies that slip is repeated during millions of years, as the high concentration and physical interconnectivity of fine-grained minerals in brittle fault rocks produce the fault's intrinsic weakness in the crust. Therefore, faults rarely express only on single, discrete deformation episode, but are the cumulative result of several superimposed slip events.

  18. Non-destructive testing of building materials | Danso | Journal of ...

    African Journals Online (AJOL)

    Journal of Applied Science and Technology. Journal Home · ABOUT THIS JOURNAL · Advanced Search · Current Issue · Archives · Journal Home > Vol 1, No 1 (1996) >. Log in or Register to get access to full text downloads.

  19. Subsurface displacement of the Tachikawa fault; Tachikawa danso no chika shinbu ni okeru danso hen`i

    Energy Technology Data Exchange (ETDEWEB)

    Yamaguchi, K.; Kano, N.; Kiguchi, T.; Tanaka, A. [Geological Survey of Japan, Tsukuba (Japan); Sato, H. [The University of Tokyo, Tokyo (Japan). Earthquake Research Institute

    1997-10-22

    Seismic exploration using the reflection method was carried out at the central section of the Tachikawa fault located in the western part of the Musashino high plain spreading over Tokyo and Saitama Prefectures. The course of traverse was set on a road running in the east to west direction, which crosses the running direction of the Tachikawa fault in Sunagawa, Tachikawa City by about 65 degrees. The area near the course of traverse is a terraced alluvial fan, with the nature of its surface soil consisted of a gravelly bed of the Quaternary period. In order to identify the fault structure in detail, the focal point interval was set to 5 m, being half of the vibration receiving point interval of 10 m. The CMP was defined at a 2.5-m interval rather than a 5-m interval. The S/N ratio of the derived data was found not good. This is because of scattering of seismic energy into the gravelly bed with a thickness of about 100m in the shallow portion and because of noise from passing vehicles. The data processing was applied with correlation, geometry, static correction, velocity analysis and CMP polymerization to have prepared a preliminary CMP polymerization time cross section. As a result, it was elucidated that the Tachikawa fault forms a bend zone or a crush zone under the ground, and continues down to a great depth at a high angle. 9 refs., 3 figs.

  20. Achievement report for fiscal 1998. Optical tomographic system; 1998 nendo seika hokokusho. Hikari danso imaging system

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    1999-05-01

    Evaluations were given on spatial resolution and measurement time of an optical tomographic system by using the developed 64-channel time-resolved spectroscopy and an image reconstruction algorithm. With respect to the spatial resolution, the target value of 1 cm was verified from tomographic images of a phantom with a diameter of 10cm, simulating a neonate. The measurement time achieved 20 minutes, being one third of the target value. In installing the equipment at Hokkaido University, speeds of the optical switches and attenuators were increased to have reduced the measurement time to one minute. For installation at Kanagawa Rehabilitation Center, development has been made on a nano-second light pulser, whose average beam quantity has been increased to 40 times, and improvement has been given on the optical switches, the attenuators, and the indication software, by which the measurement time was decreased further by 30 seconds than that at Hokkaido University. In performing the clinical evaluation, the evaluation protocol resolved by the Experiment Evaluation Special Committee was submitted for deliberation at the Medical Welfare Device Clinical Evaluation Committee. Upon having been authorized by the Committee, the clinical evaluations were performed at Hokkaido University and the Kanagawa Rehabilitation Center. (NEDO)

  1. Faults survey by 3D reflection seismics; Sanjigen hanshaho jishin tansa ni yoru danso chosa

    Energy Technology Data Exchange (ETDEWEB)

    Tsuchiya, T.; Ejiri, T.; Yamada, N.; Narita, N.; Aso, H.; Takano, H.; Matsumura, M. [Dia Consultants Company, Tokyo (Japan)

    1996-10-01

    This paper describes fault survey by 3D seismic reflection exploration. Survey has been conducted mainly at flat land area without pavement not in urban area in Japan. Subsurface structure is complicated with intersecting multiple faults. In this area, a lot of geological investigations have been done prior to the seismic reflection exploration. Fairly certain images of faults have been obtained. However, there were still unknown structures. Survey was conducted at an area of 170m{times}280m in the CDP range. Measurements were carried out by using 100 g of dynamite per seismic generation point combined with 40 Hz velocity geophones. Fixed distribution consisting of lattice points of 12{times}12 was adopted as an observation method. In and around the lattice, a great number of explosions were carried out. The CDP stacking method and the method of migration after stacking were used for the data processing. The 3D structures of six horizons and five faults could be interpreted. Interpreted horizons were well agreed with the logging results. 3 figs.

  2. Array TDEM survey at the Yufuin fault; Yufuin danso ni okeru array shiki TDEM tansa

    Energy Technology Data Exchange (ETDEWEB)

    Mogi, T. [Kyushu University, Fukuoka (Japan). Faculty of Engineering; Tanaka, Y.; Fukuda, Y. [Kyoto University, Kyoto (Japan). Faculty of Science; Jomori, N. [Chiba Electric Research Institute Co., Chiba (Japan)

    1996-10-01

    The array arrangement of receivers was studied to improve the resolution of LOTEM (long offset transient electromagnetics) survey. To eliminate the effect of underground structure from a source to a receiving point, continuous array arrangement from a source site is desirable. The survey at the Yufuin fault was carried out by arranging TEM receivers at intervals of 100m from the source. Since the synchronization between transmitting and receiving points by high-precision clock is essential, an amplifier for a flux gate magnetometer capable of measuring at four points at the same time was used. In the south plateau of the Yufuin basin, a relatively high resistivity stratum more than several tens ohm m exists at depth less than several hundreds meter, and a low resistivity stratum less than 10 ohm m exists under that. Those boundary depth increases toward the north up to 950m, and the depth subsequently decreases toward the north until the low resistivity stratum disappears. In addition, the uniform stratum of 1000m deep continues toward the north. Such precise resistivity structure around the fault was obtained by dense arrangement of measuring points. 4 refs., 7 figs.

  3. Fault structure analysis by means of large deformation simulator; Daihenkei simulator ni yoru danso kozo kaiseki

    Energy Technology Data Exchange (ETDEWEB)

    Murakami, Y.; Shi, B. [Geological Survey of Japan, Tsukuba (Japan); Matsushima, J. [The University of Tokyo, Tokyo (Japan). Faculty of Engineering

    1997-05-27

    Large deformation of the crust is generated by relatively large displacement of the mediums on both sides along a fault. In the conventional finite element method, faults are dealt with by special elements which are called joint elements, but joint elements, elements microscopic in width, generate numerical instability if large shear displacement is given. Therefore, by introducing the master slave (MO) method used for contact analysis in the metal processing field, developed was a large deformation simulator for analyzing diastrophism including large displacement along the fault. Analysis examples were shown in case the upper basement and lower basement were relatively dislocated with the fault as a boundary. The bottom surface and right end boundary of the lower basement are fixed boundaries. The left end boundary of the lower basement is fixed, and to the left end boundary of the upper basement, the horizontal speed, 3{times}10{sup -7}m/s, was given. In accordance with the horizontal movement of the upper basement, the boundary surface largely deformed. Stress is almost at right angles at the boundary surface. As to the analysis of faults by the MO method, it has been used for a single simple fault, but should be spread to lots of faults in the future. 13 refs., 2 figs.

  4. Research and development of peripheral technology for photovoltaic power systems. Development of inverter technology for photovoltaic (PV) system which is connected to the utility grid; Shuhen gijutsu no kenkyu kaihatsu. Fukusu kino tan`itsuka shuhen sochi no kenkyu kaihatsu

    Energy Technology Data Exchange (ETDEWEB)

    Tatsuta, M. [New Energy and Industrial Technology Development Organization, Tokyo (Japan)

    1994-12-01

    This paper reports the study results on development of integrated multifunctional peripheral equipment in fiscal 1994. (1) On development of inverters with no transformer, the following study results were obtained. Converter efficiency reached the target of 95.0% by using an improved general purpose IGBT as switching element of main circuit. Distortion factor of output current harmonics achieved 5% in total current distortion factor, and less than 3% in each order harmonic current one. In control of the DC part of output current, the target less than 0.3% was achieved by inserting a capacitor into detection signal circuit and by detection/correction control of current detector offset. Detection level of 100mA was achieved for DC grounding detection by installing a DC grounding detector in the DC input side of inverters. VCCI 1 level was also achieved for EMI measurement. (2) On development of integrated multifunctional peripheral equipment, evaluation test of the prototype equipment of 0.025m{sup 3} in volume and 17kg in mass was carried out. 3 figs., 1 tab.

  5. Fault analysis in the very shallow seismic reflection method. Part 3. Migration; Gokusenso hanshaho ni okeru danso kaiseki. 3. Migration

    Energy Technology Data Exchange (ETDEWEB)

    Nagumo, S.; Muraoka, S.; Takahashi, T. [OYO Corp., Tokyo (Japan)

    1997-10-22

    Concerning the analysis of data obtained by the seismic reflection method, migration in the very shallow layer is discussed. When the dip angle of the reflection plane involved is disclosed by DMO conversion, the amount of migration (travelling sideways) can be calculated by use of simple geometrical formulas though on the presumption that the sector velocity is constant. Categorized into this technique are such methods as DMO conversion migration, direct dip migration, F-K method, and finite difference method. This means that waveforms are not damaged by migration processing although elongation occurs due to time base conversion. When it is taken into account that waveform distortion is generally grave in the migration related methods widely in use, this feature has to be said valuable in holding information on faults. This is especially advantageous in the very shallow layer because the amount of migration is proportionally larger when the level is deeper and, in addition, migration processing is useful when it is necessary to know more accurately the character of the fault plane. 8 figs.

  6. Seismic reflection survey of the Uemachi fault in Osaka Prefecture; Osaka Uemachi danso no hanshaho danseiha tansa

    Energy Technology Data Exchange (ETDEWEB)

    Sugiyama, Y. [Geological Survey of Japan, Tsukuba (Japan); Yoshizawa, M.; Hirooka, S. [Nikko Exploration and Development Co. Ltd., Tokyo (Japan); Yokota, H.; Ito, S. [Hanshin Consultant Co., Osaka (Japan); Hayashi, K.; Aizawa, H.

    1997-05-27

    Reflection survey is conducted using three traverse lines in Sakai City for confirming the presence of a southward stretch of the Uemachi fault underground along the western periphery of the Uemachi terrace, Osaka, and for elucidating its connection to the Sakamoto fault distributed near Izumi. Another reflection survey is conducted in the bed of Kanzaki river, Osaka, for the confirmation of its connection to the Nembutsuji-zan fault in Senri hillock. It is estimated on the basis of boring data that there exists another flexural structure approximately 3km south of the flexural structure whose presence is confirmed by the Sakai second traverse line. Accordingly, possibilities are high that the southward stretch of the Uemachi fault connects to the Sakamoto fault. The confirmation by the Kanzaki river traverse line of the flexural structure again confirms the continuity between the Uemachi fault and Nembutsuji-zan fault. The above-said findings enable an inference that the three faults of Nembutsuji-zan, Uemachi, and Sakamoto constitute a chain of active faults. Furthermore, there exists an active fault to the south of the Sakamoto fault, which zigzags to the south on the right-hand side as far as the south of the Kumeda pond. Accordingly, the Uemachi fault system as a whole spans approximately 43km from the northern end of the Nembutsuji-zan fault as far as the south of the Kumeda pond. 5 refs., 6 figs.

  7. Application of vector CSAMT for the imaging of an active fault; CSAMT ho ni yoru danso no imaging

    Energy Technology Data Exchange (ETDEWEB)

    Kobayashi, T.; Fukuoka, K. [Oyo Corp., Tokyo (Japan)

    1997-05-27

    With an objective to identify three-dimensionally resistivity in deep fault in the Mizunawa fault in Fukuoka Prefecture, a measurement was carried out by using the CSAMT method. The measurement was conducted by arranging seven traverse lines, each line having observation points installed at intervals of about 500 m. Among the 68 observation points in total, 33 points performed the vector measurement, and the remaining points the scaler measurement. For observation points having performed the vector measurement, polarized wave eclipses were depicted in the electric field to discuss which direction the current will prevail in. For analyses, a one-dimensional analysis was performed by using an inversion with smoothing restriction, and a two-dimensional analysis was conducted by using the finite element method based on the result of the former analysis. The vector measurement revealed that the structure in the vicinity of a fault was estimated to have become complex, and the two-dimensional analysis discovered that the Mizunawa fault is located on a relatively clear resistivity boundary. In addition, it was made clear that the high resistivity band may even be divided into two regions of about 200 ohm-m and about 1000 ohm-m. 2 refs., 7 figs.

  8. Fault analysis in the very shallow seismic reflection method. 2; Gokusenso hanshaho ni okeru danso kaiseki. 2

    Energy Technology Data Exchange (ETDEWEB)

    Nagumo, S.; Muraoka, S.; Takahashi, T. [Oyo Corp., Tokyo (Japan)

    1997-05-27

    Fault analysis is required in addition to the ordinary process of structural analysis (CDP stacking) for the examination of discontinuity in the reflection horizon in question. The fault shape restoration principle is that the reflection point of a reflection wave observed at a certain receiving point is on an ellipse with the shock point and receiving point at its focal points and that the sum of the distances between the reflection point and the focal points is equal to the reflection wave propagation time. The DMO velocity is worked out by calculation using the positive travel time and inverse travel time from the common reflection surface. When the reflection surface is inclined by {theta}, the average interval velocity/cos{theta} is called the DMO velocity. When the reflection surface inclination and the average interval velocities are determined separately in this way, the position of the reflection point may be worked out, and this enables the calculation of the amount of migration (lateral movement). The reflection wave lineups carried by the original record are picked up one by one, and the average interval velocities are treated very prudently. After such a basic DMO conversion treatment, the actualities of the fault are described fairly correctly. 3 figs.

  9. The effect of technological changes on unemployment in the beverage sector of the South African economy / A.K. Danso

    OpenAIRE

    Danso, Alex Kwame

    2007-01-01

    The ability of the South African economy to absorb labour has been declining since the 1960's, with the manufacturing sector employment declining since 1990. The decline in manufacturing jobs flies in the face of increased output of the sector. This trend is attributed to the application of technology and sophisticated equipments in the manufacturing process leading to a loss of jobs, particularly for unskilled labour. Unemployment in South Africa has become one of the biggest ...

  10. Fault analysis in the very shallow seismic reflection method; Gokusenso jishin hanshaho ni okeru danso kaiseki. 1

    Energy Technology Data Exchange (ETDEWEB)

    Nagumo, S.; Muraoka, S.; Kaida, Y.; Takahashi, T. [OYO Corp., Tokyo (Japan)

    1996-10-01

    To effectively use the very shallow seismic reflection for active fault survey, a method has been investigated by which fault structures can be appropriately reconstructed from the fault information detected in the original records. The first step of reconstructing the fault system from the travel time reflection curve was to grasp an outline of fault structure from the patterns of travel time curve observed in the original record. For the very shallow seismic reflection method, especially, the low velocity layers in a shallow part succeeding from the ground surface made the issue complicated. Then, the travel time reflection curves were calculated in the case of existing several horizontal reflection surfaces in the surface layer. The constant values, mean velocities to the depth at individual reflection surfaces were used for the approximation of velocities. The outline of fault structure was grasped from the observation of original record. Then, the structure was reconstructed from the travel time curves. When the mean velocity in the medium was known, reconstruction of the feature of reflection surfaces from the travel time curves could be determined by simple mapping. When the mean velocity was unknown, it was calculated using the reciprocal travel time from the common reflection surface for individual reflection surfaces. 7 figs.

  11. Agrosearch - Vol 13, No 2 (2013)

    African Journals Online (AJOL)

    Reactions of some Confectionery Groundnut Accessions to Plant Parasitic Nematodes Infection · EMAIL FREE FULL TEXT EMAIL FREE FULL TEXT · DOWNLOAD FULL TEXT DOWNLOAD FULL TEXT. K Osei, JY Asibuo, JY Asibuo, A Agyeman, A Agyeman, P Osei-Bonsu, P Osei-Bonsu, Y Danso, Y Danso, J Adomako, ...

  12. Browse Title Index

    African Journals Online (AJOL)

    Items 151 - 200 of 217 ... Vol 13, No 2 (2013), Reactions of some Confectionery Groundnut Accessions to Plant Parasitic Nematodes Infection, Abstract PDF. K Osei, JY Asibuo, JY Asibuo, A Agyeman, A Agyeman, P Osei-Bonsu, P Osei-Bonsu, Y Danso, Y Danso, J Adomako, J Adomako. Vol 1, No 2 (1995), Real price and the ...

  13. Geoelectric study in attempt to detect of deformation around slice gate in the embankment; Hiteiko eizoho wo mochiita himon shuhen no yurumi ryoiki no suitei

    Energy Technology Data Exchange (ETDEWEB)

    Natori, T.; Nakayama, Y. [Hokkaido Sapporo Public Works Office, Sapporo (Japan); Hashimoto, Y.; Matsuo, J. [OYO Corp., Tokyo (Japan)

    1997-10-22

    For the river structures, such as slice gates and slice pipes, constructed on the weak ground, structures often come out due to forced settlement of embankment, which results in the formation of cavity and loose ground. These deformations can cause disasters due to leakage by water channel and fracture of bank. It is significant to detect and grasp these situations in early stage. In this study, resistivity imaging was conducted around slice gate in several times, to estimate the loose region based on the difference in the obtained resistivity data. Resistivity was measured in two times with a certain interval using the same line. The loose region around the slice gate was estimated from the change of saturation condition and the saturation line by considering the difference. Even in the case when judgment was hard by a single measurement, it was possible to estimate the loose region based on the difference from multiple measurements. 3 refs., 6 figs.

  14. On the sea-covering effect of a huge floating structure on the surrounding water; Choogata futai shuhen no kaisui ni taisuru kaimen shahei no eikyo ni tsuite

    Energy Technology Data Exchange (ETDEWEB)

    Fujino, M.; Kagemoto, H.; Hamada, T. [The University of Tokyo, Tokyo (Japan)

    1996-12-31

    The numerical analysis program based on the difference method for dynamics of sea water with sea-surface displacement, flow rate, salt content and temperature as the parameters is modified to more accurately assess the effects of a huge marine structure on surrounding environment by adding the effects of insolation and boundary conditions of the sea-covering effects of the floating structure. The numerical simulation was done for summer and winter seasons, not in a sea area but using a rectangular bay with the floating structure at the center. A new flow evolves around the floating structure, due to the sea-covering effect. The flow patterns in summer and winter are clearly different, due to difference in insolation. The predicted flow is also sensitive whether stratification is considered or not, by which is meant that it is important what stratification effect is taken into account. Daily insolation changes are accompanied by vertical distribution of water temperature and its temporal change. These effects are also observed under the floating structure which shields insolation. 10 refs., 17 figs., 4 tabs.

  15. Achievement report on research and development of medical and welfare equipment technology. Optical tomographic imaging method; Iryo fukushi kiki gijutsu kenkyu kaihatsu seika hokokusho. Hikari danso imaging system

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    1999-11-01

    The aim is to develop a method of processing oxygen concentration distribution in human organs into an image by computed tomography using near infrared rays capable of transmitting through living tissues. Since the photoabsorption spectra of hemoglobin etc. in blood vary according to the degree of their oxidation, an oxygen concentration level is determined by measuring the magnitude of the variation. In the imaging method named in the title, the object is irradiated with picosecond-level near infrared pulses from all directions successively, the pulses after transmission through the object are measured at all directions at a picosecond-level time resolution, and the distribution of pulse scattering and absorption characteristics are subjected to algorithmic calculation, the outcome is converted into oxygen concentration levels, and an image is obtained. A 64-channel time resolution measurement system is constructed, and is applied to living tissue models (phantoms) and animals, and an image is obtained and evaluated. On the basis of the result, a patient is examined for clinical evaluation, and an image reflecting the distribution of variations in hemoglobin oxygen concentration is obtained for the head of the adult patient. A spatial resolution of 1cm is achieved in case of a phantom 10cm in diameter. In the case of 64 channels, measurement takes approximately 20 minutes and mapping image data measurement takes approximately 7 minutes. (NEDO)

  16. Simulation of fault-bend fold by incompressible Newtonian fluid; Hiasshukusei Newton ryutai ni yoru danso oremagari shukyoku kozo no simulation

    Energy Technology Data Exchange (ETDEWEB)

    Tamagawa, T.; Matsuoka, T. [Japan Petroleum Exploration Corp., Tokyo (Japan); Tsukui, R. [Japan National Oil Corp., Tokyo (Japan). Technology Research Center

    1997-10-22

    Incompressible Newtonian fluid simulation is experimentally applied to faults typical of the compression and extension fields. A fault-bend folding structure of the flat-ramp flat fault in the compression field and a folding structure of a normal fault in the extension field are studied, and the results are compared with those obtained by the balanced cross section method. The result of calculation indicates that the velocity gradient with the ramp angle set at 30deg is correspondent to stress and that stress concentration is taking place at the ramp section of the fault. This solution is an approximation and does not necessary support the conservation of area but, when the ramp angle is allowed to change from 10 through 40deg, it is found that the conservation of area holds though roughly. It is found that the configuration of the folding structure formed by a flat-ramp flat fault is positioned between the anomalous-mode layer parallel shear typical of a balanced cross section and the folding structure formed by a vertical shear. 7 refs., 7 figs.

  17. {Gamma}-ray prospecting of major faults of Miocene basins; Chushinto taisekibon no keisei ni kakawaru danso wo taisho to shita hoshano tansa

    Energy Technology Data Exchange (ETDEWEB)

    Iwata, A. [Shimada Technical Consultants, Ltd., Shimane (Japan); Yamauchi, S.; Adachi, K. [Shimane University, Shimane (Japan); Yoon, S.; Kil, R, [Pusan National University, Pusan (Korea, Republic of)

    1997-05-27

    The Masuda basin in the western edge of Shimane Prefecture and the Pohang basin in the southern part of the east cost of Korea had been formed in the middle of Miocene epoch of Neogene period, and show similarity in their geology and structure. A gamma-ray prospecting was carried out on major faults that have had been involved in forming these basins. A portable gamma-ray analysis device, model 8630 made by Clearpulse Corporation was used for the measurement. Emanation of radon and its migration are known generally, whereas rise in radon is recognized above crevices with deep opening trend. The present faults having been involved in forming the basins are thought to have large falls in positive faults and often accompany crevices with opening trend. This estimation is thought endorsed by the result of the present prospecting. In addition, such faults may often form geological boundaries, and the present survey has had geological division made easily with total gamma-ray. A gamma-ray exploration using both of the spectrum method and the total count method is a process sufficiently utilizable in geological surveys on structures in peripheries of sedimentary basins. 6 refs., 7 figs.

  18. Fault detection by Turam TEM survey. Numerical model studies and a case history; TEM ho Turam sokutei haichi ni yoru danso kenshutsu no kokoromi. Model keisan to jisshirei

    Energy Technology Data Exchange (ETDEWEB)

    Wada, K.; Tsutsui, T. [Mitsui Mineral Development Engineering Co. Ltd., Tokyo (Japan); Ito, T. [Chiba Univ., Chiba (Japan). Faculty of Science; Takeuchi, A. [Toyama University, Toyama (Japan). Faculty of Science; He, P. [Power Reactor and Nuclear fuel Development Corp., Tokyo (Japan)

    1997-05-27

    With an objective to detect faults estimated to exist along the Shigesumi valley in the Kamioka mine, discussions were given by using electromagnetic survey, which uses the Turam measurement arrangement based on the TEM method, and three-dimensional model calculations. The Turam measurement arrangement, which installs transmission loop fixedly, is used to identify nature and distribution of electrically conductive objects upon noticing abnormal portions in magnetic fields in the measurement data. In the model calculation, the plate model calculation method and the FDTD method were used, and so was the calculation code TEM3DL. The result revealed that strong topographical influence is seen from steep V-shaped valley existing along the traverse line in the measurement data, but an abnormal resistivity band accompanying remarkable distortion in the curve was detected. According to the result of the model calculation, anomaly detection may be found difficult in locations where a low resistivity band has not grown enough locally. It was possible from these facts to assume a model in which the low resistivity band exists directly below the Shigesumi valley, suggesting existence of faults. 2 refs., 8 figs.

  19. Results of geophysical survey on Hanaore-fault in the Kyoto urban area; Butsuri tansa ni yoru Kyoto shigaichi ni okeru Hanaore danso chosa

    Energy Technology Data Exchange (ETDEWEB)

    Yoshioka, T. [Geological Survey of Japan, Tsukuba (Japan); Echigo, T. [Osaka Soil Test, Osaka (Japan); Toshioka, T.; Matsubara, Y. [Oyo Corp., Tokyo (Japan)

    1997-05-27

    This paper reports results of gravity survey and seismic survey using the shallow bed reflection method to identify distribution of the Hanaore fault in the Kyoto urban area. In the gravity survey, level differential structure caused by the fault was identified as an abrupt change in Bouger anomalous values. The continuity therefrom made the estimation possible on existence and positions of such faults as the Hanaore fault belonging to the Hanaore fault system, the Shishigaya fault, the Kaguraoka fault, and the Okazaki fault. The estimation as a result of the gravity survey include the following findings: the Hanaore fault runs from south of the Yoshidayama in the south-north direction; the distribution of the Okazaki fault has a level differential structure falling on the east side; the structure shows low Bouger anomaly distribution; and this area forms a rift valley belt. In the seismic survey using the shallow bed reflection method, no distinct reflection plane considered as the basement was verified because of influence from urban area noise. However, it was possible to estimate such an underground structure as a monoclinal fold from shapes of the reflection plane and the distribution depths. 7 refs., 5 figs.

  20. Extension of the Fukaya fault and deep structure of the Konan terrace; Fukaya danso no encho to Konan daichi no chika kozo

    Energy Technology Data Exchange (ETDEWEB)

    Yamaguchi, K.; Kano, N.; Yokokura, T.; Kiguchi, T.; Yokota, T.; Tanaka, A. [Geological Survey of Japan, Tsukuba (Japan); Sato, H. [The University of Tokyo, Tokyo (Japan). Earthquake Research Institute

    1997-10-22

    With an objective to elucidate the relationship between the central tectonic line in the Kanto area and the active faults appearing in topography, seismic exploration using the reflection method has been carried out. The course of traverse was set in the south west to north east direction starting from the north east part of the Kanto mountainous area to the Menuma lowland passing through the Konan high plain. The line crosses nearly perpendicularly the direction in which the general beds in this area run. A 400-kg weight was used as a vibration source in the western half of the course of travel, and the MinivibT15000 (made by IVI Corporation) in the eastern half. Considerations given based on the preliminary CMP polymerization time cross section may be summarized as follows: the Fukaya fault cannot be tracked topographically further to the south east side than Mikejiri in Kumagaya City, but the reflection face from CMP 2050 to about 2100 shows an inclined bed on the south west side and a horizontal bed on the north east side; judging from change in the inclination in the beds, the Fukaya fault is thought to extend to the south east direction; the location of inclination change on the cross section turns to the south west side as the depth increases; and, if this is regarded as the fault face, the Fukaya fault could be said an inverse fault. 5 refs., 2 figs.

  1. Acoustic surveys of the southern extension of the Tomikawa fault off Kamiiso in Hakodate bay, southwest Hokkaido; Hakodatewan Kamiisooki ni okeru Tomikawa danso enchobu no onpa tansa

    Energy Technology Data Exchange (ETDEWEB)

    Uchida, Y.; Sagayama, T.; Osawa, M.; Hamada, S.; Suga, [Hokkaido Geological Survey, Sapporo (Japan)

    1997-10-22

    With an objective to identify extension into sea area of the Tomikawa fault in southwest Hokkaido, an acoustic survey was carried out off Kamiiso in Hakodate Bay. Using a sound wave exploring machine transmitting frequencies from 5.5 to 8.5 kHz, the acoustic survey was conducted on a workboat cruising at speeds of 4 to 6 knots. The courses of traverse were set on the sea area off from Kamiiso Tomikawa Town to Moheji Town based on the sediment distribution map and the geological map. A total of 17 courses were set: 16 in the east to west direction so as to cross the extension of active faults on the land, and one in the south to north direction. The east-west courses had a length of about 2 km with the line interval of about 300 m, while the south-north course extended nearly parallel with the coast line over a distance of 4.8 km. As a result of the present investigation, verification was given on existence of boundary faces with different sediment structures and displacement falling eastward on several courses of traverse running from east to west. If the locations of these boundary faces are connected, its strike agrees well with the strike of the Tomikawa fault on the land. From the fact that its extension is linked to the end section of the fault, a possibility was shown that the land fault may be extending into the sea area. 8 refs., 4 figs.

  2. Stress estimation around the survey wells in Hanshin-Awaji area by means of AE/DR and DSCA experiments; AE/DR ho to DSCA ho ni yoru Hanshin Awaji chiiki chosa kui shuhen no chikaku oryoku sokutei

    Energy Technology Data Exchange (ETDEWEB)

    Ito, H.; Kuwahara, Y.; Nishizawa, O. [Geological Survey of Japan, Tsukuba (Japan); Yamamoto, K. [Tohoku University, Sendai (Japan). Faculty of Science; Sano, O. [Yamaguchi University, Yamaguchi (Japan). Faculty of Engineering; Yokoyama, T.; Kudo, R. [OYO Corp., Tokyo (Japan); Xue, Z. [Kiso-Jiban Consultants Co. Ltd., Tokyo (Japan)

    1996-05-01

    A total of 5 wells were excavated in the Hanshin-Awaji area (Ikeda, Takarazuka, Tarumi, Hirabayashi and Ikunami) to collect the core samples, which were analyzed by the AE/DR and DSCA methods to determine crustal stresses. For the AE/DR analysis, the core sample was cut in the vertical direction, and in the horizontal direction at intervals of 45{degree}. The sample of unknown orientation was provided with a datum line common for both methods, to compare the results by these methods. A load was applied to the sample, provided with an AE sensor and strain gauge on the sides, in the longitudinal direction. For the DSCA analysis, the core sample was cut into a cube having a side length of 33mm, with a pair of planes directed in parallel to the datum line. A total of 18 strain gauges, 10mm in gauge length, were attached to the cube. The AE/DR analysis gave the maximum and minimum principal stresses in the horizontal plane and stresses in the vertical direction, whereas the DSCA the maximum, intermediate and minimum principal stresses. 3 refs., 7 figs.

  3. Research and development of peripheral technology for photovoltaic power systems. Research and development of photovoltaic modules integrated with construction materials (detachable plane panel); Shuhen gijutsu no kenkyu kaihatsu. Kenzai ittaigata module no kenkyu kaihatsu (chakudatsushiki heiban panel)

    Energy Technology Data Exchange (ETDEWEB)

    Tatsuta, M. [New Energy and Industrial Technology Development Organization, Tokyo (Japan)

    1994-12-01

    This paper reports the study results on R and D of photovoltaic modules integrated with construction materials in fiscal 1994. (1) On development of technology for module structures, specifications of the horizontal muntin system module were newly determined in addition to the improved muntin system module, and the prototype pseudo-module integrated with construction material was prepared. The comparison results of the basic performance of both system modules clarified superior waterproofing and module temperature uniformity of the horizontal muntin system. Based on this specifications, integration technology of modules with back metal plates was studied. Formation of the integrated module close to final specifications was ascertained to be possible by use of passivation equipment to irregular form. (2) On development of construction and installation methods of modules, improvement of the waterproofing and workability of both system modules was studied. (3) On the study on practical use of modules, their design and ventilation/cooling structure were studied. 38 figs., 13 tabs.

  4. Research and development of evaluation system for photovoltaic power generation system. Research and survey on test and evaluation method for BOS component devices; Taiyoko hatsuden system hyoka gijutsu no kenkyu kaihatsu. Shuhen gijutsu hyoka system no kenkyu kaihatsu

    Energy Technology Data Exchange (ETDEWEB)

    Tatsuta, M. [New Energy and Industrial Technology Development Organization, Tokyo (Japan)

    1994-12-01

    This paper reports the study results on R and D of the evaluation method for BOS component devices in fiscal 1994. (1) On the study on requirements of BOS component devices for practical use, the study results on storage battery, inverter, protective device for system interconnection, and effective use means for storage battery were summarized. On the future device technology, it was clarified that the following value added technologies are promising: simple design of inverter circuit, cost reduction by common specification and mass production, and stabilization of voltage and compensation of momentary peak load by combining inverter with small-capacity storage batteries. (2) On the study on the performance test method for BOS component devices, basic characteristic (capacity, efficiency) test, PSOC charge/discharge cycle test, and accelerated life cycle test were performed for 4 kinds of new storage batteries developed by NEDO. The whole characteristic test results satisfied specifications, and long-term cycle test is in promotion for all new storage batteries. 3 figs., 4 tabs.

  5. Research and development of peripheral technology for photovoltaic power systems. Research and development of redox flow battery for photovoltaic power generation; Shuhen gijutsu no kenkyu kaihatsu. Taiyoko hatsuden`yo redox denchi no kenkyu kaihatsu

    Energy Technology Data Exchange (ETDEWEB)

    Tatsuta, M. [New Energy and Industrial Technology Development Organization, Tokyo (Japan)

    1994-12-01

    This paper reports the study results on R and D of redox flow battery for photovoltaic power generation in fiscal 1994. (1) On the production method of electrolyte, silica reduction treatment was attempted to use ammonium metavanadate recovered from boiler as electrolyte of redox flow battery. Silica removal rates more than 90% were achieved by crystallizing V as polyvanadate while keeping molten silica. It was ascertained in minicell experiment that trivalent and quadrivalent V electrolytes produced from recovered V are applicable to continuous charge/discharge operation for one week. (2) On development of battery systems, the relation between battery characteristics and physicochemical properties of carbon fiber electrodes was studied to improve carbon fiber electrodes. The efficiency of 80% was achieved at current density of 160mA/cm{sup 2} by use of layered electrodes, resulting in considerable cost reduction. Performance evaluation operation of the 2kW battery prepared in the last fiscal year was also carried out. 4 figs.

  6. Research and development of peripheral technology for photovoltaic power systems. Meteorological analysis for suitable design of photovoltaic power generation systems; Shuhen gijutsu no kenkyu kaihatsu. Saiteki sekkei no tame no kisho data no chosa kenkyu

    Energy Technology Data Exchange (ETDEWEB)

    Tatsuta, M. [New Energy and Industrial Technology Development Organization, Tokyo (Japan)

    1994-12-01

    This paper reports the study results on the standard weather data necessary for simulation of PV power generation systems in fiscal 1994. In the study on the selection criterion of the standard weather data from the viewpoint of PV power generation systems, three typical years are used; a year with average solar radiation, and two years with extremely less and more solar radiation for safe simulation. The standard weather data are arranged for output calculation of PV power generation systems by selecting the most typical year based on long-term observation data. The data to be arranged are as follows; total, direct and scattered solar radiations incident upon a horizontal surface, solar radiation upon a slope surface, sunshine duration, air temperature, wind direction, wind velocity, amount of precipitation, and snow depth. For arrangement of the nationwide standard weather data, estimation of total solar radiation is necessary based on sunshine duration data observed by all weather bureaus. In this study, the estimation model was developed of the total solar radiation integrated with time from rotary pyrheliometer data. 5 figs.

  7. Research and development of peripheral technology for photovoltaic power systems. Research on engineering methods for cost effective PV installation; Shuhen gijutsu no kenkyu kaihatsu. Tashu secchi koho no kenkyu kaihatsu

    Energy Technology Data Exchange (ETDEWEB)

    Tatsuta, M. [New Energy and Industrial Technology Development Organization, Tokyo (Japan)

    1994-12-01

    This paper reports the study results on R and D of engineering methods for photovoltaic power system installation in fiscal 1994. (1) On the survey on applicable fields, various application aspects, applicability, and problems on location and legal regulation were continuously studied for railway, river reservation, lake surface and public facility as promising locations after highway in the last fiscal year. The result pointed out relatively easy possibility of PV power generation of nearly 11,700MW except residence and building fields. (2) On installation technology of solar cell arrays, several models based on various installation conditions, construction methods and system configurations were studied, and various application aspects were proposed by combination of simple design conditions. (3) On test and evaluation of the structural design of array racks, wind tunnel experiments were conducted for structure wall, platform shed and highway sound insulation wall. (4) On basic design of various promising systems, the conceptual design of interconnection systems was carried out assuming applications to highway and railway. 7 figs., 3 tabs.

  8. Research and development of peripheral technology for photovoltaic power systems. Study of nickel-hydride storage battery for photovoltaic generation systems; Shuhen gijutsu no kenkyu kaihatsu. Taiyoko hatsuden`yo suiso denchi no kenkyu kaihatsu

    Energy Technology Data Exchange (ETDEWEB)

    Tatsuta, M. [New Energy and Industrial Technology Development Organization, Tokyo (Japan)

    1994-12-01

    This paper reports the study results on R and D of nickel-hydride storage battery for photovoltaic generation systems in fiscal 1994. (1) On the study on low-cost electrode materials, the physical properties and electrode characteristics were studied of the prototype hydrogen absorbing alloys prepared by substituting Cu or Ni for Co in Mm(Ni-Co-Mn-Al)5 (Mm: mixture of rare earth elements). The result clarified that it is difficult to reduce Co content in the alloy to 0.4 atom or less. Simple heat treatment and milling processes in production of hydrogen absorbing alloy electrodes were achieved by adopting an improved metal mold and gas atomization method. Characteristics and cycle life of the Ni positive electrode prepared by applying active paste material of Ni(OH)2 were studied, however, the result showed only lives of nearly 300 cycles. (2) On the study on electrode structure for high-performance (long-life) battery, the 3-D porous metal electrode support was evaluated, and various battery configurations were studied. 11 figs., 1 tab.

  9. Research and development of molten carbonate fuel cell power generation systems. ; Development of stacks and peripheral systems. Yoyu tansan'engata nenryo denchi hatsuden system no kenkyu kaihatsu. ; Sutakku oyobi shuhen system no kaihatsu

    Energy Technology Data Exchange (ETDEWEB)

    1994-02-01

    This paper reports research and development of molten carbonate fuel cell power generation systems of composite large-capacity type, variation large-capacity type, and internal reforming type. Development works on the composite large-capacity type stacks included trial fabrication of basic modules and composite large-capacity cells, development of high-performance long-life electrodes, electrolyte plates, and high corrosion resistant cell constitutive materials, heat resistant cycling tests and life tests, and development of a technology to use higher pressures in fuel cells, and a technology to cool and seal laminar cells. Development works on the variation large-capacity stacks have performed studies on electrode life extension, pressurized operation technologies, tightening methods, fabrication of thin plate processed separators, electrodes, and electrolyte plates, power generation tests on large-area cells, and cooling characteristics analysis. In order to establish an internal reforming fuel cell technology, elucidation has been given on deactivation mechanisms in internal reforming catalysts, as well as discussions on structures of internal reforming fuel cells. As stack operational researches, evaluation tests have been given on 10-kW and 100-kW class stacks. Discussions have been given on heat exchange type and two-step catalyst combustion type reformers as peripheral devices. 26 figs., 6 tabs.

  10. Report on achievements in fiscal 1998. Development of technologies to put photovoltaic power generation systems into practical use - Research and development of solar beam power generation and utilization systems and ancillary technologies (Development of ancillary devices for AC modules); 1998 nendo taiyoko hatsuden system jitsuyoka gijutsu kaihatsu seika hokokusho. Taiyoko hatsuden riyo system shuhen gijutsu no kenkyu kaihatsu (AC module yo shuhen sochi no kenkyu)

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    1999-03-01

    Reasonability evaluation was progressed on the fundamental technologies having been proposed in fiscal 1998, and development was made on elementary technologies required for system structuring. The proposals made in fiscal 1998 include the deepening of the evaluations on effectiveness of AC modules, long-term stability evaluation on the system control schemes, trial fabrication and evaluation on AC battery modules, and development and installation of 2-kW demonstration facilities. In the effectiveness evaluation, discussions were given not only on advantages, but also on disadvantages. As the advantageous point, theoretical analyses were progressed on the effect of reducing the output drop due to shading, which was made clear by providing values. Effects of increase in switching units on electric wave interference as a disadvantage were made clear. As a form that can be applied consistently from an independent power source to a system coordination system, a flexible system using the module system comprising of AC modules and AC batteries was proposed as an effective utilization measure. A proposal was also made on an autonomous discrete type system control scheme as a control system that has sufficient expandability, and is durable against disasters. (NEDO)

  11. Fault-related-folding structure and reflection seismic sections. Construction of earth model using balanced cross section; Danso ga kaizaisuru shukyoku kozo no keitai to jishin tansa danmen. 1. Balanced cross section wo mochiita chika model no kochiku

    Energy Technology Data Exchange (ETDEWEB)

    Matsuoka, T.; Tamagawa, T. [Japan Petroleum Exploration Corp., Tokyo (Japan); Tsukui, R. [Japan National Oil Corp., Tokyo (Japan). Technology Research Center

    1997-05-27

    Pre-stacking depth migration treatment is studied for the estimation of the fold configuration from seismic survey cross sections. The estimation of a velocity structure is necessary for the execution of such treatment, and the utilization of structural-geological knowledge is required for its interpretation. The concept of balanced cross section in relation to the fault-bend fold constructs a stratum structure model under conditions that the deformation during fold and fault formation is a planar strain, that there is no change in volume due to deformation, and that a fold is a parallel fold. In addition to the above geometric and kinetic approach, there is another fold formation process simulation model using a Newtonian fluid for study from the viewpoint of dynamics. This simulation stands on the presumption that the boundary contains a ramp that had been in presence before fold formation and that an incompressible viscous matter is mounted on the top surface. The viscous matter flows and deforms for the formation of an anticline on the ramp. Such enables the reproduction of a fault-bend fold formation process, and helpful discussion may be furthered on the dynamic aspect of this simulation. 5 refs., 4 figs.

  12. Fault-related-folding structures and reflection seismic sections. Study by seismic modeling and balanced cross section; Danso ga kaizaisuru shukyoku kozo no keitai to jishin tansa danmen. 2. Seismic modeling oyobi balanced cross section ni yoru study

    Energy Technology Data Exchange (ETDEWEB)

    Tamagawa, T.; Matsuoka, T. [Japan Petroleum Exploration Corp., Tokyo (Japan); Tsukui, R. [Japan National Oil Corp., Tokyo (Japan). Technology Research Center

    1997-05-27

    It occasionally happens that there exists a part where reflection near the thrust is not clearly observed in a thrust zone seismic survey cross section. For the effective interpretation of such an occurrence, the use of geological structures as well as the reflected pattern is effective. When the velocity structures for a fold structure having a listric fault caused anticline (unidirectionally inclined with a backlimb, without a forelimb) and for a fault propagation fold are involved, a wrong interpretation may be made since they look alike in reflection wave pattern despite their difference in geological structure. In the concept of balanced cross section, a check is performed, when the stratum after deformation is recovered to the time of deposition, as to whether the geologic stratum area is conserved without excess or shortage. An excess or shortage occurs if there is an error in the model, and this shows that the fault surface or fold structure is not correctly reflected. Positive application of geological knowledge is required in the processing and interpreting of data from a seismic survey. 6 refs., 6 figs.

  13. Achievement report for fiscal 2000 on the fundamental research on functional sectional imaging system using optical interference; 2000 nendo hikari kansho riyo kokino danso gazo sokutei sytsem ni kansuru kiban kenkyu seika hokokusho

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    2001-05-16

    This project promotes the fundamental research on the conventional OCT technology to make it applicable to wider clinical applications of diagnoses and therapies by greatly improving the technology in view of higher spatial resolution, smaller size, and functional diversification. The research is supported by the medical and engineering cooperative research that utilizes the medical and engineering knowledge. Furthermore, as the fundamental technologies for the next generation, the sectional image measuring technology is established that makes possible to measure the three-dimensional flow and movement such as blood flow distribution in very small blood vessels, and performs the basic research on high-speed sectional image measurement to measure moving images of sectional images. The research contents for the current fiscal year may be summarized as follows: in the research on a small integrated optical element to make diagnostic application possible for skin cancers, retinal detachment, and cataract, research on trial production of a small OCT has been performed, and research on high spatial resolution has been implemented; furthermore, research was carried out on an endoscope integrated type OCT system intended of textural diagnoses of gastric cancer, hemorrhoidal cancer, and colic cancer, and on a sectional image measuring system intended of extracting biochemical information, and on a high-precision absorptive spectrum measuring technology for biogenic structures. (NEDO)

  14. Excitation of tsunami by a pure strike-slip earthquake. ; Izu Oshima kinkai earthquake tsunami on Feb. 20, 1990. Yokozure danso jishin ni yoru tsunami no reiki. ; 1990 nen 2 gatsu 20 nichi Izu Oshima kinkai jishin tsunami

    Energy Technology Data Exchange (ETDEWEB)

    Abe, K. (Nippon Dental University, Tokyo (Japan). Niigata Junior College); Okada, M. (Meteorological Research Institute, Tsukuba (Japan))

    1993-06-24

    A numerical experiment was performed to reproduce the tsunami from the Izu-Oshima Kinkai Earthquake which occurred on February 20, 1990, using a tsunami excited by a pure strike-slip fault. An existence of a vertical fault with a length of 15 km and a width of 12 km was hypothesized in the south-north direction on the ocean bottom around the focal region. Then, a tsunami was assumed to have been excited when the fault was given a side-slip movement to create discrepancies of 1 m in the fault. Water level change for one hour after onset of the tsunami was calculated in one-second interval in each unit square with a side length of 1 km over an ocean area of 200 km from east to west and 150 km from north to south centering on the wave source. The results obtained from the calculation were harmonious with tsunami waveforms observed at five stations in the subject region and their spectral analytic results. Reproduced were the two predominant frequencies commonly observed at more than two stations, and difference in predominant cycles that appear according to azimuths of the observation points to the epicenter. These facts endorse the reasonability of the above hypothesis. 9 refs., 11 figs.

  15. West African Journal of Applied Ecology - Vol 17, No 1 (2010)

    African Journals Online (AJOL)

    Soil microbial biomass Carbon, Nitrogen and Phosphorus dynamics under different amendments and cropping systems in the semi-deciduous Forest Zone of Ghana · EMAIL FREE FULL TEXT EMAIL FREE FULL TEXT · DOWNLOAD FULL TEXT DOWNLOAD FULL TEXT. V Logah, EY Safo, C Quansah, I Danso ...

  16. Agricultural and Food Science Journal of Ghana - Vol 4 (2005)

    African Journals Online (AJOL)

    Accounting for training results: an evaluation of the training activities of the root and tuber improvement programme · EMAIL FULL TEXT EMAIL FULL TEXT · DOWNLOAD FULL TEXT DOWNLOAD FULL TEXT. CK Osei, JN Berchie, IOO Ansah, S Gyasi-Boakye, SN Asante, AA Adjekum, Salome Danso, 279-290.

  17. Author Details

    African Journals Online (AJOL)

    Danso, AP. Vol 56, No 1-4 (2010) - Articles Tubular ectasia of the rete testis associated with azoospermia: A case report. Abstract. ISSN: 0008-9176. AJOL African Journals Online. HOW TO USE AJOL... for Researchers · for Librarians · for Authors · FAQ's · More about AJOL · AJOL's Partners · Terms and Conditions of Use ...

  18. Journal of the Ghana Science Association - Vol 11, No 1 (2009)

    African Journals Online (AJOL)

    Rapid multiplication of Bambool (Bambusa heterostachya): the effect of culm age and length of cuttings on sprouting · EMAIL FULL TEXT EMAIL FULL TEXT DOWNLOAD FULL TEXT DOWNLOAD FULL TEXT. BN Nuertey, A Opoku, I Danso. http://dx.doi.org/10.4314/jgsa.v11i1.46984 ...

  19. Genomic heterogeneity within cowpea bradyrhizobia isolated from ...

    African Journals Online (AJOL)

    Genomic heterogeneity within cowpea bradyrhizobia isolated from Ghanaian soils. JO Fening, A Sessitsch, SK Offei, SKA Danso. Abstract. No Abstract. Full Text: EMAIL FREE FULL TEXT EMAIL FREE FULL TEXT · DOWNLOAD FULL TEXT DOWNLOAD FULL TEXT · http://dx.doi.org/10.4314/wajae.v6i1.45605.

  20. Browse Title Index

    African Journals Online (AJOL)

    Items 251 - 300 of 366 ... S N Anyanwu. Vol 63, No 4-6 (2017), Stepwise minimal debridement in Fournier's gangrene: a technical note, Abstract. M.C. Kabeya, A Danso, L Gwanzura. Vol 46, No 9 (2000), Storage of breast milk: effect of temperature and storage duration on microbial growth, Abstract. E O Igumbor, R D Makura, ...

  1. Polycyclic Aromatic Hydrocarbons (PAHs) Content in Cattle Hides ...

    African Journals Online (AJOL)

    ADOWIE PERE

    tyres for processing food. ©JASEM https://dx.doi.org/10.4314/jasem.v21i6.19. Keywords: Cattle hide ... on the substance used as fuel for meat processing. Traditionally, firewood has been the main source of ... and other forms of meat processing in some third world countries (Obiri-Danso et al., 2008). Scrap tyre, according to ...

  2. Sensing of subsurface faults based on an imaging technique for teleseismic waveform data. 2. Feasibility study for application to oblique incidence, multi-event and noise data; Enchi jishin hakei data wo mochiita chika kozo imaging ni yoru chichu danso kenshutsu no kokoromi. 2. Naname nyusha, multi event, noise wo fukumu hakei eno tekiyo

    Energy Technology Data Exchange (ETDEWEB)

    Murakoshi, T.; Takenaka, H.; Saita, T. [Kyushu University, Fukuoka (Japan). Faculty of Science; Suetsugu, D. [Building Research Institute, Tokyo (Japan); Furumura, T. [Hokkaido University of Education, Sapporo (Japan)

    1996-05-01

    An examination was made on the method in which imaging of subsurface was carried out with teleseismic waveform data for sensing of faults. In the examination, an experiment was done on the sensing of faults with higher precision, by applying oblique incidence as well as perpendicular upward incidence of SH plane waves, and thereby stacking the imaging in plural events. In numerical experiments, 28 observation points were arranged at 500m spaces apart on the surface, and the incident waves were made the SH plane waves having a bell-shaped time function, with incidence made at an angle varied as 0{degree}, +15{degree} and -15{degree} from the lowest layer of a model. In the calculation of the wave motion field, a difference calculus with secondary accuracy was used for both time and space. In addition, data was prepared with a random noise added to a synthesized waveform to be used as observation data. The calculated waveform data were likened to the observation waveform, to which the method for imaging faults was applied. Consequently, it was noted that satisfactory results were obtained compared with the case where faults were sensed by one event alone. 5 refs., 4 figs.

  3. New Sunshine Program for fiscal 2000. Development of photovoltaic power system commercialization technology (Development of ultrahigh-efficiency crystalline compound solar cell manufacturing technology - Surveys and studies of peripheral key technologies/Surveys of environmentally-friendliness enhancement for next-generation solar cell development); 2000 nendo New sunshine keikaku seika hokokusho. Taiyoko hatsuden system jitsuyoka gijutsu kaihatsu - Chokokoritsu kessho kagobutsu taiyo denchi no seizo gijutsu kaihatsu (Shuhen yoso gijutsu ni kansuru kenkyu chosa, Jisedai taiyodenchi kaihatsu kankyo tekioka chosa)

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    2001-03-01

    Though the trends of solar cell development are becoming increasingly diverse across the world, yet none has emerged to promise a stable solar cell supply in the future. Under the circumstances, studies were conducted to clarify strategies for solar cell technology development which would be well adapted to Japan's social environments, with the trends of development in the United States and European countries taken into consideration. The surveys covered the research and development and diffusion of photovoltaic power generation in the United States and European countries, and their solar cell research and development strategies and trends of development were put together. Surveys were also conducted into the research and development of unconventional types of solar cells, such as the dye-sensitized solar cell, organic solar cell, conjugate polymer solar cell, and the polymer/C{sub 60} based solar cell, and into the status of resources of materials for solar cells such as gallium, arsenic, cadmium, tellurium, indium, selenium, and germanium. Regarding the future of photovoltaic power generation research and development, it was concluded that commercialization technology development and basic research and development should continue. Also pointed out was the importance of the enlargement of the market for photovoltaic power generation systems. (NEDO)

  4. Fiscal 1999 research and development of technologies for practical application of photovoltaic power generation systems. Development of ultrahigh-efficiency crystalline compound solar cell manufacturing technology (Survey of peripheral element technologies - Survey of environmental adaptation of next-generation solar cell development); 1999 nendo taiyoko hatsuden system jitsuyoka gijutsu kaihatsu seika hokokusho. Chokokoritsu kessho kagobutsu taiyo denchi no seizo gijutsu kaihatsu (shuhen yoso gijutsu ni kansuru chosa kenkyu - jisedai taiyo denchi kaihatsu kankyo tekioka chosa)

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    2000-03-01

    Surveys are conducted of photovoltaic power system development projects and their utilization in Japan and overseas, and a discussion is made on the progress, technical challenges, effects, and implementation systems relating to the solar cell application technology development project under the New Sunshine Program. Compiled in the report are the results of surveys of the research and development of photovoltaic power systems and their diffusion in the U.S. and European nations, and the research and development strategies for and the trends of the development of various types of solar cells in these countries. The trends of research and development of non-conventional type solar cells are also collected, which include 3 cases of TPV (thermophotovoltaic) devices, 5 cases of new inorganic materials, 1 case of new organic materials, and 4 cases of dye-sensitized solar cells. In relation to the status of resources of crystalline compound-based solar cell materials, raw materials for solar cells other than silicon are taken up, and their reserves, manufacturing methods, quantities yielded and consumed, costs, etc., are surveyed. These are all taken into consideration in discussing the basic approach to the study of future research and development as it ought to be. (NEDO)

  5. FY 2000 report on the results of the development of commercialization technology of the photovoltaic power system. R and D of the photovoltaic power generation utilization system/periphery technology (R and D of the new solar cell module integrated with construction materials - Investigative study on analysis for commercialization); 2000 nendo New sunshine keikaku seika hokokusho. Taiyoko hatsuden system jitsuyoka gijutsu kaihatsu, Taiyoko hatsuden riyo system, shuhen gijutsu no kenkyu kaihatsu (Shinkenzai ittaigata taiyodenchi mojuru no kenkyu kaihatsu - Jitsuyoka kaiseki ni kansuru chosa kenkyu)

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    2001-03-01

    For the purpose of supporting the study for commercialization of the new module integrated with construction materials, survey of the technical trend of the new module integrated with construction materials in Japan and abroad was conducted, and the FY 2000 results were summarized. As to the module material correspondent to construction materials, the results of the survey made in the past three years were summarized, and the subjects to be considered in future were arranged from a viewpoint of disposal/recycle of modules. Concerning the marketability, various policies for the spread of solar cell module that is an immature good were arranged. Survey was also made of the photovoltaic power system using the field test project as a sample, and the following were made clear: The photovoltaic power generation has appeal for environmental consideration and energy conservation; In some cases, the power generation effect was not as much as expected because the information on design/construction is not sufficient. Relating to the evaluation of its effect on the environment, the paper summarized the environmental influence in each of the module methods at each stage of production/utilization/disposal and the basic items for measures to cope with the influence. (NEDO)

  6. FY 1999 report on the results of the R and D project on the industrial technology for the global environment. R and D of the prediction technology of environmental effects brought by CO2 ocean sequestration (Development of prediction technology of environmental effects around the point of CO2 discharge and the research support survey); 1999 nendo chikyu kankyo sangyo gijutsu kenkyu kaihatsu jigyo NEDO seika hokokusho. Nisankatanso no kaiyo kakuri ni tomonau kankyo eikyo yosoku gijutsu kenkyu kaihatsu (CO2 horyuten shuhen'iki no kankyo eikyo yosoku gijutsu no kaihatsu narabini kenkyu shien chosa)

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    2000-03-01

    For the purpose of studying viability of CO2 ocean sequestration by discharging it at the intermediate depth of ocean, the R and D were conducted of 'prediction technology of environmental effects around the point of CO2 discharge,' and the FY 1999 results were summarized. In the study of elucidation of behavior of liquid CO2 at the time of discharge, melting speed of CO2 in water and seawater, 2D CO2 concentration distribution, etc. were measured using the circulation type deep-sea simulation experimental equipment. In the study of technology to send CO2 into the sea and dilute it, the process test using mock liquid was conducted. In the indoor experiment on CO2 effects on marine organisms, conducted were the detailed experiment on long-term effects of low concentration CO2 on sea urchins and shellfish, experiment on CO2 acute effects on eggs/fry and experiment on CO2 effects on adult fish. In the developmental study of the model to predict environmental effects around the point of CO2 discharge, carried out were the improvement of the model for prediction of effects on marine organisms, study of the CO2 diffusion in topographic features supposed to be Hawaii, etc. In the international joint study, measurement/observation technology, facilities, etc. were studied in preparation for the experiment actually conducted in the sea. (NEDO)

  7. FY 2000 report on the results of the project on the R and D of the global environmental industry technology. R and D of the technology for predicting environmental effects associated with the CO2 ocean sequestration (Development of the technology for predicting environmental effects in the area around the CO2 discharge point and survey for supporting study); 2000 nendo chikyu kankyo sangyo gijutsu kenkyu kaihatsu jigyo. Nisanka tanso no kaiyo kakuri ni tomonau kankyo eikyo yosoku gijutsu kenkyu kaihatsu (CO2 horyuten shuhen'iki no kankyo eikyo yosoku gijutsu no kaihatsu narabini kenkyu shien chosa)

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    2002-03-01

    To obtain the technical outlook for CO2 ocean sequestration by CO2 discharge into the intermediate layer, the R and D was conducted of the technology for predicting environmental effects in the area around the CO2 discharge point, and the FY 2000 results were summed up. In the elucidation study of the behavior at the time of discharging liquid CO2, the melting process of CO2 droplets discharged/dispersed into the seawater of the intermediate layer was observed, and the specific phenomenon of hydrate formation in the process of CO2 droplet formation was grasped. As to the technology for sending CO2 into the ocean and diluting it, experimental study was made of CO2 transportation technology from on the sea to the intermediate layer, technology for rapid dilution immediately after discharge, etc. About the indoor experiment on the CO2 influence on marine organisms, experiment on the CO2 influence was carried out using shells, sea urchin, red sea bream, etc. In the developmental study of models for predicting environmental effects in the area around the CO2 discharge point, the 3D two-phase flow LES model was developed as a model for predicting the CO2 behavior, and the simulation of the liquid CO2 discharge was made at the planned experimental site. The model for evaluation of the biological influence was also made which can consider the interaction between two kinds of organisms. (NEDO)

  8. FY 2000 report on the results of the development of commercialization technology of the photovoltaic power system. Summary. R and D of the photovoltaic power generation utilization system/periphery technology (R and D on the improvement of reliability of photovoltaic power generation - Investigative study of long-term reliability of inverter - Separate volume: Data on the life evaluation test); 2000 nendo New sunshine keikaku seika hokokusho(Sokatsu ban). Taiyoko hatsuden system jitsuyoka gijutsu kaihatsu, Taiyoko hatsuden riyo system shuhen gijutsu no kenkyu kaihatsu (Taiyokohatsuden no shinraisei kojo ni kansuru kenkyu kaihatsu - Inbata no choki shinraisei no chosa kenkyu - Bessatsu : Jumyo hyoka shiken datashu)

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    2001-03-01

    For the purpose of establishing a life evaluation method for power conditioner of about several kilowatts for general housing use, the acceleration test was made, and the data were summarized for maintenance of power quality, cooperation with the protection system at power system, insuring of safety of personnel/facilities, etc. As to the acceleration method, by paying attention to heat deterioration of thermal plasticity materials being used for power conditioner and by using the acceleration method using the 10-degree C half law by the Arrhenius law, temperature and humidity were set at 40 degrees C and 36%, respectively. The operation hour and stopping time were fixed at 3.5 hours and 4.5 hours, respectively. The life evaluation measurement by the acceleration test was composed of the continuous evaluation measurement with the aim of early finding the degradation of performance, anomaly, etc. of power conditioner and of the evaluation measurement at specified intervals with the aim of precisely measuring the state of degradation of power conditioner. As a result of the continuous evaluation measurement, the paper reported the data on the rise in temperature inside the power conditioner during the acceleration test and the change in electric characteristics of input/output. (NEDO)

  9. Report on achievements in fiscal 1998. Research and development of a technology to forecast environmental effect in association with isolation of carbon dioxide in oceans. (Surveys on development and research support on a technology to forecast environmental effect in areas in the vicinity of CO2 discharging points); 1998 nendo nisanka tanso no kaiyo kakuri ni tomonau kankyo eikyo yosoku gijutsu kenkyu kaihatsu seika hokokusho. CO{sub 2} horyuten shuhen'iki no kankyo eikyo yosoku gijutsu no kaihatsu narabini kenkyu shien chosa

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    1999-03-01

    Atmospheric concentration of CO2 is increasing, and discussions are urged on measures to suppress emission of CO2 into atmosphere. While different CO2 fixing technologies may be conceived, there is a technology to utilize CO2 absorbing capability of ocean by discharging and dissolving CO2 artificially into middle layer of the ocean to separate CO2 from atmosphere. This technology is one of the technologies which are promising in the aspects of technology, economic performance, and possible amount of CO2 reduction. However, it is difficult to say that scientific and technological discussions have been given sufficiently on behavior of CO2 discharged into the ocean, effect of the discharge on environments, and CO2 separation capability of the ocean. Therefore, in the present research and development, a 'technology to forecast environmental effect in areas in the vicinity of CO2 discharging points' is developed to serve for acquiring technological prospect on the feasibility to realize the CO2 ocean separation by discharging CO2 into the middle layer of the ocean. The present fiscal year has performed researches on the following research and development items: elucidation of behavior of liquefied CO2 when discharged into the ocean, CO2 feeding and diluting technologies, indoor experiments on the effects of CO2 on ocean living organisms, and development of a model to forecast environments in areas in the vicinity of CO2 discharging points. (NEDO)

  10. SURFACE FAULT CHARACTERISTICS OF THE 1995 HYOGOKEN-NAMBU EARTHQUAKE

    OpenAIRE

    Takashi, NAKATA; Kiyoshi, YOMOGIDA; Professor, Department of Geography, Hiroshima University:Associate Professor, Department of Earth and Planetary Systems Science, Hiroshima University; Professor, Department of Geography, Hiroshima University:Associate Professor, Department of Earth and Planetary Systems Science, Hiroshima University

    1995-01-01

    Distinctive ruptures in the surface faulting that generated the destructive 1995 Hyogoken-nambu earthquake (Ms = 7.2) appeared along the Nojima fault, an active fault on the northwestern coast of Awaji Island, Japan. These surface fault ruptures extend continuously southwestward for 10 km from Ezaki lighthouse, near the epicenter to Toshima Town in Hokudan, and display prominent right-lateral off-sets of roads, paddy dikes and so on of 1.9 m maximum with vertical displacement of 1.2 m maximum...

  11. Ferrimagnetic resonance signal produced by frictional heating: A new indicator of paleoseismicity

    Science.gov (United States)

    Fukuchi, Tatsuro; Mizoguchi, Kazuo; Shimamoto, Toshihiko

    2005-12-01

    High-speed fault slips during earthquakes may generate sufficient frictional heat to produce fused fault rocks such as pseudotachylyte. We have carried out high-speed slip tests using natural fault gouge to judge whether or not frictional heating universally occurs during seismic fault slips. In our shearing tests, natural fault gouge is put between two cylindrical silica glasses and sheared under a fixed axial stress of 0.61 MPa. Despite such a low stress near the Earth's surface, a darkened cohesive material resembling pseudotachylyte is made from the fault gouge along the edge of a circular shear plane when shearing at a high speed of 1500 rpm (the maximum slip rate reaches ˜1.96 m/s at the edge). Electron spin resonance measurements reveal that the darkened cohesive material has a strong ferrimagnetic resonance (FMR) signal, which is derived from bulky trivalent iron ions in ferrimagnetic iron oxides (γ-Fe2O3). The FMR signal is produced by the thermal dehydration of antiferromagnetic iron oxides (γ-FeOOH) in the fault gouge. This may be applicable to the detection of past heating during seismic fault slip. We thus attempt to reconstruct the temperature of frictional heat generated on the Nojima fault plane in the 1995 Kobe earthquake (M = 7.3) by inversion using the FMR signal. The computer simulation indicates that the frictional heat generated on the Nojima fault plane at ˜390 m depth may have attained ˜390°C during the 1995 Kobe earthquake. The temperature in the fault plane may have returned to its initial state after ˜1 year. This result suggests that a heat flow anomaly generated by faulting may be difficult to detect.

  12. Generation of mouse and human induced pluripotent stem cells (iPSC) from primary somatic cells.

    Science.gov (United States)

    Lorenzo, I M; Fleischer, A; Bachiller, D

    2013-08-01

    Cellular reprogramming consists of the conversion of differentiated cells into pluripotent cells; the so-called induced Pluripotent Stem Cells. iPSC are amenable to in vitro manipulation and, in theory, direct production of any differentiated cell type. Furthermore, iPSC can be obtained from sick individuals and subsequently used for disease modeling, drug discovery and regenerative treatments. iPSC production was first achieved by transducing, with the use of retroviral vectors, four specific transcription factors: Oct4, Klf4, Sox2 and c-Myc (OKSM), into primary cells in culture Takahashi and Yamanaka, (Cell 126(4):663-676, 2006). Many alternative protocols have since been proposed: repeated transfections of expression plasmids containing the four pluripotency-associated genes Okita et al. (Science 322(5903):949-953, 2008), lentiviral delivery of the four factors Sommer et al. (Stem Cells 27(3):543-549, 2009), Sendai virus delivery Fusaki et al. (Proceedings of the Japan Academy. Series B, Physical and Biological Sciences 85(8):348-362, 2009), removal of the reprogramming vectors by 'piggyBac' transposition Woltjen et al. (Nature 458(7239):766-770, 2009); Kaji et al. (Nature 458(7239):771-775, 2009), Cre-recombinase excisable viruses Soldner et al. (Cell 136(5):964-977, 2009), episomal vectors Yu et al. (Science 324(5928):797-801, 2009), cell-penetrating reprogramming proteins Zhou et al. (Stem Cells 4(5):381-384, 2009), mammalian artificial chromosomes Hiratsuka et al. (PLoS One 6(10):e25961, 2011) synthetically modified mRNAs Warren et al. (Scientific Reports 2:657, 2012), miRNA Anokye-Danso et al. (Cell Stem Cell 8(4):376-388, 2009); however, although some of these methods are commercially available, in general they still need to attain the reproducibility and reprogramming efficiency required for routine applications Mochiduki and Okita (Biotechnol Journal 7(6):789-797, 2012). Herein we explain, in four detailed protocols, the isolation of mouse and human

  13. Magnetic insights on seismogenic processes from scientific drilling of fault

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    Ferre, E. C.; Chou, Y. M.; Aubourg, C. T.; Li, H.; Doan, M. L.; Townend, J.; Sutherland, R.; Toy, V.

    2017-12-01

    Modern investigations through scientific drilling of recently seismogenic faults have provided remarkable insights on the physics of rupture processes. Following devastating earthquakes, several drilling programs focused since 1995 on the Nojima, Chelungpu, San Andreas, Wenchuan, Nankai Trough, Japan Trench and New Zealand Alpine faults. While these efforts were all crowned with success largely due to the multidisciplinarity of investigations, valuable insights were gained from rock magnetism and paleomagnetism and deserve to be highlighted. Continuous logging of magnetic properties allows detection of mineralogical and chemical changes in the host rock and fault zone particularly in slip zones, whether these are caused by frictional melting, elevation of temperature, ultracataclasis, or post-seismic fluid rock interaction. Further magnetic experiments on discrete samples including magnetic susceptibility, natural remanent magnetization, hysteresis properties, isothermal remanent magnetization acquisition and first order reversal curves, provide additional constrains on the nature, concentration and grain size of magnetic carriers. These experiments typically also inform on magnetization processes by thermal, chemical, or electrical mechanisms. Magnetic fabrics are generally not investigated on fault rocks from drill cores primarily in an effort to conserve the recovered core. However, recent methodological developments now would allow chemically non-destructive anisotropy of magnetic susceptibility (AMS) measurements to be performed on small 3.5 mm cubes. The mini-AMS method could provide crucial information on the kinematics of frictional melts produced during recent or ancient earthquakes and therefore would constrain the corresponding focal mechanisms. Finally, demagnetization experiments of the natural remanent magnetization (NRM) are one of the most powerful items in the magnetic toolkit because they provide chronological constrains on magnetization processes

  14. Clinicopathological and immunohistochemical features of lung invasive mucinous adenocarcinoma based on computed tomography findings

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    Shimizu K

    2016-12-01

    Full Text Available Katsuhiko Shimizu, Riki Okita, Shinsuke Saisho, Ai Maeda, Yuji Nojima, Masao Nakata Department of General Thoracic Surgery, Kawasaki Medical School, Kurashiki, Okayama, Japan Background: We performed an analysis to clarify differences in clinicopathological and molecular features of lung invasive mucinous adenocarcinoma (IMA based on computed tomography (CT findings and their impact on prognosis.Patients and methods: On the basis of CT findings, we divided lung IMA into three subtypes: solid, bubbling, and pneumonic. We then investigated differences in clinicopathological characteristics, prognosis, and the expressions of well-identified biomarkers, including cyclooxygenase-2 (Cox-2, excision repair cross-complementation group 1 (ERCC1, ribonucleotide reductase M1 (RRM1, class III beta-tubulin, thymidylate synthase (TS, secreted protein acidic and rich in cysteine (SPARC, programmed cell death-1 ligand-1 (PD-L1, and epidermal growth factor receptor mutation, among the three subtypes.Results: A total of 29 patients with resected lung IMA were analyzed. Compared with the solid or bubbling type, the pneumonic type had a higher proportion of symptoms, a larger tumor size, a higher pathological stage, and a significantly worse prognosis. The immunohistochemical findings tended to show high expression of RRM1, class III beta-tubulin, and Cox-2 in the tumor and of SPARC in the stroma, but not of ERCC1, TS, and PD-L1 in the tumor. None of the biomarkers with high expression levels in the tumor were prognostic biomarkers, but the expression of SPARC in the stroma was correlated with a poor outcome.Conclusion: Clinical and pathological features, in conjunction with molecular data, indicate that IMA should be divided into different subgroups. In our results, the pneumonic type was correlated with a significantly worse outcome. Further studies should be performed to confirm our conclusion and to explore its molecular implications. Keywords: non-small cell

  15. An investigation of coseismic OSL / TL time zeroing of quartz gouge based on low- to high-velocity friction experiments

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    Akasegawa, K.; Oohashi, K.; Hasebe, N.; Miura, K.

    2016-12-01

    To determine an age of coseismic event of an active fault, we generally examine crosscutting relationship between faults and overlying strata by trenching. However, we could not apply this method in case there are no overlying young strata in the vicinity of the fault zones. The alternative is a dating of fault zone materials whose age experienced resetting with seismic fault slip (for example, the ESR method;. Ikeya et al,1982; the OSL and TL methods). The idea behinds to the OSL (optically stimulated luminescence) and TL (thermoluminescence) dating methods for a determination of paleo-earthquake event is the accumulated natural radiation damage becomes to zero (time zeroing) by the frictional heating and grinding. However, physical and geological conditions required to induce time zeroing is not well understood because there is only few experimental investigations under the limited conditions (Hiraga et al,2004;. Kim et al, 2014) . In this study, we conduct low- to high-velocity friction experiments using quartz gouge under various experimental conditions (e.g., normal stress, displacement, moisture content) to establish an empirical relationship and physical and geological conditions of coseismic OSL time zeroing. In this experiment, we carry out the friction experiments using quartz in Tsushigawa granite taken from the east wall of the Nojima fault Ogura trench site, which was excavated in 2015. Samples were taken from the most distant position from the fault in the trench site. The samples were clashed using a mortar and sieved to a grain size of treatment. The residual is user for the friction experiments after having known radiation dose using an artificial gamma-ray source. In this presentation, we show results of the friction experiments and dating of the quartz gouge and discuss physical and geological conditions of OSL time zeroing. References Okumura, T., and Shitaoka, Y., 2011. Engineering Geology of Japan, No. 1, 5-17. Hiraga, S., Yoshimoto, A., and

  16. Two-way crossover comparison of insulin glargine and insulin detemir in basal-bolus therapy using continuous glucose monitoring

    Directory of Open Access Journals (Sweden)

    Abe S

    2011-07-01

    Full Text Available Shinya Abe1,2, Gaku Inoue1,2, Satoru Yamada1,3, Junichiro Irie1,3, Hiroyuki Nojima2, Kaoru Tsuyusaki2, Kensuke Usui2, Koichiro Atsuda2, Toshikazu Yamanouchi41Diabetes Center, Kitasato Institute Hospital, 2Center for Clinical Pharmacy and Clinical Sciences, Kitasato University, 3Department of Internal Medicine, Keio University School of Medicine, 4Department of Internal Medicine, University of Teikyo School of Medicine, Tokyo, JapanObjective: This study aimed to compare the glucose-lowering effect and glycemic variability of insulin glargine with those of insulin detemir.Material and methods: This was an open-label, single-center, randomized, two-way crossover study in patients with diabetes on basal-bolus insulin therapy, with neutral protamine Hagedorn (NPH insulin as basal insulin. Patients switched from NPH insulin to a course either of insulin glargine followed by insulin detemir, or insulin detemir followed by insulin glargine, continuing the same dose of the prior bolus of insulin. To evaluate the glucose-lowering effect, daily glycemic profiles were recorded for 72 hours by continuous glucose monitoring (CGM in an outpatient setting. The mean amplitude of glycemic excursions, standard deviation (SD, and the mean of daily difference (MODD were used to assess intraday and day-to-day glycemic variability.Results: Eleven patients were enrolled and nine completed the study. Mean blood glucose calculated from CGM values was significantly lower with insulin glargine compared with insulin detemir (9.6 ± 2.4 mmol/L versus 10.4 ± 2.8 mmol/L, P = 0.038. The SD was significantly lower with insulin glargine versus insulin detemir (2.5 ± 0.9 mmol/L vs 3.5 ± 1.6 mmol/L, P = 0.011. The MODD value was significantly lower with insulin glargine than with insulin detemir (2.2 ± 1.1 mmol/L vs 3.6 ± 1.7 mmol/L, P = 0.011. There was no significant difference between the two insulin analogs in terms of hypoglycemia.Conclusion: This study suggests that

  17. Fault pseudotachylyte: a coseismic lightning rod

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    Ferre, E. C.; Conder, J. A.; MathanaSekaran, N.; Geissman, J. W.

    2013-12-01

    The electrical conductivity of fault rocks varies considerably during an earthquake due to catastrophic physical changes, such as cataclastic deformation and frictional melting. We model independently the role of each parameter affecting electrical conductivity for a rock of granitic composition with an initial electrical conductivity s = 6.25 x 10^-7 S/m at 300 K and a density d = 2.64 x 10^3 kg/m3. In dry, unfractured rock, the electrical conductivity increases with temperature by one order of magnitude between 300 and 1300 K. Above 1300 K, partial melting generally takes place and the electrical conductivity drastically increases because metallic conduction prevails in a melt. Complex phase transitions, involving hematite, maghemite and magnetite, are responsible for discrete changes in electrical conductivity as a function of temperature. As the number and width of fractures increases towards the fault core and during slip, due to high strain rates (10^-2 m/s), the porosity also increases. The electrical conductivity can be modeled using a variation of Archie's Law. Our model assumes an increase in porosity from 0.2 to 2.0 %, similar to that observed for both the Nojima and the Soultz fault, which cut granites, and a fluid conductivity of Sw = 0.5 S/m, consistent with conductivity of fluids commonly present at depths of 2000 m. An increase in electrical conductivity by two orders of magnitude is predicted. Finally, the electrical conductivity of a mixture of solid rock and silicate melt is a composite of the electrical properties of both components. The electrical conductivity of the silicate melt results from metallic conduction and varies considerably with melt temperature. During seismic slip, the solid rock temperature is considered constant due to the low thermal conductivity of granitic rocks. Our model, a variant of the brick layer model of Partzsch et al. (2000), reveals another cause for the rise in electrical conductivity due to increasing abundance