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Sample records for butsuri tansa gakkai

  1. Future petroleum geophysicists and SEGJ; Sekiyu gyokai ni okeru butsuri tansa gijutsusha no shoraizo to Butsuri Tansa Gakkai eno kitai

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    Takahashi, A. [Japan Petroleum Exploration Corp., Tokyo (Japan)

    1998-08-01

    This paper describes future petroleum geophysicists and an anticipation to SEGJ (The Society of Exploration Geophysicists of Japan). Among various elemental technologies, it is undoubted that three-dimensional seismic exploration would be a main technology for prospecting petroleum gas. In the early stage of three-dimensional exploration, an improvement of accuracy for geological evaluation was a major purpose based on the successful exploratory drilling. In the 1990`s, some companies have a policy in which three-dimensional exploration is initially employed especially for the marine seismic prospecting as a major exploration technology. Since simple structures have been already prospected, it is required to prospect more complicated traps with higher accuracy. It is also required to shorten the turnaround time from the initial prospecting to the start of production. Furthermore, the three-dimensional exploration is used as a control technology for advancing the recovery by improving the accuracy of reservoir management. It is required for the geophysicists to have wide knowledge with keeping original exploration technologies. 2 refs.

  2. Proceedings of the 95th SEGJ Conference; Butsuri tansa gakkai dai 95 kai (1996 nendo shuki) gakujutsu koenkai koen ronbunshu

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    NONE

    1996-10-01

    This is a proceedings of the 95th SEGJ (The Society of Exploration Geophysicists of Japan) Conference (fall 1996). The number of the papers made public totaled 72: 6 in seismic survey processing; 11 in seismic survey; 7 in ground vibration; 5 in strong magnetic force; 7 in logging/underground measurement; 6 in the IP method and others; 5 in spontaneous potential/streaming potential; 6 in electrical prospecting; 6 in tomography; 5 in electromagnetic method; 8 in time-domain electromagnetic method/radar. As for the seismic survey, reported were the following papers titled An experiment of exploration using the active-faults exploration system; Detection of traveltime delay caused by dilation of an artificial fracture due to pressurization; Faults survey by 3D reflection seismics; etc. As to the ground vibration, Applicability of the spatial autocorrelation method for estimation of basement structure in Kanto Plain-Array measurements of microtremors close to the Iwatsuki and Shimousa Deep Borehole Observatory; Prediction of strong acceleration motion depended on focal mechanism; etc. With relation to the logging/underground measurement, Trial to active seismic while drilling; Estimation of fracture aperture using simulation technique: etc.

  3. Proceedings of the 94th SEGJ (The Society of Exploration Geophysicists of Japan) Conference; Butsuri tansa gakkai dai 94 kai (1996 nendo shunki) gakujutsu koenkai koen ronbunshu

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    NONE

    1996-05-01

    The fiscal 1996 SEGJ Conference was held in Tokyo during May 15-17, and 101 papers were reported. As for disaster prevention, the following were reported: Questionnaire investigation for the earthquake, Localization of b-values and maximum earthquakes, Cooperative measurements of microtremors in the north-eastern region of Nishinomiya City, Hyogo Pref., etc. As to elastic wave data recording and modeling data processing, Optimization of dynamite source depth for seismic surveys, Simulation of breakage of heterogeneous materials caused by detonative loading, etc. With relation to archeology, radar, and refraction method, Reexamining results of Iwatoyama tumulus by means of directive antenna, Application of geophysical method to investigation of old castle, etc. Concerning microtremors and surface waves, Estimation of shallow ground structure using short-period microtremors array observation, etc. Besides, papers were reported on electromagnetism, tomography, gravity/magnetism/numerical calculation, measurement while drilling, etc. Moreover, a symposium on underground structures in the Hanshin/Awaji area as viewed from geophysical exploration was held presenting nine papers.

  4. Proceeding of the 96th (spring, fiscal 1997) SEGJ Conference; Butsuri tansa gakkai dai 96 kai (1997 nendo shunki) gakujutsu koenkai koen ronbunshu

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    NONE

    1997-05-27

    This is a proceedings of the 96th SEGJ (The Society of Exploration Geophysicists of Japan). As for the well measurement, described were seismic survey and logging of geothermal wells and hot dry rock artificial reservoirs. As to the reflection method, analyzed were characteristics of seismic propagation and stratum structures. In the data processing, topics were on the neural network, stacking process and resolution, migration, etc. Concerning the electromagnetic method, research results were reported of TEM, CSAMT, EM tomography, MT method, etc. About the electrical exploration, introduced were resistivity structures by the electrical log, and exploration by the streaming potential or self-potential methods. Relating to the gravity/magnetic force exploration, reported were continuous gravity monitoring of geothermal activity, magnetic structures of rock, data on magnetic susceptibility, aeromagnetic survey, and remote sensing. As to the underground radar method, described were the survey of buried pipes and the inspection of fracture zones using the borehole radar, etc. With respect to the global system, the global structure was discussed from a global point of view. Additionally, reports were made on radioactive prospecting, seismometer observation, and ground motion.

  5. Chronology of petroleum geophysics; Sekiyu butsuri tansa nenpyo

    Energy Technology Data Exchange (ETDEWEB)

    Kametani, T.

    1996-10-01

    A table, chronology of petroleum geophysics in overseas and in Japan, has been prepared for the convenience of checking events, which are thought to be important as notable affairs in application, success, and technical innovation. In overseas, successes in the 1920s were remarkable, when the US modern geophysical exploration made a start. Successes in determining the position of exploratory drilling by means of the gravity torsion balance, fan shooting seismic refraction method, and seismic reflection method occurred one after another. The USA has kept its situation stably as the number one by the seismic reflection method occurred most lately, and its life has been further elongated by adopting digital techniques. The CDP technique which became to be used simultaneously, and the seismic sources without using explosives, such as vibro-seismic source and air gun, extended the success of digital techniques drastically. In the future, the progress of 3-D exploration technology is expected. In Japan, about 18 years lag in the seismic reflection method is observed when compared with the USA. Japan has provided leading techniques in the shallow layer seismic reflection method and S-wave exploration. 40 refs., 1 tab.

  6. Geotechnology for groundwater and salinisation soil using geophysical prospecting; Butsuri tansa wo mochiita chikasui enrui dojo no tansa gijutsu

    Energy Technology Data Exchange (ETDEWEB)

    Chiba, A. [Sumitomo Metal Industries, Ltd., Osaka (Japan); Imaizumi, M.; Takeuchi, M. [National Research Institute of Agricultural Engineering, Tsukuba (Japan)

    1997-12-01

    This paper takes a general view of geophysical prospecting on groundwater and salinisation soil. It also explains the following examples of prospecting: an example of pursuing movement of saline water lump charged with a tracer by using a specific resistance monitor, as a monitoring survey being a representative example of `visualization of movement` expected as a direction to which physical prospecting should proceed in the future, an example of elucidating distribution of soil salts vertically and two-dimensionally by using the electromagnetic exploration method, and an example of surveying distribution of three-dimensional water permeation coefficients by utilizing geophysical prospecting systems, as an example of estimating property values from geophysical prospecting. Electrical prospecting has been used as an exploration method related to groundwater, whereas its method has been increasing the diversity, such as from vertical exploration to high-density horizontal exploration and tomography. Noticeable progress can also be seen in electromagnetic exploration and logging techniques. In addition, what is demanded in application of physical prospecting to groundwater field may include visualization of ground water flow, more precise estimation of hydraulic constants, and complement of their distribution. 22 refs., 21 figs., 3 tabs.

  7. Geophysical characteristics of active faults in Hanshin district; Katsudanso chosa eno butsuri tansa no tekiyosei

    Energy Technology Data Exchange (ETDEWEB)

    Koreishi, Y.; Fujita, J.; Nakahigashi, H.; Asakawa, S.; Senna, S.; Ishigaki, K. [Dia Consultants Company, Tokyo (Japan)

    1996-05-01

    This paper reports the result of experiments on applicability of the geophysical investigation methods described below to investigation on active faults. The experiments were carried out in the vicinity of trenches excavated along the Nojima fault in Awaji Island and the Arima-Takatsuki tectonic line on the northern edge of the Osaka plains. Underground radar investigation is capable of identifying positions and shapes of faults and detecting difference of several ten centimeters in the levels of geological strata by applying such processing as velocity filter migration to original records that are affected largely by multiple reflections. Two-dimensional specific resistance investigation can recognize the remarkably abnormal structures in specific resistance if a clay stratum exists along a fault, and can identify fault positions and apparent inclination of faults. Investigation using S-wave reflection in a very shallow ground bed may be capable of verifying precisely fault positions if there is a noticeable change in a structure with a fault as a boundary. However, if the displacement is small, the method can identify only some signs that suggest existence of a fault. 1 ref., 4 figs., 1 tab.

  8. Geophysical exploration in environmental engineering; Kankyo engineering ni okeru butsuri tansa

    Energy Technology Data Exchange (ETDEWEB)

    Shima, H. [OYO Corp., Tokyo (Japan)

    1997-12-01

    This paper describes underground environmental issues to which geophysical exploration can be applied. Especially, ground pollution, waste treatment and unexploded ordnance (mine) detection are discussed by considering worldwide technology trends through examples in Japan and the USA. Since environmental surveys are generally conducted for regional and rather shallow ground, rapidity, economy and high resolution are required for geophysical exploration. In response to these demands, a mapping system using capacitor electrodes and a complex resistivity method for detecting organic compounds are promising for the electrical prospecting. A shallow electromagnetic method is being standardized for the electromagnetic prospecting. A cesium magnetic gradient meter is also being standardized for the magnetic prospecting. An underground radar, seismic prospecting, and gravitational prospecting are also applied to some grounds. Prospecting of pollution sources, high- and low-concentration ground pollution, monitoring of pollutant removal, soundness survey of water barrier in management-type waste treatment place, and detection of unexploded ordnance are illustrated for the examples. 15 refs., 10 figs., 4 tabs.

  9. Role of geophysical exploration for civil engineering; Doboku chosa ni okeru butsuri tansa no yakuwari

    Energy Technology Data Exchange (ETDEWEB)

    Tanaka, S.; Sato, S. [OYO Corp., Tokyo (Japan)

    1997-12-01

    This paper describes the current status of applying geophysical exploration to civil engineering works, application examples of latest geophysical exploration technologies in typical civil engineering fields (dams, tunnels, banks, and civil engineering works in urban areas), and of geophysical exploration technologies specially devised at civil engineering work sites. The applications include utilization in rock classification and weathering division, estimation of grouting effect and its injection scope, determination of loosening as a result of tunnel excavation, utilization of the relationship between S-wave velocity and N-value revealed by the standard penetration test, and tunnel front exploration. A well logging technique utilizing boring holes is available as a latest technology. Tomography technology using elastic waves, specific resistance and radar has its application increased as it is used in dams, tunnels, and foundations of other important structures. Attempts are made on application of explorations using the shallow bed reflection method and three-dimensional exploration method. Frequently used technologies include seismic exploration using the refraction method for dams, high-density electric exploration for tunnels, electric exploration for banking, and PS logging using the suspension method for structure foundations. 30 refs., 13 figs., 5 tabs.

  10. Geophysical survey on trench excavation of active faults; Butsuri tansa to katsudanso trench chosa

    Energy Technology Data Exchange (ETDEWEB)

    Kanayama, S.; Hasegawa, S.; Tsuruta, S. [Shikoku Research Inst. Inc., Kagawa (Japan); Kawakami, H. [Yonden Consultants Co. Inc., Kagawa (Japan)

    1997-12-01

    This paper describes cases of geophysical survey used for investigation on a few active faults, and future requirements thereof to help develop active fault surveys. Seismic exploration using the reflection method on the Nagao fault revealed distinct existence of a reverse fault with southward inclination of about 50 degrees. A crush zone caused by this fault was recognized also in the granite base. A few small crush zones in reverse direction to the main fault were found in granite in upper base of the fault, which were thought secondary to activities of the main fault. Seismic exploration using the reflection method was performed on the Iyo fault in the central tectonic line to identify underground structures of the Iyo fault and the Gunchu fault, by which the location of the Iyo fault was verified. The Chichio fault in the central tectonic line was explored by using the {rho}a-{rho}u method, and the Okamura fault in the central tectonic line by using the specific resistance imaging method. The length of a fault per action, which is always a problem, or the problem of fault groups acting associatively could not be discussed if structural analysis of ground of great depths is omitted, when estimating scales of earthquakes from active faults. 18 refs., 10 figs.

  11. Application of geophysical methods to investigation of old castle, especially of the moat; Joshi no chosa ni okeru butsuri tansa no tekiyo (horiato no tansa)

    Energy Technology Data Exchange (ETDEWEB)

    Tanaka, A.; Karube, F.; Kobayashi, M.; Toge, M. [OYO Corp., Tokyo (Japan)

    1996-05-01

    An explanation is made about the application of geophysical methods to the investigation of the ruins of old castles especially of their moats. Techniques currently in use for exploration of the ruins of castles are mainly underground radar exploration and electric exploration. The underground radar method sends electromagnetic waves through the ground and receives the reflection for a high-precision exploration of the layers shallow in the ground. Therefore, this method is suitable for probing the ruins of castles relatively shallow in the flat land, hills, and mountains. The electric method (resistivity image method) do the probing by use of the two-electrode arrangement, performs inverse analysis on the basis of the obtained data for the determination of the underground resistivity distribution, and displays the distribution in an image easy to read. This method, when there is a great separation between the two electrodes, explores relatively deep into the ground. Thanks to this feature, this method is effective in probing relatively wide and deep ruins of moats, that is, the ruins of moats of castles built in later years, especially of those then filled with water. 2 refs., 5 figs.

  12. Geophysical exploration for preserving archaeological site in construction projects; Kokudo no kaihatsu to iseki hozon no tame no butsuri tansa

    Energy Technology Data Exchange (ETDEWEB)

    Karube, H. [OYO Corp., Tokyo (Japan)

    1997-12-01

    When considering more harmonious ways of mutual existence of development and preservation of buried cultural assets subjected to today`s social demand, how far can exploration of archeological sites make a contribution. This paper discusses the possibility thereof while introducing some examples of explorations done in recent years. The geophysical exploration includes the following groups of ancient tombs (field improvement operations using underground radar), remains of ditches around ancient temples (construction of golf courses using underground radar and electric exploration), castles in the modern period (urban redevelopment using electric exploration and underground radar), castles in the medieval period (improvement of parks in hilly areas using underground radar), moated settlements (improvement of historic site parks using underground radar and electric exploration), remains of settlements (land improvement operations using underground radar), two kiln remains (highway construction using magnetic exploration), bronze wares (road construction using electromagnetic method and metal exploration), and remains of stream sluices in the modern period (development of four rivers using underground radar, specific resistance imaging method, and gravity exploration). It is intended to take up as a theme for the future development issues that how archeological conceptions should be `fused` into scientific technologies. 5 refs., 20 figs., 5 tabs.

  13. Fracture mapping in rock slope using geophysical instruments; Butsuri tansa ni yoru ganban shamennai no kiretsu bunpu hyoka

    Energy Technology Data Exchange (ETDEWEB)

    Kurahashi, T.; Inazaki, T. [Public Works Research Institute, Tsukuba (Japan); Watanabe, S. [Geological Survey of Japan, Tsukuba (Japan)

    1997-05-27

    An attempt was made to visualize distribution of cracks in a rock slope by applying geophysical survey onto a rock slope. Geophysical logging and seismic survey using the reflection method were used as the methods for the geophysical survey. The rock slope subjected to the survey is located in a gorge along the Yoshino river in Yamashiro Town, Tokushima Prefecture. The slope has a width of 25 m and a height of 30 m. Its overhang in a nose form may has a possibility of causing collapse due to sliding. Cracks developed by horizontal schistosity were detected by performing geophysical logging on VSP, calipers, natural gamma-ray spectra, temperature and borehole in a borehole drilled vertically from the top of the slope. The seismic survey using the reflection method detected the cracks by emphasizing joints in the perpendicular direction. A possibility was shown to visualize the crack distribution with high resolution by using the above geophysical survey on the rock slope. In order to detect the crack distribution with still higher resolution, development into a three-dimensional exploration in the future is desired, not to speak of improvement in signal receivers, and discussions on geometry. 1 ref., 6 figs.

  14. Case study of geostructural prospect of a tunnel by using geophysical methods; Butsuri tansa ni yoru tunnel chisan yosoku to jissai

    Energy Technology Data Exchange (ETDEWEB)

    Ueda, H. [Japan Railway Construction Public Corp., Tokyo (Japan); Kawakami, J. [Taisei Construction Corp., Tokyo (Japan); Nagasue, I.; Hiwatashi, S.; Wakuno, M. [Oyo Corp., Tokyo (Japan)

    1997-05-27

    A preliminary survey was carried out by combining elastic wave exploration (using a refraction method) and electrical exploration (using a resistivity imaging method) on a long tunnel planned in a granite distributed area. This paper describes a case of verifying geological condition in the area by using a trial survey well and horizontal boring. This tunnel goes through the Seburi mountainous area on the border of Fukuoka Prefecture and Saga Prefecture for a total distance of 12 km. The refraction method and the resistivity imaging method were selected from the necessity of identifying the weathering condition in natural ground, and distributions of fault crush zones and underground water in a section extending 560 m from the well entrance. As a result of comparing the natural ground condition interpreted from the geophysical survey results with the construction records, the fault was detected as a cracked or deformed section in the part where the resistivity value changes abruptly or where the resistivity is low. The tunnel natural ground classification showed a good correspondence with the elastic wave velocities. The largest flooding section showed a good agreement with the section where the resistivity changes suddenly to a lateral direction. Thus, the geological information interpreted from both surveys presented a good correspondence with the construction records, leading to a judgment that the prediction is possible. 3 refs., 4 figs., 5 tabs.

  15. 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.

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

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    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.

  17. Rostros de una diáspora. Comunidad japonesa y religiosidad en la Soka Gakkai Internacional (Argentina

    Directory of Open Access Journals (Sweden)

    Mariano Gancedo

    2015-06-01

    Full Text Available Resumen En este artículo se analizan aspectos concernientes a la inmigración japonesa en Argentina, poniendo énfasis en el fenómeno social y religioso que configura la Soka Gakkai Internacional (SGI. El objetivo es proponer una lectura interpretativa enfocada en los discursos y prácticas inscriptos en las actividades y en la filosofía que promueve la SGI. El propósito es ofrecer una lectura del fenómeno donde éste representa, entre otras cosas, tanto una reserva de valores culturales como un modo de visibilización social desarrollado por parte de la comunidad japonesa en la Argentina.

  18. A Study on Firm Mergers One of the Financial Structure Strengthening Precautions: Tansaş-Migros Merger

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    Berna YILDIZ TULUM

    2009-06-01

    Full Text Available In last years, it is examined that there is an increase in the number of firms that faces with financial distress in both our country and in west. In terms of social and economic results, the financial distress of the firms is a very big problem. Consequently, financial distress prediction carries an very big importance. By forecasting the probability of facing with financial distress, the firms can be able to catch the opportunity of taking necessary financial structure strengthening precautions. Firm mergers is one of the many financial structure strengthening precautions. This study aims to improve models that provides the prediction of financial distress 1-3 years before in firms that is active in retail sector and have transactions in IMKB by showing the firm mergers which is one of the financial structure strengthening precautions in Tansaş and Migros Merger in retail sector.

  19. Basic surveys for developing coal resources in fiscal 1989. A report on re-analysis of on-shore physical exploration in the Ariake sea area; 1989 nendo sekitan shigen kaihatsu kiso chosa. Ariakekai chiiki kaijo butsuri tansa saikaiseki hokokusho

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    NONE

    1990-03-01

    The present survey was intended to enhance accuracy of analysis and interpretation of the geological structures in the northern and north-western parts of this area, and the status of coal seam existence. The survey used the most part of the earthquake exploration data obtained in fiscal 1988, and parts of the earthquake exploration data obtained in fiscal 1983 and fiscal 1985 in the vicinities thereof, and incorporated a new treatment method to perform re-analysis. The quaternary deposit seam has thickness of 80 to 610 m, and the Palaeogene deposit seam has thickness of 600 to 1600 m as a whole. The structure of the foundation bed is nearly parallel with the structure of the top of a coal seam in the Palaeogene deposit seam, having a distance of 300 m between the seams. The surveys combining the test drillings having been done to date and the physical exploration estimates that the coal seam groups are distributed over the entire area of Ariake Sea. Possibility has heightened, that the coal seam groups may spread over the land area. The collapsed fault passing east-west the northern most area of the Ariake Sea and having drop of 200 to 300 m forms the northern boundary of the Miike coal field. However, the coal seam groups are estimated to spread north of the coal field as a sedimentary basin, and continue to the northern side of the fault. (NEDO)

  20. Borehole geophysics for delineating the geological structure in the Sakonishi prospect, the Hida area, Japan; Hida chiiki Sako nishi chiku ni okeru boring ko riyo butsuri tansa ni yoru chishitsu kozo kaiseki

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    Katayama, H.; Hishida, H.; Yoshioka, K. [Metal Mining Agency of Japan, Tokyo (Japan)

    1997-05-27

    In order to discuss effectiveness of physical exploration in the Sakonishi prospect in the Hida area, physical exploration was carried out by utilizing bored wells. This area contains the Kamioka mine, one of the major base metal mines in Japan, where electrical exploration has been attempted several times in the past. No effective results have been obtained, however, because specific resistance contrast between mine beds and base rocks is too small, and the topography is too steep making site workability inferior. As part of the investigations on geological structures over wide areas, electrical logging (specific resistance and natural potential) was performed in fiscal 1995 and 1996 by utilizing the boreholes. Induced polarization logging was also conducted on the same boreholes. A traverse line on the ground with a length of 600 m and boreholes were used to execute specific resistance tomography. Clear extraction was possible on a fault structure which is thought related with limestone distribution and mine bed creation. However, it was not possible to identify upward continuity of zinc ores expected in the exploration. Because of not large a specific resistance contrast between zinc ores and base rocks, it is difficult to find mine bed locations only from the information on the specific resistance. 5 refs., 5 figs., 1 tab.

  1. Electric and VLF-MT survey of Tegatayama tunnel; Tegatayama tunnel no denki tansa oyobi VLF tansa

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    Nishitani, T. [Akita University, Akita (Japan). Mining College

    1997-05-27

    To survey the structure at the depth between 20 and 30 m, field tests were conducted by means of vertical electric and VFL-MT (magnetotelluric) survey. Tegatayama tunnel has a total length of 276 m, width of 7.5 m, and height of 4.7 m, and the depth from the surface is about 28 m near the top of mountain. Near the tunnel, the thickness of surface soil is about 60 cm, which consists of clay soil including soft mudstone gravel. It was found that terrace deposit is distributed up to the depth of 8 m, and that mudstone is distributed below the depth of 8 m. Weighted four-electrode method was adopted for the vertical electrical survey. Measurements were conducted at the immediately above the tunnel, 10 m apart from the center of tunnel in the right and left, and 20 m apart from the center in the east. For the VLF-MT method, component of frequency 22.2 kHz was used. As a result of the tests, it was difficult to illustrate the existence of tunnel from the vertical electrical survey only at one point. Feature of the tunnel could be well illustrated by means of the VLF-MT method. 3 refs., 9 figs.

  2. Experiment of exploration using the active-faults exploration system; Katsudanso tansa system wo mochiita chika tansa jikken

    Energy Technology Data Exchange (ETDEWEB)

    Mikada, H.; Sato, H.; Iwasaki, T.; Hirata, N. [The University of Tokyo, Tokyo (Japan). Earthquake Research Institute; Ikeda, Y. [The University of Tokyo, Tokyo (Japan). Faculty of Science; Ikawa, T.; Kawabe, Y.; Aoki, Y. [JAPEX Geoscience Institute, Tokyo (Japan)

    1996-10-01

    A system for exploration of active-faults by seismic reflection profiling method was introduced at Earthquake Research Institute, University of Tokyo. A test-run was conducted to check the performance of this system at Ranzan, Saitama Prefecture. This paper describes the confirmed performance of mini-VIB as a wide band frequency seismic source, the quality of data obtained using a digital data acquisition system, and problems for data processing of fault exploration in the future. For the test-run at Ranzan, two-dimensional exploration was conducted by the quasi-three-dimensional data acquisition method using three geophones of 8 Hz, 28 Hz, and 40 Hz, simply arranged in parallel on the measurement line. Using an active seismic vibrator, mini-VIB, data acquisition of faults in the wide band frequency was achieved, which would result in the highly accurate imaging. Operation of data acquisition and processing systems is easy, and the system can be also used as a kind of black box. The existing methods are to be used sufficiently as a tool for imaging of faults. Further research for accumulating experience may become necessary toward the extension of the system expected in the future. 5 refs., 6 figs.

  3. Examination of Existing Shear Wave Velocity and Shear Modulus Correlations in Soils

    Science.gov (United States)

    1987-09-01

    in Terms of Characteristic Indices of Soil," Butsuri- Tanko (Geophysical Exploration) (in Japanese), Vol 29, No. 4, pp 34-41. . 1978a. "Empirical Shear...34Physical Background of the Statistically Obtained S-Wave Velocity Equation in Terms of Soil Indexes," Butsuri- Tanko (Geophysical Explo- ration) (in Japanese

  4. Interpretation method for hot spring well logging data; Onsensei no butsuri kenso

    Energy Technology Data Exchange (ETDEWEB)

    Fujiwara, C. [Techno Rent Co. Ltd., Tokyo (Japan); Sato, T. [Shiga Boring Co., Nagano (Japan); Matsuoka, K. [Geophysical Surveying and Consulting Co. Ltd., Tokyo (Japan); Aizawa, K. [Tone Co. Ltd., Tokyo (Japan)

    1996-10-01

    Basic problems in the interpretation of hot spring well logging data are discussed, and report is made on the result of effective analysis obtained experimentally based on many on-the-spot data. Interpretation of hydraulic properties of hot spring aquifers is discussed based on electrical and temperature logging data obtained at hot spring wells in Japan. As a result of many case studies, it is found that a reservoir can be evaluated roughly by the value of the specific resistance coefficient of the bed even when there is no temperature abnormality on the logging curve. It has been known by ground water investigation that the specific resistance of aquifer is almost proportionate to the specific resistance of ground water, but such simple relationship can not be found for hot spring wells because of extremely large electric conductivity of hot water, profound alteration of beds, or fracture development. However, it is found from the case study that the specific resistance coefficient of the bed is significant for the evaluation of reservoirs. 10 refs., 9 figs.

  5. Religión y espiritualidad, ¿dos modelos enfrentados?. Trayectorias poscatólicas entre budistas Soka Gakkai

    Directory of Open Access Journals (Sweden)

    Cornejo, Mónica

    2012-08-01

    Full Text Available In the context of the privatization of religion, still ongoing, many contemporary religious biographies seem to be motivated by the individual search for a religious alternative far away from the repertoires of beliefs, rituals and institutions of traditional religion. Following the increasing use of this term by many social actors at least since the sixties of the twentieth century, part of the Sociology of Religion has referred to the alternative religiosity as Spirituality (Wood 2009 (Heelas 2008 (McGuire 2008 (Flanagan 2007 (Giordan 2007. The new models of spirituality account both for the decay of traditional forms of religiosity (based on the community of faith, the participation in collective rituals and the congregational identity and for the spreading of a new spiritual subjectivism, whose high individualism have moved some authors to assert that a reconstitution of collective religiosity is impossible, as Steve Bruce (1996 and Daniele Hervieu-Leger (2003 have argued. This paper tries to explore the possibilities of this theoretical framework analyzing some discourses, discourses and practices of Buddhist converts in Spain, who have previously developed an extensive spiritual ride through several varieties of the so-called New Age milieu, the most important style of religious fragmentation and subjective revolution in the religious fields.

    En el contexto de la privatización de lo religioso aún en curso, muchas biografías religiosas contemporáneas parecen estar motivadas por la búsqueda individualista de una religiosidad alternativa a los repertorios de creencias, rituales e instituciones religiosas tradicionales. Siguiendo el uso creciente de este término por parte de numerosos actores sociales, al menos desde la década de los sesenta del siglo XX, una parte de la Sociología de la Religión se ha referido a esta religiosidad alternativa como “espiritualidad” (Wood 2009 (Heelas 2008 (McGuire 2008 (Flanagan 2007 (Giordan 2007. Los nuevos modelos de espiritualidad dan cuenta del decaimiento de aquellas formas de religiosidad en las que primaba la comunidad de fe, la participación en la ritualidad colectiva, la membresía como referente identitario. mientras se abre paso a una atomización, un subjetivismo y relativismo tales, que la reconstitución de una religiosidad colectiva parece imposible, como han sostenido Steve Bruce (1996 o daniele Hervieu-Leger (2003. Para explorar las posibilidades de este marco teórico se propone aquí el análisis de los discursos y prácticas de conversos budistas que previamente han desarrollado un extenso itinerario espiritual por diversas variedades de la llamada Nueva Era, referente por antonomasia de la fragmentación religiosa y de la revolución subjetiva de lo religioso.

  6. State of the art of aeromagnetic survey. High-resolution aeromagnetic survey; Kuchu jiki tansa no saizensen. Kobunkaino kuchu jiki tansa

    Energy Technology Data Exchange (ETDEWEB)

    Okuma, S.; Makino, M.; Morijiri, R.; Nakatsuka, T. [Geological Survey of Japan, Tsukuba (Japan)

    1997-04-01

    This paper describes the technology trend of aeromagnetic survey in Japan and overseas countries. For the aeromagnetic survey, intensity of geomagnetism (total force) is measured in the air using a probe with a magnetometer. Recently, low-altitude high-density aeromagnetic survey can be done with a support of positioning technique using GPS (global positioning system). In Japan, the aeromagnetic survey is utilized for the surveys of latent active faults and internal structure of volcanoes. In the U.S., magnetometers developed for the detection of submarines were utilized for the aeromagnetic survey after the war. At the initial stage, they were used for the survey of hydrocarbon resources. In addition, they have been used for the survey of mineral resources, and the survey covers the whole US mainland. A data base of magnetic anomaly has been also constructed. In the West Coast, the surveys of latent active faults and internal structure of volcanoes are conducted to reduce the disasters due to earthquakes and volcanic activities. In Canada and Australia, the aeromagnetic surveys are positively performed for the exploration of mineral resources. 22 refs., 9 figs.

  7. Survey of ancient river trace in Hotta stockade site using vertical electrical method; Denki tansa (suichoku tansa) ni yoru futsudenssaku sekinei no kasenseki chosa

    Energy Technology Data Exchange (ETDEWEB)

    Nishitani, Tadasho; Takano, Kasumi; Matsuno, Katsutoshi [Akita University, Akita (Japan); Kodama, Jun

    1999-02-01

    The vertical electric prospecting was carried out at a high density to investigate the characteristics of ancient river trace in Hotta stockade site, and therefore the ancient river trace at the final stage, the distribution of sand soil and gravel layers due to flooding were clarified. It has been known that the rive terrace was roughly divided into two and merged into one near the government office trace. When estimating the river trace at the final stage, it was also found that the watercourse was divided into two on the east side. It was considered that there were two watercourses existing simultaneously or the watercourse had changed and moved. (translated by NEDO)

  8. Subsurface geology by shallow seismic reflection survey and microgravity survey in Kobe area; Senso hanshaho danseiha tansa oyobi seimitsu juryoku tansa ni yoru Kobe chiiki no chika chishitsu

    Energy Technology Data Exchange (ETDEWEB)

    Endo, H.; Makino, M.; Murata, Y.; Watanabe, S. [Geological Survey of Japan, Tsukuba (Japan)

    1996-05-01

    This paper reports discussions on subsurface structure of the Kobe area by means of microgravity survey. A Bouguer anomaly distribution graph was obtained (which is close to a near straight line) by measuring the gravity at measurement points with an interval of about 25 m along a traverse line (with a total length of about 1.7 km) in an approximately NNW-SSE direction crossing the downtown of the city of Kobe. Viewing the residuals to a straight line linking the values at both ends of the traverse line revealed that the gradient in the Bouguer anomaly distribution changes as if it is bent at a point near the center of the traverse line as a boundary. Deriving the residuals from fine changes seen in a distribution graph for the residuals made clear that this residual distribution has two discontinuous points. The paper indicates that the bending point in the former case corresponds to a reverse fault in a base bed of a flat land as compared with the result of model calculation on the base structure and gravity distribution. The discontinuous points in the latter case agree with positions of fault distribution derived by a reflection elastic wave survey. 6 refs., 4 figs.

  9. Feasibility study of various geophysical methods at the Nojima fault; Nojima danso ni okeru kakushu butsuri tansaho no tekiyo jikken

    Energy Technology Data Exchange (ETDEWEB)

    Takahashi, T.; Nozaki, K.; Shima, H.; Yamane, M.; Igarashi, T. [OYO Corp., Tokyo (Japan)

    1996-05-01

    This paper reports a feasibility study of various geophysical methods at the Nojima fault. A shallow bed investigation (to a depth of several ten meters) was performed at the Nojima-Hirabayashi area, a very shallow bed investigation (to a depth of several meters), a shallow bed investigation and a medium depth bed investigation (to a depth of several hundred meters) at the Kokura area, and a very shallow bed investigation at the Nashimoto area. Combinations of two to four investigation methods were used according to the objectives and depths of the investigations at each area. The combinations were selected from the following methods: seismic investigations (P-wave reflection and N-wave reflection methods), electric investigation using the IP image method, electromagnetic investigation using the VLF method, underground radar investigation, micro-gravity investigation, and gravity investigation. The result may be summarized as follows: in places where a fault forms a boundary between base rocks and a sedimentation bed, it was possible to identify clearly position of the fault, and estimate inclination angles and vertical shift; and during the medium depth investigation at the Kokura area, identification was made on a geological structure (deformation of a sedimentation bed above the base bed) which is important in verifying the nature of an active fault. 2 refs., 5 figs., 1 tab.

  10. Using of the geophysical methods to an investigation in city; Toshi ni okeru butsuri tansaho no tekiyo

    Energy Technology Data Exchange (ETDEWEB)

    Sato, S. [Oyo Corp., Tokyo (Japan)

    1995-02-10

    Some of the exploration methods are taken up out of the geophysical methods, which have made drastic change by technological advancement, to discuss their technological development and application in cities. The elastic wave exploration is classified into the refraction method which uses refracted waves and the reflection method which utilizes reflected waves. Shallow reflection method allows visual observation of the complex underground structure, and is an excellent exploration method which provides highly accurate data. There are many types in the electrical exploration. New exploration methods have been developed as a result of improvement in the computer performance, advancement in the technology of numerical analysis, and improvement in the performance of exploration equipment, and they are being applied to the electrical exploration in many fields including tunnel and dam construction works. Geotomography is an application of the technology of medical tomography to ground exploration. Underground radar method is a method of investigating the ground structure by radiating electromagnetic waves from the ground surface in similar way to that of the reflection method and capturing the reflected waves from underground. 8 refs., 7 figs.

  11. Groundwater exploration by self-potential method; Shizen den`iho ni yoru chikasui tansa

    Energy Technology Data Exchange (ETDEWEB)

    Onaru, I.; Irie, S.; Mizunaga, H.; Ushijima, K. [Kyushu University, Fukuoka (Japan). Faculty of Engineering

    1997-05-27

    This paper describes results measured from the field experiments and data analysis of the groundwater exploration by self-potential method. The field survey was conducted in the vicinity of spring water source in the suburbs of Fukuoka City. For the field experiments, potential differences from the standard potential electrode set at the distance about 200 m were measured at multi-points, simultaneously. For the laboratory experiments, assuming that the groundwater flows in a permeable layer, streaming potential change was observed against the changes of flow rate and electrical conductivity. Thus, the generation of streaming potential was investigated. For the experiment using specimens obtained at the spring water source, the potential changed to negative and was stabilized in around -80 mV after 15 minutes. Numerical simulation was conducted by means of the three-dimensional finite difference method using parameters obtained from the laboratory experiments. From these results, the groundwater flow image could be obtained. It was also confirmed that the self-potential observed in the spring water source area was caused by the streaming potential. 11 refs., 9 figs.

  12. Magnetotelluric (MT) surveying in the Kakkonda geothermal area; Kakkonda chinetsu chiiki deno MT ho tansa jikken

    Energy Technology Data Exchange (ETDEWEB)

    Ogawa, Y.; Takakura, S. [Geological Survey of Japan, Tsukuba (Japan); Uchida, T. [New Energy and Industrial Technology Development Organization, Tokyo, (Japan)

    1997-05-27

    This paper describes the MT surveying conducted at the vicinity of a deep well (WD-1) in the Kakkonda geothermal area. For the MT surveying, the interval between measuring points was 300 m. Electric field dipole with a length of 300 m was given in the direction of traverse line, and that with a length of 50 m was given in the direction perpendicular to the line. Three components of magnetic field were measured using induction coil. Frequency band of the data was between 0.0005 Hz and 300 Hz. Characteristics of specific resistance model obtained from the MT surveying were illustrated. Low specific resistance zone less than 30 ohm-m was observed in the shallow zone below the altitude 0 m. This zone was comparable to the distribution of montmorillonite. High specific resistance anomaly was analyzed at the western half of the traverse line in the altitude between 0 m and -2000 m, which corresponded to the collective part of focuses. The bottom surface of the anomaly agreed well with the upper surface of neo-granite, i.e., the lower limits of earthquakes. Low specific resistance was observed in the altitude below -2000 m. 17 refs., 5 figs.

  13. Application of EM tomography to detect a buried pipe; EM tomography no maisetsukan tansa eno tekiyorei

    Energy Technology Data Exchange (ETDEWEB)

    Sakashita, S. [OYO Corp., Tokyo (Japan)

    1996-10-01

    EM tomography was applied to detect buried pipes. Underground radar exploration method is limited to 10m in depth. Positive use of bored holes is desirable, and in such case, magnetic logging based on the magnetic susceptibility (MS) contrast between buried body and surrounding ground is effective. The primary magnetic field is generated by coil current, and the secondary one is generated by the primary one responding to foreign bodies in the ground. Since the measured primary magnetic field of low frequency within 10Hz can be treated as static magnetic field responding to MS in the ground, it is useful to determine MS distributions. Since the measured magnetic field of high frequency within 100kHz can be treated as induction field responding to conductivity in the ground, it is useful to determine resistivity distributions. The EM tomography which can image both above distributions by using electromagnetic wave in a wide frequency range, was applied to detect buried pipes. The EM tomography could detect an buried foreign body of 3m in diameter at 10m in distance between bored holes. The theoretical equation for analysis was also derived. 5 refs., 9 figs., 1 tab.

  14. Present situation of underground cavity exploration. Romenka kudo tansa no genjo

    Energy Technology Data Exchange (ETDEWEB)

    Cho, K.; Koike, K. (Ministry of Construction, Tokyo (Japan))

    1994-03-25

    Due to many sinking accidents occurring in urban roads, a high-performance exploration vehicle was developed about three years ago and has been used to perform field investigations. The present report describes the outline covering the progress in its development and the results of cavity investigations. While electromagnetic waves, sound waves, vibrational waves, infrared rays have been used for non-destructive exploration of underground cavities, the present method adopts the electromagnetic underground radar system which observes the reflecting conditions of pulse electromagnetic waves radiated from an antenna to the underground at boundaries of layers different in dielectric factor. This device loaded on a reformed bus of medium-size has power of exploration depth of 1.2m, exploration width of 2m, and maximum exploration speed of 20km/h. According to the investigations on a total of 1600km since 1990, 175 cavities which include those reaching 15m[sup 2] in area and 2.3m in depth have been detected. The results of excavation immediately following detection showed a lot of information also on the causes of cavity generation. 7 figs., 1 tab.

  15. 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.

  16. New seismic source `BLASTER` for seismic survey; Hasaiyaku wo shingen to shite mochiita danseiha tansa

    Energy Technology Data Exchange (ETDEWEB)

    Koike, G.; Yoshikuni, Y. [OYO Corp., Tokyo (Japan)

    1996-10-01

    Built-up weight and vacuole have been conceived as seismic sources without using explosive. There have been problems that they have smaller energy to generate elastic wave than explosive, and that they have inferior working performance. Concrete crushing explosive is tried to use as a new seismic source. It is considered to possess rather large seismic generating energy, and it is easy to handle from the viewpoint of safety. Performance as seismic source and applicability to exploration works of this crushing explosive were compared with four kinds of seismic sources using dynamite, dropping weight, shot-pipe utilizing shot vacuole, and impact by wooden maul. When considered by the velocity amplitude, the seismic generating energy of the crushing explosive of 120 g is about one-fifth of dynamite of 100 g. Elastic wave generated includes less high frequency component than that by dynamite, and similar to that using seismic source without explosive, such as the weight dropping. The maximum seismic receiving distance obtained by the seismic generation was about 100 m. This was effective for the slope survey with the exploration depth between 20 m and 30 m. 1 ref., 9 figs., 2 tabs.

  17. Refraction experiment in the Kobe-Hanshin area; Kobe Hanshin kan ni okeru kussetsuho tansa

    Energy Technology Data Exchange (ETDEWEB)

    Koketsu, K. [The University of Tokyo, Tokyo (Japan). Earthquake Research Institute

    1996-05-01

    The refraction experiments were conducted to investigate the underground structures reaching the basement by analyzing the results of the artificial earthquakes the explosion earthquake research group produced in City of Kobe and the Hanshin District on December 12 to 15, 1995. Considering that noise level can exceed 1 mkine in an urban area even in the mid-night, the courses of traverse were drawn focusing on Points S2 through S4 and U1. The earthquake waves from Points S2 through S4 are generally low in amplitude. However, the major components of the signals have a dominant frequency exceeding 10Hz, which makes them distinguishable from urban noise having a lower frequency, contrary to the previous indication that such a low-amplitude wave might not be distinguishable. On the other hand, the signals from the explosion at Point 4 in Awaji Island cannot be distinguished in the urban area, even on the nearby course of traverse D. At present, the analytical group is organized to read various phases running and analyze the P-velocity structures. 2 refs., 10 figs., 1 tab.

  18. High resolution seismic refraction method (development and applications); Koseido kussetsuho jishin tansa no kaihatsu to tekiyorei

    Energy Technology Data Exchange (ETDEWEB)

    Hayashi, K.; Saito, H. [OYO Corp., Tokyo (Japan)

    1998-10-01

    Described herein are measurement/analysis procedures of the high-resolution seismic refraction method. Recently, use of explosives has been limited for many explorative activities. The measurement systems and waveform processing procedures described herein can minimize use of explosives and widen applicability of non-explosive seismic sources. The seismic refraction method is now advanced, e.g., to process large quantities of high-quality data, use tomographic algorithm and include analysis of vibration-receiving points in holes, and is applicable to grounds of complicated structures, for which the conventional method is difficult to use. The new method is aided by a personal computer to give the analysis results almost automatically, thereby establishing objectivity of the explorative results and securing data quality. The high-resolution seismic refraction method, aided by the new techniques of measurement/analysis, can now give the results in a much shorter time than the conventional one. 40 refs., 22 figs.

  19. 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.

  20. Application of wavelet transform to seismic data; Wavelet henkan no jishin tansa eno tekiyo

    Energy Technology Data Exchange (ETDEWEB)

    Nakagami, K.; Murayama, R.; Matsuoka, T. [Japan National Oil Corp., Tokyo (Japan)

    1996-05-01

    Introduced herein is the use of the wavelet transform in the field of seismic exploration. Among applications so far made, there are signal filtering, break point detection, data compression, and the solution of finite differential equations in the wavelet domain. In the field of data compression in particular, some examples of practical application have been introduced already. In seismic exploration, it is expected that the wavelet transform will separate signals and noises in data in a way different from the Fourier transform. The continuous wavelet transform displays time change in frequency easy to read, but is not suitable for the analysis and processing large quantities of data. On the other hand, the discrete wavelet transform, being an orthogonal transform, can handle large quantities of data. As compared with the conventional Fourier transform that handles only the frequency domain, the wavelet transform handles the time domain as well as the frequency domain, and therefore is more convenient in handling unsteady signals. 9 ref., 8 figs.

  1. Development of measurement apparatus for high resolution electrical surveys; Komitsudo denki tansa sokuteiki no kaihatsu

    Energy Technology Data Exchange (ETDEWEB)

    Moriuchi, H.; Matsuda, Y.; Shiokawa, Y. [Sumiko Consultants Co. Ltd., Tokyo (Japan); Uchino, Y. [Cosmic Co. Ltd., Tokyo (Japan)

    1996-05-01

    For the enforcement of the {rho}a-{rho}u survey method which is a type of high-density electrical survey, a multichannel resistivity measuring instrument has been developed. This instrument, in addition to the above, conducts resistivity tomography and various other kinds of high-density electrical survey. A potential produced by a low frequency rectangular current of 1Hz or lower outputted by the transmitter of this instrument is received and measured by the receiver connected to electrodes positioned at 100 or less locations. The receiver comprises a scanner that automatically switches from electrode to electrode, conditioner that processes signals, and controller. A transmitter of the standard design outputs a maximum voltage of 800V and maximum current of 2A, making a device suitable for probing 50 to several 100m-deep levels. The receiver is operated by a personal computer that the controller is provided with. The newly-developed apparatus succeeded in presenting high-precision images of the result of a {rho}a-{rho}u analysis for an apparent resistivity section and of the underground structure, verifying the high quality of the data collected by this apparatus. 10 refs., 5 figs., 1 tab.

  2. Archaeological prospecting by DEF method; Denkai zansaho ni yoru iseki tansa

    Energy Technology Data Exchange (ETDEWEB)

    Kishikawa, H.; Aono, T.; Tanaka, T.; Mizunaga, H. [Kyushu University, Fukuoka (Japan). Faculty of Engineering

    1996-05-01

    A study is made of a newly-developed differential electric field (DEF) method, wherein potentials between potential electrodes equidistant from a current electrode is measured for directly detecting the secondary potential attributable to an anomalous-resistivity body. In this method, a current is fed into the ground from a point source C1, and four potential electrodes, two each on the X-axis and Y-axis, are provided equidistant from the point source C1 for the measurement of the potentials in the directions of X and Y. Numerical experiments and field experiments in a playground were conducted for this DEF method, and it was found that this method is effective in detecting an anomalous-resistivity bodies (ruins, etc.) situated in a homogeneous medium or in a horizontal multi-layer structure, is capable of displaying anomalous vectors enabling the estimation of the direction from the observation point of the anomalous-resistivity body, improves on work efficiency over the conventional mapping method, enables the estimation of the boundary of the anomalous-resistivity body on the basis of the peak of the anomalous electric field residue on the display, and that the obtained data can be easily processed by use of a personal computer on the site. 3 refs., 9 figs.

  3. Near-surface 3D reflections seismic survey; Sanjigen senso hanshaho jishin tansa

    Energy Technology Data Exchange (ETDEWEB)

    Nakahigashi, H.; Mitsui, H.; Nakano, O.; Kobayashi, T. [DIA Consultants Co. Ltd., Tokyo (Japan)

    1997-05-27

    Faults are being actively investigated across Japan since the Great Hanshin-Awaji Earthquake. Discussed in this report is the application of the 3D near-surface reflection seismic survey in big cities. Data from trenching and drilling is used for the geological interpretation of the surroundings of a fault, and the reflection seismic survey is used to identify the position, etc., of the fault. In this article, when the results obtained from the experimental field are examined, it is found that the conventional 2D imaging reflection survey betrays the limit of its capability when the geological structure is complicated, that the 3D reflection seismic survey, on the contrary, is capable of high-precision imaging and, when augmented by drilling, etc., becomes capable of a more detailed interpretation, and that it also contributes effectively to the improvement of local disaster prevention in big cities. Using as the model the Tachikawa fault that runs near JR Tachikawa Station, embodiment of the 3D reflection seismic survey is reviewed. For the acquisition of data excellent in quality in a 3D reflection seismic survey conducted utilizing the roads in the sector chosen for experiment in the urban area, the shock generating points and receiving points should be positioned by taking into account the parameters in the bin arranging process so that the mid-points will be regularly distributed on the surface. 3 refs., 11 figs., 1 tab.

  4. Denchuken review. Prospecting and visualization technology; Denchuken review. Chika no tansa kashika gijutsu

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    1997-05-30

    This paper introduces the prospecting and visualization technology cultivated in Denchuken (Central Research Institute of Electric Power Industry). The fluctuations in underground gas, underground water, gravity, terrestrial magnetism, and terrestrial current are information from the earth. The change in underground structure, underground water movement, and underground properties can be grasped using this information. With the progress of electronic engineering, a geophysical exploration method has been rapidly developed in recent years. This method is the most advanced technology in many ground examination methods. In the Denchuken, the following methods have been put to practical use between the shallow section of several meters under ground and the deep section of several kilometers. An underground radar method, seismic prospecting method, electrical prospecting method, CSAMT method that estimates the position of geothermal sources or faults by electromagnetic waves, TDEM method, and AE method that destroys the rock at the depth of the ground and detects by slight sound. Moreover, a geotomography method that can visualize the ground depth in precision using a bore hole by nondestruction executes the tomography based on specific resistance, elastic waves, electromagnetic waves, and percolation. 127 refs., 94 figs., 4 tabs.

  5. Preprint of the Fall 1996 Meeting of the Society of Naval Architects of Japan; Nippon zosen gakkai (1996 nen) shuki koen ronbun maezuri

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    1996-12-31

    Among the papers made public in the Fall 1996 Meeting of the Society of Naval Architects of Japan, 35 papers pertaining to structure, materials, welding, construction and design were summed up as the second book. Concerning structure and materials relations, the book included papers titled An elasto-plastic analysis and the resisting mechanism during large deflection of thin shell structures; Collapse behaviour of stiffened plating under thrust; Post-yield behavior of ship plates; Strength of aluminum alloy members for hull structures; etc. With relation to welding and construction relations, Fatigue strength evaluation method using local and structural stress concentration factors for weld toe of welded joint; Practical evaluation of CTOD for highly strain concentrated structural components; Evaluation of HAZ fracture toughness of welded joints with strength mis-matching by the local approach; etc. As to the design relation, A study of structural optimization design system based on product model in shipbuilding; Basic studies on design supporting system of offshore structures; etc.

  6. 1996 Annual Meeting of Geothermal Research Society of Japan. Abstracts with programs; Nihon chinetsu gakkai 1996 nendo gakujutsu koenkai. Koen yoshishu

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    1997-12-08

    This is a compilation of all the papers made public in the meeting. It includes a total of 111 papers; 14 papers on physical survey, 14 on hot dry rock, 10 on geology, 4 on drilling, 4 on utilization, 21 on heat structure, 3 on scale, 4 on logging, 24 on reservoir, and 13 on geochemistry. Main themes were as follows: Study of MT method and self-potential method and results of the physical survey in New Zealand in the physical survey section. Plan in Ogachi, Akita pref. and development in Hijiori, Yamagata, pref. in the hot dry rock section. Heat source evaluation in the Yuzawa-Ogachi area, Akita pref., and electrical resistivity feature of hot spring reservoir in green tuff bed, Japan, in the geology section. Study of the MWD system in the drilling section. Utilization of geothermal water in Hokkaido in the utilization section. Formation of smectite scale, silica precipitation, and scale prevention measures for steam turbines, in the scale section. High-temperature PT memory system in the logging section. Study of areas of Kuju volcano, Mori, Kakkonda, Otake and Hacchobaru, in the heat structure section. Analysis of fluids from well of the geothermal power plant in the geochemistry section. Heat extraction system from magma in the reservoir section.

  7. Impressions on being awarded with the fiscal 1995 prizes from the Japan Solar Energy Society; Nihon taiyo energy gakkai jusho shokan

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    1996-07-31

    Studies have been made on a microorganism battery which converts solar energy directly into electric energy by utilizing photosynthetic reactions in micro-algae. Electric energy is drawn out from an end of the electronic transmission system for photosynthesis when light is irradiated, and from decomposition of glycogen in organisms when light is shut off. An amorphous solar cell was made capable of restoring output deterioration by annealing. Annealing cycle is important in addition to annealing temperature and time. Investigations were conducted on the relationship between a long-time integral error in irregularly varying insolation intensity and sampling time for the purpose of establishing a measuring method to incorporate it into the Japan Industrial Standard. Development was made on a high-efficiency Fresnel prism having a skylight function, but having no light carrying duct. Awards were given to a solar battery charger applying a counter-flow preventing relay, a solar light/heat hybrid heat pump system, and development of hybrid of hydrogen generation by photovoltaic power (power storage using hydrogen absorbing alloys) with a fuel cell. Cold and hot waste heat recovery by using a seasonal heat storage tank, a water pumping wind mill for irrigation, and water facilities and environmental effects in urban areas also won awards. 3 figs.

  8. Preprint of the papers of the Spring 1997 Meeting of the Society of Naval Architects of Japan; Nippon zosen gakkai (1997 nen) shunki koen ronbun maezuri

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    1997-08-01

    This is a proceedings of the Spring 1997 Meeting of the Society of Naval Architects of Japan. It includes 19 papers on structures, materials, welding, building, design and machinery of ships and floating structures. For the automation of ocean surveys, a development is conducted of cruising-type autonomous underwater vehicles (AUV). The following are important studies: `Development of a small cruising-type AUV and training of constant altitude swimming,` `Visual feedback navigation for cable tracking by autonomous underwater vehicles,` and `Development of the hull inspection robot (RTV-SHIP).` Large floating bodies for the ocean space utilization are being proposed, and the following are useful for strength analyses: `Structural analyses of very large semi-submersibles in waves,` `An investigation on the dynamic response and strength of very long floating structures by beam modeling on an elastic foundation` relating especially to pontoon-type floating bodies with no mooring, and `A basic investigation on deflection wave propagation and strength of very large floating structures.` The title `Temperature effect on corrosion fatigue strength of coated ship structural steel` is very useful for prevention of the hull corrosion.

  9. Proceedings of the 55th Meeting on Cryogenics and Superconductivity; Dai 55 kai 1996 nendo shuki teion kogaku chodendo gakkai koen gaiyoshu

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    1996-11-06

    This is a proceedings of the 55th Meeting on Cryogenics and Superconductivity. As for wires, made public were Bi-system 2223, Y-system NbTi, NbSn, Nb3Al, etc. As to oxide superconductors, some of them are promising. The study of those characteristics and the developmental application to the electric power field such as coils and cables were introduced. Beside wires, multilayer film superconductors were also introduced. With relation to fundamentals and theories, became topics were pinning characteristics, NbTi proximity effects, magnetic flux and visualization, stability, etc. About the application, large refrigerators are discussed in the refrigeration field in addition to GM/pulse tube refrigerators. Concerning cooling technology, made public were the development of a floating railroad use 80K cooling system, etc. Also studied were power leads, superconducting magnet, control action characteristics, etc. SMES (superconducting magnetic energy storage) also became a topic, and the element coil energization experiment, stability and mechanical properties were described. The paper also touched on accelerators, large superconducting devices such as LHD (large helical device) and ITER (international thermal-nuclear experimental reactor) as well as generators and current limiters. The cryogenetic engineering was also reported such as fracture toughness and superfluidity of cryostats and structural materials for extremely low temperatures.

  10. 56th (fiscal 1997) Meeting on Cryogenics and Superconductivity; Dai 56 kai 1997 nendo shunki teion kogaku chodendo gakkai koen gaiyoshu

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    1997-05-14

    In the meeting, 266 papers were made public which deal with the following fields: GM refrigerators, pulse tube refrigerators, cold storage equipment, Bi-2212 system, coil application, superconducting generators, LHD/ITER/accelerators, cable-in conduit conductors, electromagnetic phenomena/proximity effect, oxide cable, Nb3Sn, Nb3Al, metal materials, WE-NET, friction/organic materials, composite materials, Nb3Sn, Nb3Al wires, strand wire structure analysis, hybrid superconducting wire, Y system, Bi system, low temperature device, measurement, high magnetic field NMR magnet, oxide NMR application, Bi-2223 system wire, pinning, NbTi ac wire, pinning/ac loss, various characteristics, superconducting application, refrigerating system, heat transfer, cryostat, Hg/Ti/Y system wire, ac loss/application, superconducting electric power storage system and the development of element technology therefor, current limiter/magnetic flotation, stability and drift of strand conductors, stability, ITER, LHD/accelerator/SLIM, oxide application, conductor stability test and others, and quench of ac cable.

  11. Preprint of the Fall 1996 Meeting of the Society of Naval Architects of Japan; Nippon zosen gakkai (1996 nen) shuki koen ronbun maezuri

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    1996-12-31

    Among the papers made public in the Fall 1996 Meeting of the Society of Naval Architects of Japan, 40 papers pertaining to resistance, propulsion, motion, and ocean were summed up as the first book. Concerning the resistance relation, the book included papers titled Analysis of wave-making characteristics of ship form by Mathieu function expansions of wave-amplitude functions derived from wave analysis; Studies on surface tension effect on free surface flow around floating models; Numerical computation of viscous flows with free surface around a series 60 model; etc. As to the propulsion and motion, Design system for optimum contra-rotating propellers; Performance of the patrol icebreaker `TESHIO` in ice-covered waters; A study on effect of bow shape on icebreaking resistance; Time domain analysis of ship response in directional irregular wave; Study on prediction method for hydrodynamic force acting on a ship hull in swaying motion; etc. With relation to the ocean relation, On statistical properties of wave amplitudes in stormy sea; Statistical properties of encounter wave grouping phenomena in following and quartering seas; Development of hybrid type on board measuring system for directional wave spectrum; etc.

  12. Proceedings of the 55th Meeting on Cryogenics and Superconductivity; Dai 55 kai 1996 nendo shuki teion kogaku chodendo gakkai koen gaiyoshu

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    1996-11-06

    This is a proceedings of the 55th Meeting on Cryogenics and Superconductivity. As for wires, made public were Bi-system 2223, Y-system NbTi, NbSn, Nb3Al, etc. As to oxide superconductors, some of them are promising. The study of those characteristics and the developmental application to the electric power field such as coils and cables were introduced. Beside wires, multilayer film superconductors were also introduced. With relation to fundamentals and theories, became topics were pinning characteristics, NbTi proximity effects, magnetic flux and visualization, stability, etc. About the application, large refrigerators are discussed in the refrigeration field in addition to GM/pulse tube refrigerators. Concerning cooling technology, made public were the development of a floating railroad use 80K cooling system, etc. Also studied were power leads, superconducting magnet, control action characteristics, etc. SMES (superconducting magnetic energy storage) also became a topic, and the element coil energization experiment, stability and mechanical properties were described. The paper also touched on accelerators, large superconducting devices such as LHD (large helical device) and ITER (international thermal-nuclear experimental reactor) as well as generators and current limiters. The cryogenetic engineering was also reported such as fracture toughness and superfluidity of cryostats and structural materials for extremely low temperatures.

  13. Preprint of the papers of the Spring 1997 Meeting of the Society of Naval Architects of Japan; Nippon zoen gakkai (1997 nen) shunki koen ronbun mazezuri

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    1997-08-01

    This is a proceedings of the Spring 1997 Meeting of the Society of Naval Architects of Japan. It includes 21 papers on resistance, propulsion, movement and ocean relating to ships and floating structures. Recently, large floating structures have been regarded as promising as ocean structures having potential usability for floating airports, etc., and the response to lots of waves is being studied. The title `Numerical response analysis of a large pontoon-type or mat-type floating structure in regular waves` will be useful. Moreover, the pontoon-type floating body being proposed as the floating airport is very large having a length of 5,000m and a width of 1,000m, but very small having a thickness of 5m at thickest, several figures smaller than the dimension of the horizontal plane. Therefore, it is predicted that large elastic deformation is induced by dynamic external force such as waves. Accordingly, the title `On the prediction of hydroelastic behaviors of a huge floating structure in waves` is a useful paper.

  14. Study of seismic data acquisition using physical modeling system; Butsuri model jikken sochi wo mochiita data shutoku gijutsu ni kansuru kento

    Energy Technology Data Exchange (ETDEWEB)

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

    1996-10-01

    For the physical modeling system of Technology Research Center, Japan National Oil Corporation, data acquisition on the ocean and ground can be simulated using models. This system can provide data for verification of the data processing and elastic wave simulation algorithm. This can also provide data for decision of experiment specifications by making a model simulating the underground structure of the given test field. The model used for the physical modeling system is a gradient multilayer model with six-layer structure. Depth migration before stacking was conducted using data obtained through two acquisition methods, i.e., up-dip acquisition and down-dip acquisition. The depth migration before stacking was performed for data obtained by up-dip acquisition in addition to the records obtained by down-dip acquisition. Consequently, a definite reflection surface was observed, which has not been observed from the processing results of down-dip acquisition data. 9 figs.

  15. Detecting technology of buried pipes and hollow areas by using physical detecting method; Senbu chika deno butsuri tansaho ni yoru maisetsukan, kudo chosa

    Energy Technology Data Exchange (ETDEWEB)

    Nagashima, Y. [NTT Technical Assistance and Support Center, Tokyo (Japan)

    1997-12-01

    No precise records are available on positions of buried pipes which constitute such life lines as electric power, water supply, gas supply, and telecommunications under roads. This record unavailability is causing troubles of damaging these pipes when road excavating constructions are carried out. Therefore, a technology has been demanded, which can measure positions of buried pipes non-destructively from the ground surface. To meet this requirement, development has been performed on a technology to explore pipes buried in depths up to 3 meters. Research results thereon have made achievements today causing a large number of practically usable devices to emerge into existence. Major exploration methods include the electromagnetic wave method and the electromagnetic induction method. This paper describes principles, problems, and exploration application examples of the pulse radar electromagnetic wave method and the electromagnetic induction method, and some considerations thereon. No devices have been completed to date, which can fully satisfy the requirements in exploring buried objects. This is because electromagnetic waves get attenuated sharply under the ground, and because a large number of boundary faces exist underground to reflect electromagnetic waves. It is necessary to continue research and development efforts. 7 refs., 32 refs.

  16. Historical overview of geophysical exploration for hydrocarbon prospecting in Japan; Nippon no sekiyu kogyo ni okeru butsuri tanko gijutsu no kaihatsu

    Energy Technology Data Exchange (ETDEWEB)

    Tamura, Y. [Japan Petroleum Exploration Corp., Tokyo (Japan)

    1998-08-01

    This paper describes a historical overview of geophysical exploration for hydrocarbon prospecting in Japan. In general, history is divided into eras by the qualitative change. In the case of geophysical exploration, the history is desired to be divided by considering the both of qualitative change in the technology and that in the practical application. In the early time of geophysical prospecting, gravitational exploration, magnetic exploration, seismic refraction method and seismic reflection method were elementarily and successfully tried. In the era of classical geophysical exploration, seismic reflection method and gravitational/magnetic methods were basically completed, and accumulation structures of potential petroleum were discovered around existing oil fields. In the era of systematic geophysical exploration, techniques of underground geological reflection profiles were completed with digitalization, and systematic petroleum exploration was conducted. In the era of modern geophysical exploration, 3D seismic was put into practice, and the inversion accuracy was improved, in which the geophysical exploration could be contributed jointly with the geological techniques. New development era of geophysics is expected. 31 refs., 10 figs., 5 tabs.

  17. Study of seismic data acquisition using physical modeling system; Butsuri model jikken sochi wo mochiita data shutoku gijutsu ni kansuru kento

    Energy Technology Data Exchange (ETDEWEB)

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

    1996-05-01

    The Physical Modeling System introduced into the Technology Research Center, Japan National Oil Corporation, and data collected by use of the system are presented. The Physical Modeling System is 10,000 times smaller than the real one, comprising a water tub section, measuring device section, and control section, etc. The water tub section comprises a tub for housing the model, transducers for transmitting and receiving vibration, controllers, etc. The water tub measures 1.8{times}1.2{times}0.9m. The model used in the experiment is an `inclined multilayer model` with each of its six layers pinching out toward the top, and is usable for the comparison of various migration methods. In one case in the records, reception was made at 184 reception points deployed at intervals of 3mm, when the minimum offset was 15mm and the maximum offset 564mm. Nothing very obvious was observed when the ordinary overlapping of DMO and CDP was applied to this record, which suggests that pre-overlapping migration treatment is required. 5 figs.

  18. Physical chemistry of water at low temperatures. Present state and future prospects; Teion to mizu no butsuri kagaku. Kenkyu no genjo to shorai

    Energy Technology Data Exchange (ETDEWEB)

    Murase, N. [Tokyo Denki Univ., Tokyo (Japan). Faculty of Science and Engineering

    1996-02-05

    The various characteristics of water are explained qualitatively based on the combinations of the hydrogens among the water molecules. However, in the quantitative understanding of such characteristics, the forms of the hydrogen-combination should be referred and the water-structure of liquid has to be explained at the molecular level. The attention is attracted again to the study of water conjointly with the clarification of the exhalation behavior as the property of water in the hyperquenching field and the progress of the computer simulations including X-ray, neutron diffraction and atomic dynamics. On the other hand, water is always the subject of the researches in respect of food engineering and low-temperature biology with the theme for preserving biological resources as well as samples. Deeply interesting data relating to the structures and the properties of liquid water are provided by the study of the water at low temperature. Simultaneously with said recognition, physical chemistry of water at low temperatures are explained in this paper centering at the models of liquid water, hydration, hyperquenching water, the freezing of water and the glassy state of water. 9 refs. 4 figs.

  19. Trends on recycling of metallic resources and physical chemistry of recycle processes. Kinzoku shigen no recycling no doko to recycle process no butsuri kagaku

    Energy Technology Data Exchange (ETDEWEB)

    Nakamura, T. (Kyushu Institute of Technology, Kitakyushu (Japan). Faculty of Engineering)

    1991-08-20

    Taking up smelting processes incorporated in the currently used recycling systems that handle Fe, Al and Cu scraps which are much recycled as metallic resources, considerations were given on the physical chemistry of the processes. In considering wastes and scraps as resources, it is necessary to recognize that the object metals are high in grades, but unstable quantitatively and they contain many kinds of elements (impurity elements) to be treated. As a method to remove copper from solid Fe scraps, the separation method utilizing the melting point difference is simple as a process, and is worth discussing for a practical use. However, a method to remove copper from alloyed iron melt and steel melt is difficult thermodynamically. Enumerating and discussing the problems in refining Al and Cu scraps revealed that there are a number of points insoluble by the currently available refining technologies, and concluded that superior refining processes must be developed, and the recycling problems must be considered including as far as the recovery systems. 66 refs., 11 figs., 9 tabs.

  20. Optimization of dynamic source depth for seismic surveys. Part 7; Dynamite shingen no hasshin shindo no saitekika ni tsuite (hyoso kozo no suitei (kusssetsuho jishin tansa oyobi denki denjiho tansa)). 7

    Energy Technology Data Exchange (ETDEWEB)

    Tanaka, H.; Murayama, R.; Mitsuhata, Y.; Ishikawa, H. [Japan National Oil Corp., Tokyo (Japan). Technology Research Center

    1996-05-01

    For the improvement of quality of data collected by reflection aided seismic exploration using dynamite as the seismic source, information has to be collected about the surface layer structure before the charge depth is determined. For this purpose, refraction, electric, and electromagnetic exploration methods were tried. In the refraction method, an impactor was used as the seismic source. In the records, the surface wave prevails because vibration was generated on the surface. Analysis was made by the use of the initial travel time tomography. In the electric exploration, a double pole array was used to measure resistivity. The measured data was subjected to a fully automatic inversion for analysis. As the result, it was disclosed that it was useful to know the deep-level structure directly by use of tomographic methods in refraction seismic exploration so as to find the optimum charge level. Furthermore, about the electric and electromagnetic exploration techniques, it was found that these methods can be applied making use of resistivity to the evaluation of groundwater saturation. 7 refs., 5 figs., 3 tabs.

  1. How to minimize the phase difference for the array microtremor observation; Soi gosa no sukunai bido tansa no kansokuho

    Energy Technology Data Exchange (ETDEWEB)

    Moriya, T.; Ishikawa, K.; Miyakoshi, K.; Okada, H. [Hokkaido Univ., Sapporo (Japan). Graduate School of Science

    1996-06-01

    The microtremor observation is a method that the surface wave of cycle of 0.1-5 seconds contained in the vertical component of a microtremor is extracted, its phase velocity is estimated and an one dimensional underground structure is estimated from the obtained dispersion curve. The microtremor observation in the microtremor survey conducts about 10 earthquake motion observations by an array (grouped observation network) spreading over the ground surface maintaining simultaneity, hence many seismometers, multichannel data recorders and clocking devices become necessary. The authors of this paper have so far studied and experimented on methods for minimizing a phase error caused by asynchronous sampling peculiar to independent digital observation, methods for maintaining simultaneity at each observation spot, high precision adjusting methods of natural period of seismometer and selection of the seismometer constant hardly affected by environmental changes, and in this paper, these matters are reported. In case when the array observation is made with independent digital observation devices, it is important to minimize the phase shift after clocking correction. 10 refs., 8 figs.

  2. Fundamental study on airborne electromagnetic survey using grounded source; Chihyo source gata kuchu denji tansa no kisoteki kenkyu. 2

    Energy Technology Data Exchange (ETDEWEB)

    Mogi, T.; Fujimitsu, Y. [Kyushu University, Fukuoka (Japan). Faculty of Engineering; Tanaka, Y. [Kyoto University, Kyoto (Japan). Faculty of Science; Jomori, N. [Chiba Electronics Research Institute, Chiba (Japan); Morikawa, T. [Dowa Engineering Co. Ltd., Okayama (Japan); Kusunoki, K. [Central Research Institute of Electric Power Industry, Tokyo (Japan)

    1997-05-27

    With an objective to develop an airborne electromagnetic survey method for greater depths achievable of exploration, a discussion was given on an exploration method of a type in which a transmitting device is placed on the ground to receive signals in an atmosphere. A prototype exploration apparatus is mounted with a fluxgate magnetometer, an attitude meter, a GPS, and a battery. This exploration apparatus is suspended on a 30 meter long rope from a helicopter to perform the exploration. Two flight tests on this apparatus were carried out in the Unzen area, Nagasaki Prefecture and the Motomiya area, Wakayama Prefecture. The ground source was extended to a distance of 1.5 km, and a current of about 20 A was flown with a quiescent wave having four-second cycles. The helicopter flew nearly horizontally at a ground speed of about 50 km, a flight altitude of 450 m above sea level, and a terrain clearances of 100 to 400 m. The obtained data had variations in correspondence with changes in roll and pitch angles, whereas the variation of about 5000 nT was reduced to about 1000 nT as a result of correction. It was not possible, however, to correct completely the variation with short cycles, requiring further discussions on frequency characteristics of the magnetometer. 6 figs., 1 tab.

  3. Seismic reflection survey in Omama fan area, Gunma prefecture; Gunma Omama senjochi ni okeru hanshaho jishin tansa

    Energy Technology Data Exchange (ETDEWEB)

    Yamaguchi, K.; Kano, N.; Yokokura, T.; Kiguchi, T.; Yokota, T.; Matsushima, J. [Geological Survey of Japan, Tsukuba (Japan)

    1996-10-01

    Seismic reflection survey was performed for the Medial Tectonic Line, an important geological tectonic line in the Kanto plains, at Kushibiki district, Saitama prefecture in the north-western part of the Kanto plains. It was estimated that movements of the basement were different in the individual sides of the active fault. In this study, the seismic reflection survey was performed at the Omama fan area, Gunma prefecture, which is located at the north-eastern extension of the Kushibiki plateau, to grasp the structure of basement to the depth of about 1.0 s of return travel time, and the upper sediments. Two traverse lines passing Ota city, Kiryu city, and Nitta town were used. Southern part of the traverse line-1 was in the bottom land in the middle of Tone river, and northern part was in the Omama fan area. The ground surface along the traverse line was flat. Hachioji heights are the heights elongating in the NW-SE direction and having relative height of 100 to 200 m against the surrounding plain. Another traverse line-2 was set on the steep slope having relative height more than 100 m. The Brute stack time section of each traverse line was characterized by the gradient reflection surface AA of the traverse line-1. It was suggested that the AA or intermittent parts of reflection surfaces deeper than AA may relate to the tectonic lines in the more ancient geological ages. 2 figs., 1 tab.

  4. Study on spontaneous potential exploration considering resistivity structures; Hiteiko kozo wo koryoshita shizen den`iho tansa

    Energy Technology Data Exchange (ETDEWEB)

    Sato, H.; Sakurai, K.; Shimada, H. [OYO Corp., Tokyo (Japan)

    1996-10-01

    Spontaneous potential (SP) was measured on the known traverse line of resistivity structure crossing Hanaori fault in Ohara area, Kyoto city to observe change in SP around the fault and to examine the possibility of fault position exploration. The supposed causes of generation of SP are as follows: the existence of sulfide mineral deposit including polarized minerals, underground fluid flow, and the existence of stratum including chemical compositions from hot springs. The SP method estimates underground structures based on measured surface potential distributions using DC component under anomaly of SP. FEM modeling clarified that a fault fracture zone is one of the causes of generation of SP, by considering SP measurement and resistivity structure strongly affecting observed SP. Consequently, combination of SP measurement with resistivity structure exploration allows a reliable fault estimation method. Under the assumption that anomaly of SP is caused by polarization around fault, the horizontal dipole model based on polarization of current source dipole along fault can well explain the measured data. 2 refs., 6 figs.

  5. Data processing for the mise-a-la-masse survey; Ryuden den`iho tansa no data shori

    Energy Technology Data Exchange (ETDEWEB)

    Hashimoto, K.; Mizunaga, H.; Ushijima, K. [Kyushu University, Fukuoka (Japan). Faculty of Engineering; Kaieda, H. [Central Research Institute of Electric Power Industry, Tokyo (Japan)

    1996-10-01

    Data processing method was studied for mise-a-la-masse survey. Mise-a-la-masse method using wells as current sources measures resultant ground surface potential difference, and detects underground local resistivity anomaly. To extract resistivity anomaly largely different from surroundings, the anomaly is extracted as difference between the estimated value of regular resistivity structure (background) and potential difference or apparent resistivity. The following three approximations were attempted to estimate the background: the theoretical equation assuming isotropic homogeneous resistivity structure, that assuming horizontal multi-layered structure and the exponential function of distance from linear electrode for apparent resistivity, and these were compared with each other by numerical model experiment. The data processing method which determines the resistivity structure of the background and the residual of apparent resistivity distribution by inversion analysis using the above second equation, could precisely extract local resistivity anomaly, and estimate the depth distribution of resistivity. 5 refs., 10 figs., 2 tabs.

  6. Exploration and development of Uenotai geothermal field, Akita prefecture, northeastern Japan. Uenotai chinetsu chitai no tansa to sono kaihatsu

    Energy Technology Data Exchange (ETDEWEB)

    Naka, T. (Akita Geothermal Energy Co., Akita (Japan)); Okada, H. (Dowa Mining Co. Ltd., Tokyo (Japan))

    1992-08-30

    This paper describes exploration and development of the Uenotai geothermal field where a geothermal power plant is being build to start power generation scheduled for 1994. Geothermal reservoir beds at the Uenotai field are of fracture type. The beds consist not only of fracture zones generated from fault motions, but also autobrecciated lava structure, lithofacial boundaries including different lithofacies at lava bottom, intrusive rock circumference, and fault fracture zones crossing complexly with these formations, forming passages of geothermal fluids and the basis for heat convection. The heat source is thought to be the Quaternary magma source located deep under the upheaval area in Mt. Oyasu, where geothermal reservoir beds of hot water dominant type, steam dominant type, and high-temperature seam type exist. The produced hot water is of an alkaline NaCl type. The pre-Tertiary deposit in the Uenotai area under development would be the most important bed for the development, and geothermal reservoir beds of steam dominant type at 500 m below sea level or deeper are the target for the development. The scale of the development has been established under an assumption that it is most effective to produce steam at 232 t/h maintaining the well opening pressure at 9.5 KSCA to generate power at 27500kW. 18 refs., 16 figs., 8 tabs.

  7. Seismic exploration for methane hydrate. Example from Nankai trough; Metan haidoreto no tansa. Nankai torafu no rei

    Energy Technology Data Exchange (ETDEWEB)

    Aoki, Y. [JAPEX Geoscience Inst. Inc., Tokyo (Japan)

    1995-08-01

    The index which appears most readily in the reflected seismogram obtained in methane hydrate exploration is the change in the velocity of seismic waves originated by methane hydrate itself. The largest index is the presence of strong reflecting surface observed in earthquake cross section in a sea area. It is considered that a large amount of methane hydrate is distributed in the periphery of Japan on the shore side slope (on the Japanese Islands side) of the Nankai trough. As a result of underwater investigations carried out since 1984, it is clarified that there are many gushing points of comparatively high temperature methane-containing water in parallel with the Nankai trough on the land side slope of the Nankai trough. 583 excavation points were selected by Leg 87 of ODP held in 1982. Penetration of faults was attempted, but recovery of core was extremely difficult and faults themselves could not be found. However, the density and the rate of seismic waves could be recorded in shallow areas. 3 refs., 7 figs.

  8. Preliminary study of airborne electromagnetic survey using grounded source; Chihyo source gata kuchu denji tansa no kisoteki kenkyu

    Energy Technology Data Exchange (ETDEWEB)

    Mogi, T. [Kyushu University, Fukuoka (Japan). Faculty of Engineering; Shimoizumi, M. [Kitakyushu Polytechnic College, Kitakyushu (Japan); Kusunoki, K. [Central Research Institute of Electric Power Industry, Tokyo (Japan); Morikawa, T. [Dowa Engineering Co. Ltd., Okayama (Japan); Jomori, N. [Chiba Electronics Research Institute, Chiba (Japan)

    1996-05-01

    For the development of an airborne electromagnetic prospecting method capable of deeper exploration, a basic study was made about a system wherein a transmitter (source) is positioned on the ground and the receiving is done in the sky. Even in case of this airborne electromagnetic method, the TDEM method is supposedly advantageous over others as in case of groundborne exploration. In the study, the transient response of an airborne vertical magnetic field to a horizontal layered structure was calculated. The current source was 2000m long with a capacity of 30A. The one-layer structure was a 10 Ohm m semi-infinite ground, and the two-layer structure had a 100 Ohm m structure just under the one-layer structure. The result of the calculation suggests that, in the absence of a layer of extremely low resistivity, observation of an approximately 1 second long transient response aboard a helicopter flying at approximately 50km/h will enable an approximately 1000m deep exploration. Problems to affect airborne observation, such as swinging, natural magnetic field fluctuation, and artificially produced noises were investigated by use of a magnetometer suspended from a helicopter in flight. 2 refs., 6 figs.

  9. Shallow seismic reflection prospecting in Hachiro-kata reclaimed land; Hachirogata kantakuchi ni okeru senbu hanshaho jishin tansa

    Energy Technology Data Exchange (ETDEWEB)

    Kitsunezaki, C.; Fukutome, T.; Matsumoto, S.; Noda, K.; Sato, T. [Akita University, Akita (Japan). Mining College; Hayashi, H.; Ishii, E.; Yamanaka, Y.; Matsuno, K.; Mikuni, S. [Suncoh Consultant Co. Ltd., Tokyo (Japan)

    1997-05-27

    Along the Japan Sea coast in Akita Prefecture and in the vicinity, there exist active fault groups, such as the Kitayuri thrust fault group in the south and Noshiro thrust fault group in the north. It is estimated that there is another fault, running from Akita City located between the above-said two thrust fault groups into the Hachiro-kata reclaimed land, roughly connecting the two thrust fault groups. This third fault is supposed to be related to the hypocenter of Tencho Earthquake of 830, but its location and structural configuration are not known, and it is not known whether it is an active fault, either. Investigations are conducted using S- and P-waves. The greatest problem in the use of P-waves is that there exists a layer in which signal attenuation is high and transmission is anomalously slow. This problem is ascribed to the layer pore water rendered unsaturated though slightly by the inclusion of air bubbles, and is explained for the most part by the White model. A survey using S-waves is advantageous in that it does not experience no difficulty of this kind. In the P-wave cross section, a structure supposed to be an inversion layer is observed at a level deeper than 200m. In the case of the S-wave method, more details of the shallow structure will be available when the degree of CMP stacking is augmented as usual. 2 refs., 9 figs., 1 tab.

  10. 3D seismic experiment in difficult area in Japan; Kokunai nanchiiki ni okeru sanjigen jishin tansa jikken

    Energy Technology Data Exchange (ETDEWEB)

    Minegishi, M.; Nakagami, K.; Tanaka, H. [Japan National Oil Corp., Tokyo (Japan). Technology Research Center

    1997-05-27

    Difficult area in this context means an exploration-difficult area supposed to store oil/gas but retarded in exploration for the lack of knowledge about the geological structure due to poor quality of available seismic survey records. Discussed in this paper is a survey conducted into an area covering the southern part of Noshiro-shi, Akita-ken, and Yamamoto-cho, Yamamoto-gun, Akita-ken. An area size suitable for data collection at a target depth of 2500m is determined using an interpretation structure compiled on the basis of available well data and 2D seismic survey data. The plan for siting shock points and receiving points is modified case by case as restrictive factors come to the surface (resulting from the complicated hilly terrain, presence of pipes for agricultural water, etc.). The peculiarities of seismic waves in the terrain are studied through the interpretation of the available well data and 2D seismic survey data for the construction of a 3D velocity model for the confirmation of the appropriateness of the plan for siting shock points and receiving points. Efforts are exerted through enhanced coordination with the contractor to acquire data so that a technologically best design may be won within the limits of the budget. The quality of the data obtained from this experiment is in general better than those obtained from previous experiments, yet many problems remain to be settled in future studies about exploration-difficult areas. 4 refs., 4 figs., 1 tab.

  11. 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.

  12. Critical Comments on Brian Victoria's "Engaged Buddhism: Skeleton in the Closet?"

    Directory of Open Access Journals (Sweden)

    Koichi Miyata

    2015-02-01

    Full Text Available In "Engaged Buddhism: A Skeleton in the Closet?" (Vol. 2 Brian Daizen Victoria claims, among other things, that Tsunesaburo Makiguchi (1871-1944, founder of the Soka Kyoiku Gakkai (forebear of the Soka Gakkai and Soka Gakkai International, was an active supporter of the Japanese wars of aggression. In this response, Koichi Miyata argues that Victoria's claims rest on the highly selective use of quotes, and ignore key interpretative issues associated with Japanese imperial fascism and its underlying belief structures. Miyata discusses the significance of Makiguchi's arrest and imprisonment under a law specifically aimed at opponents of the war efforts, in his analysis of critical lapses in Victoria's article.

  13. Disease: H01316 [KEGG MEDICUS

    Lifescience Database Archive (English)

    Full Text Available ICD-10: B35 MeSH: D014005 PMID:17667895 Hiruma S [Clinical aspect of dermatophyto...sis (ringworm)]. Nihon Ishinkin Gakkai Zasshi 48:116-9 (2007) PMID:17853533 Nishimoto K [Clinical aspect and

  14. Proceedings of the Spring Meeting of the Society of Naval Architects of Japan (1996). Part 1. Resistance, propulsion, advance, and ocean; Nihon zosen gakkai (1996 nen) shunki koen ronbun maezuri. 1. Teiko, suishin shindo, kaiyo

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    1996-12-31

    This is a proceedings of the Spring Meeting of the Society of Naval Architects of Japan made public on May 15 and 16, 1996. In the basic research, the following were included: Numerical simulation for submerged body fitted with hydrofoil; Simulation of tandem hydrofoils by finite volume method with moving grid system; Determination of the unknown method surface of planning plates by a formulation based on high aspect ratio approximation; Numerical simulation of a bubble flow by modified density function method, etc. As to floating bodies, Response characteristics of a long life type floating offshore airport in waves (3rd report: Response due to short waves and an attempt of active inclination control); Feasibility design of a floating airport and estimation of environmental forces on it; On the estimation method of hydrodynamic forces acting on a huge floating structure, etc. In addition, A numerical prediction with `DMDF` model of pack ice motion in the Okhotsk Sea; Development of an observation robot `Flying Fish` for comprehensive measurements of ocean environment; Water entry simulation of free-fall lifeboat, etc.

  15. Proceedings of the papers read in the 47th Science Lecture Meeting of the Society of Materials Science, Japan; Nippon Zairyo Gakkai dai 47 ki gakujutsu koenkai koen ronbunshu

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    1998-05-21

    As to the evaluation and analysis of organs and strength at high temperature, papers were reported on high temperature reformation behavior, damage models and analysis/evaluation, long-time creep fatigue, fatigue strength, fatigue crack development, microstructures of super alloys/composite materials, high temperature characteristics of ductile materials, etc. Relating to the materials database related to phase transformation and its application to simulation, reported were quenching, phase transformation behavior and structural formulas, concrete, polycrystal reformation, timber and dynamics, analysis of composite materials, etc. Concerning strength characteristics and evaluation of surface reforming materials, papers on abrasion, thin films, monocrystal, grain boundary, corrosion, etc. About the design/evaluation of ceramic materials, the sintering process, reformation/fracture behaviors and their simulation, strength characteristics of composite ceramics, fatigue, evaluation of superconduction characteristics, etc. The paper also described composite materials/organism use materials, polymer, magnetic materials, etc. As the impact behavior of materials/structures, reported were impact pressure welding, impact loads, fatigue/fracture of composite materials, thermal analysis, etc. From time to time, measuring methods were also reported

  16. Proposal from the Japan Society of Engineering Geology in the report meeting on Hyogo-ken Nanbu earthquake; Hyogoken nanbu jishin hokokukai ni okeru Nippon oyo chishitsu gakkai kara no teian

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    1996-04-10

    Contribution to disaster protection measures and earthquake resistance technology are important activities except application of geology for Japan Society of Engineering Geology. The society carries out field measurement and analysis, and offers analytical method and inverse analytical method for engineering analyses of data. An analytical method uses physical properties of ground and seismic forces as input data, and verifies the stability and safety of some supposed structures at earthquake. It is important to acquire physical properties of ground enough and to measure accurately information of external forces. An inverse analytical method surveys various phenomena at earthquake, and diagnoses the causes of such phenomena. In this time, the engineering survey, evaluation and analysis of active faults and seismic faults are insufficient. It is also one of the issues that the society couldn`t acquire data systematically from the observation hole of underground water. It is also important to consider the point of contact with the actual world. 2 figs.

  17. Proceedings of the Spring Meeting of the Society of Naval Architects of Japan (1996). Part 2. Structure, materials, welding, construction, and design; Nihon zosen gakkai (1996 nen) shunki koen ronbun maezuri. 2. Kozo, zairyo, yosetsu, kosaku, sekkei

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    1996-12-31

    This is a proceedings of the Spring Meeting of the Society of Naval Architects of Japan made public on May 15 and 16, 1996. In the basic research, the following are included: Basic studies on computer aided concurrent engineering for hull structure design and piping design; Fundamental study on the new method to estimate vibration level on a ship; Flat plate approximation in the three-dimensional slamming; Development of new finite element by source method, etc. As to fracture and cracks, Equivalent CTOD concept based on the local approach and its application to fracture performance evaluation of welded joints; Fracture mechanical modeling of brittle crack propagation and arrest of steel; An evaluation method for ductile crack propagation in pre-strained plates; Multiple fatigue cracks propagating in a stiffened panel, etc. Relating to fatigue strength, Fatigue life estimation of welded joints of an aluminum alloy under superimposed random load waves; Study on unified fatigue strength assessment method for welded structure, etc.

  18. Archaeological prospecting using electrical resistivity method. Case history of Kaibukiyama ancient tomb; Denki tansaho ni yoru iseki tansa. Kaibukiyama kofun no chosarei

    Energy Technology Data Exchange (ETDEWEB)

    Mizunaga, H.; Ushijima, K.; Kishikawa, H. [Kyushu University, Fukuoka (Japan). Faculty of Engineering

    1997-05-27

    To grasp the three-dimensional structure of ancient tomb during the archaeological prospecting of Kaibukiyama ancient tomb, various electrical resistivity methods were tried. For the survey, firstly, in order to clarify the electrical resistivity structure of rear circular part of ancient tomb, roughly, mapping was conducted by means of two-electrode method using a multi-channel measuring system. Then, the vertical prospecting was conducted densely with a mesh form having VES intervals of 2 m as a detailed survey by means of Schlumberger method. For the three-dimensional inverse analysis of apparent electrical resistivity data by the two-electrode method, a program with high calculation speed was developed by using algorithm where Jacobian with a homogeneous model is adopted for the Jacobian calculation. As a result of the analysis, an outline of underground 3-D resistivity structure was determined. The resistivity anomaly with high values obtained from the results of 2-D inverse analysis of VES curve by means of Schlumberger method agreed well with the central part of the ancient tomb, which was confirmed during the archaeological survey. 4 refs., 8 figs.

  19. Efficient calculation of potential distribution in two-layer earth; Niso kozo daichikei ni okeru denki tansa no tame no koritsuteki den`i keisan shuho

    Energy Technology Data Exchange (ETDEWEB)

    Kataoka, M.; Okamoto, Y. [Chiba Institute of Technology, Chiba (Japan); Endo, M.; Noguchi, K. [Waseda University, Tokyo (Japan); Teramachi, Y.; Akabane, H. [University of Industrial Technology, Kanagawa (Japan); Agu, M. [Ibaraki University, Ibaraki (Japan)

    1997-05-27

    An efficient calculation method of potential distribution in the presence of an embedded body in multi-layer earth has been proposed by expanding the method of image with a consideration of multiple reflection between the ground surface and each underground boundary. For this method, when solving boundary integral equation with the potential of embedded body surface as only one unknown, i.e., when obtaining discretization equation, ordinary boundary element program developed for analyzing the finite closed region can be used. As an example, numerical calculation was conducted for the two-layer earth. The analysis expression of potential distribution in the case of the certain embedded body in two-layer earth has never published. Accordingly, the calculated results were compared with those by the integral equation method. As a result, it was concluded that the primary potential obtained from the present method agreed well with that obtained from the integral equation method. However, there was a disregarded difference in the secondary potential. For confirming the effectiveness, it was necessary to compare with another numerical calculation method, such as finite element method. 5 refs., 5 figs.

  20. High resolution seismic refraction method with multichannel digital data acquisition system; Digital ta channel sokutei system wo mochiita koseido kussetsuho jishin tansa

    Energy Technology Data Exchange (ETDEWEB)

    Hayashi, K. [Oyo Corp., Tokyo (Japan)

    1997-05-27

    This paper introduces a multichannel digital data acquisition system and examples of measurements with the system in seismic exploration using the high resolution seismic refraction method. The high resolution seismic refraction system performs analyses nearly automatically by using a computer after initial travel time has been read. Therefore, the system requires high-accuracy travel time data, for which a multichannel digital measuring instrument developed recently for seismic exploration using the refraction method has been used for the measurement. The specification specifies the number of channels at 144 as a maximum, a sampling time of 62.5 {mu}sec to 4 m sec, the maximum number of sampling of 80,000 samples, and gain accuracy of {plus_minus} 1%. The system was used for surveying a tunnel having a maximum soil cover of about 800 m. The traverse line length is about 6 km, the distance between vibration receiving points is 50 m, and the number of vibration receiving points is 194. Executing measurements of single point system using GPS can derive accurate velocity in the vicinity of the basic face of the tunnel construction. Results were obtained from the investigation, which can serve more for actual construction work. 10 refs., 6 figs., 1 tab.

  1. Laboratory study on streaming potential for exploring underground water flow; Shitsunai jikken ni yoru ryudo den`i wo mochiita mizu michi tansa no kanosei no kento

    Energy Technology Data Exchange (ETDEWEB)

    Sato, H.; Shima, H. [Oyo Corp., Tokyo (Japan)

    1997-05-27

    To investigate a possibility of exploration of underground water flow as well as to grasp the underground fluid flow by measuring streaming potential at the ground surface, some experiments were conducted using a model unit by considering the difference of permeability. For this experimental unit, water is driven by adding head difference between the polyethylene vessel filled with water and the experimental water tank. The size of water tank is 350{times}160 mm with a height of 160 mm. Twenty platinum electrodes are set on the cover of water tank. Toyoura standard sand and Kanto loam were used for the experiments. For the experiments, fluid was injected in various combined models by considering the permeability, to measure the streaming potential. As a result, it was explained by the streaming potential that the fluid flows in a form of laminar flow in the experimental water tank, and that the movement of fluid in the Kanto loam is quite slow. It was also confirmed that the streaming potential method is an effective technique for grasping the movement of fluid. 3 refs., 8 figs.

  2. Experiment for buried pipes by stepped FM-CW radar; Step shiki FM-CW radar ni yoru maisetsukan tansa jikken

    Energy Technology Data Exchange (ETDEWEB)

    Suzuki, K.; Ito, M. [Kawasaki Geological Engineering, Co. Ltd., Tokyo (Japan); Tanabe, K. [Central Research Institute of Electric Power Industry, Tokyo (Japan)

    1997-05-27

    The underground radar exploration is adopted to surveys of cavity under the road and buried pipes since the result of high resolution is obtained. However, the explorative depth of the radar is shallow, 2-3m in soil basement, and its applicable field has been limited. The continuous wave radar (FM-CW radar) was devised to get deeper explorative depth, but has been used for the geological structure survey such as the fault survey since it is lower in resolution as compared with the pulse radar. Therefore, to make use of characteristics of the continuous wave radar and enhance resolution in the shallow part, an experiment on buried pipes was conducted for the purpose of assessing and improving the FM-CW radar. In this processing, the wave form treatment used in the reflection method seismic survey was adopted for the radar survey. There are some problems, but it is effective to adopt the same algorithm to that used in the seismic survey to the radar exploration. The explorative depth was discussed from the damping rate of electromagnetic waves and dynamic range of facilities of the experimental site, and 7m was obtained. 5 figs., 1 tab.

  3. Three-dimensional seismic survey planning based on the newest data acquisition design technique; Saishin no data shutoku design ni motozuku sanjigen jishin tansa keikaku

    Energy Technology Data Exchange (ETDEWEB)

    Minehara, M.; Nakagami, K.; Tanaka, H. [Japan National Oil Corp., Tokyo (Japan). Technology Research Center

    1996-10-01

    Theory of parameter setting for data acquisition is arranged, mainly as to the seismic generating and receiving geometry. This paper also introduces an example of survey planning for three-dimensional land seismic exploration in progress. For the design of data acquisition, fundamental parameters are firstly determined on the basis of the characteristics of reflection records at a given district, and then, the layout of survey is determined. In this study, information through modeling based on the existing interpretation of geologic structures is also utilized, to reflect them for survey specifications. Land three-dimensional seismic survey was designed. Ground surface of the surveyed area consists of rice fields and hilly regions. The target was a nose-shaped structure in the depth about 2,500 m underground. A survey area of 4km{times}5km was set. Records in the shallow layers could not obtained when near offset was not ensured. Quality control of this distribution was important for grasping the shallow structure required. In this survey, the seismic generating point could be ensured more certainly than initially expected, which resulted in the sufficient security of near offset. 2 refs., 2 figs.

  4. Application of vertical electrical sounding combined with induced polarization method in ground water exploration; IP koka wo koryoshita hiteikoho suichoku tansa no chikasui chosa eno tekiyo

    Energy Technology Data Exchange (ETDEWEB)

    Kondo, M.; Sakurada, H. [Sumiko Consultants Co. Ltd., Tokyo (Japan); Suzuki, T. [Hokkaido Development Bureau, Hokkaido Development Agency, Sapporo (Japan)

    1996-10-01

    For ground water exploration using vertical Schlumberger exploration method, measurement and analysis combined with induced polarization (IP) effect were conducted as trial. For the Schlumberger method, potential is measured at the center between potential electrodes during flow of dc current between current electrodes. In the case of vertical exploration, measurements are repeated with fixed potential electrodes by extending the distance between current electrodes. Ground water exploration was conducted using this method at Otaki village, Hokkaido. Geology of surveyed plateau consists of a basement of Pliocene tuffs and Quaternary Pleistocene sediments covering on the surface. For the results of analysis, four to seven beds were detected from the resistivity. The depth up to the lowest bed was between 25 and 85 m, the resistivity of each bed was between 9 and 8,000 ohm{times}m, and the polarizability was between 1 and 15 mV/V. Among these resistivity zones, it was judged that zones satisfying following three conditions correspond to coarse grain sediments saturated with ground water, and can be expected as aquifers; having resistivity ranging between 100 and 1,000 ohm{times}m, polarizability higher than 10 mV/V, and relatively large thickness. 11 refs., 6 figs.

  5. Depth imaging system for seismic reflection data. Part 1. Outline of system; Hanshaho jishin tansa data no tame no shindo imaging system. 1. System no gaiyo

    Energy Technology Data Exchange (ETDEWEB)

    Shimizu, N. [Japex Jeoscience Institute, Tokyo (Japan); Matsuoka, T. [Japan Petroleum Exploration Corp., Tokyo (Japan); Tsuru, T. [Japan National Oil Corp., Tokyo (Japan)

    1996-10-01

    Structures of oil and gas fields to be recently explored have changed from simple structures represented by anticline into more complicated and more delicate structures in the deeper underground. In order to discover and develop prospective oil and gas fields among such geological structures, it is indispensable to construct a system which can treat seismic exploration date collectively before stacking and can easily perform imaging of underground structures accurately. Based on the advancement of hardware, Japan National Oil Corporation and Japan Petroleum Exploration Co., Ltd. have developed a depth imaging system as an interactive tool for constructing underground structures accurately through a cooperation of highly accurate imaging technology. Using this system, two-dimensional underground structure models can be easily given and modified by interactively referring to results of depth migration velocity analysis and stacking velocity analysis, well data, cross sections after depth transform, etc. 1 fig.

  6. High-resolution aeromagnetic survey in the area of Arima-Takatsuki-Rokko active fault system; Arima Takatsuki Rokko katsudanso chiiki ni okeru komitsudo kuchu jiki tansa

    Energy Technology Data Exchange (ETDEWEB)

    Nakatsuka, T.; Okuma, S.; Morijiri, R.; Makino, M. [Geological Survey of Japan, Tsukuba (Japan)

    1996-10-01

    High-resolution aeromagnetic survey was conducted in December, 1995, over the area of Arima-Takatsuki-Rokko active fault system, where the 1995 Hyogo-South (Kobe) earthquake took place. Based on the surveyed data, the magnetic anomaly distribution in the Kei-Hanshin district was illustrated. Features of magnetic anomaly observed in it were discussed. Influence of artificial structures in the coastal zone of Kobe City was tried to be removed. Distinct magnetic anomaly observed in the center of Kyoto City was located at the southern part near Shijo-Karasuma. This was mainly affected by the artificial structure. A high magnetic anomaly with a long wave length was observed in the southern part of Kyoto. There was a high magnetic anomaly in an area surrounded by central cities of Nishinomiya-Toyonaka district. At the location where positive and negative magnetic anomalies were illustrated in NEDO`s map in the coastal zone of Kobe City, the anomaly pattern was clarified. The influence of artificial structure was approximated using a point dipole. The dipole was placed in each block having a magnetic anomaly. The parameter was determined by the inverse analysis, to remove the influence. Consequently, most of magnetic anomalies due to artificial structures could be removed. 6 figs.

  7. Comparison of {gamma}-ray profile across active normal and reverse faults; Seidansogata to gyakudansogata katsudanso ni okeru hoshano tansa kekka no hikaku

    Energy Technology Data Exchange (ETDEWEB)

    Iwata, A.; Wada, N.; Sumi, H. [Shimada Technical Consultants, Ltd., Shimane (Japan); Yamauchi, S.; Iga, T. [Shimane Univ., Shimane (Japan)

    1996-10-01

    Active faults confirmed at trench and outcrop were surveyed by the {gamma}-ray spectrometry. The active fault found at trench is a normal fault, and that found at outcrop is a reverse fault. The {gamma}-ray spectral characteristics of these two types of faults were compared to each other. The normal fault is named as Asagane fault located in Aimi-machi, Saihaku-gun, Tottori prefecture. The reverse fault is named as Yokota reverse fault located in Yokota-cho, Nita-gun, Shimane prefecture. Rises of radon gas indicating the existence of opening cracks were confirmed above the fault for the normal fault, and at the side of thrust block for the reverse fault. It was considered that such characteristics were caused by the difference of fault formation in the tensile stress field and in the compressive stress field. It was also reconfirmed that much more information as to faults can be obtained by the combined exploration method using the total counting method and the spectral method. 14 refs., 7 figs.

  8. Pseudo-random data acquisition geometry in 3D seismic survey; Sanjigen jishin tansa ni okeru giji random data shutoku reiauto ni tsuite

    Energy Technology Data Exchange (ETDEWEB)

    Minegishi, M.; Tsuburaya, Y. [Japan National Oil Corp., Tokyo (Japan). Technology Research Center

    1996-10-01

    Influence of pseudo-random geometry on the imaging for 3D seismic exploration data acquisition has been investigate using a simple model by comparing with the regular geometry. When constituting wave front by the interference of elemental waves, pseudo-random geometry data did not always provide good results. In the case of a point diffractor, the imaging operation, where the constituted wave front was returned to the point diffractor by the interference of elemental waves for the spatial alias records, did not always give clear images. In the case of multi point diffractor, good images were obtained with less noise generation in spite of alias records. There are a lot of diffractors in the actual geological structures, which corresponds to the case of multi point diffractors. Finally, better images could be obtained by inputting records acquired using the pseudo-random geometry rather than by inputting spatial alias records acquired using the regular geometry. 7 refs., 6 figs.

  9. {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.

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

    Energy Technology Data Exchange (ETDEWEB)

    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.

  11. Forward prediction of tunnel face by use of equi-traveltime planes; Tosojimen no riyo ni yoru tunnel kiriha zenpo tansa

    Energy Technology Data Exchange (ETDEWEB)

    Ashida, Y. [Kyoto University, Kyoto (Japan). Faculty of Engineering; Hirano, T. [Nishimatsu Construction Co. Ltd., Tokyo (Japan)

    1996-05-01

    The result is reported herein of a depth transform algorithm application utilizing equi-traveltime planes in reflection seismic exploration for the purpose of knowing the structure configuration in front of the tunnel face in a tunnel excavation process. A vibration producing hole was provided 0.5m above the ground surface while a vibration receiving hole was provided at 1.5m above the ground surface, and the excavated lengths were 1.5m and 0.5m, respectively. There were 24 recording channels, from which inline offset records were taken. The on-site records were subjected to 100-1000Hz band pass filtering. The elastic wave propagation rate in the rock used for depth conversion was set at 400m/s in consideration of the distance and direct wave travel time from the vibration source to the vibration receiving point. As the result of study, weak layers were found in the neighborhood of 230-240m, 260-270m, and 280-290m. This method requires less core memory for calculation and completes calculation in a shorter period of time, which enables a conclusion that it will be effective in grasping the 3-dimensional structure in front of the tunnel face in the working scene. 4 refs., 7 figs.

  12. Geophysical exploration of sedimentary layers for estimation of strong ground motion; Jishindo hyoka no tame no chika kozo tansa to sono katsuyo

    Energy Technology Data Exchange (ETDEWEB)

    Yamanaka, H.; Kurita, K. [Tokyo Institute of Technology, Tokyo (Japan)

    1997-12-01

    This paper introduces the result of a case study in the Kanto Plain, Japan on estimation of strong ground motion taking underground structure into account and exploration of the underground structures. Methods for estimating the strong ground motion may be classified into the following three methods: an empirical method represented by the distance attenuation expression, a semi-empirical method, in which small to medium earthquakes occurred in the vicinity of a focus fault of the subject earthquake are conceived as a Green function, and superposed according to the analogy of the earthquakes, and an analytic method. These three approaches are used respectively in the present situation. Micro motion array observation is being carried at a large number of points in the Kanto Plain to explore S-wave velocity structures. Seven seismograph arrays have observed micro motions with slightly long cycles, phase velocities of Raleigh waves were derived, and then S-wave velocity distribution down to the seismic base was estimated from reverse analysis therefrom. S-wave amplification characteristics were calculated by using one-dimensional duplicate reflection on the prepared ground bed model. The result well explains the observation values, indicating that the ground bed model is reasonable for estimating the seismic motion amplifying characteristics. 33 refs., 10 figs., 1 tab.

  13. Interpretation of seismic section by acoustic modeling. Study of large amplitude events; Hadoba modeling ni yoru jishin tansa danmen no kaishaku. Kyoshinhaba event ni taisuru kosatsu

    Energy Technology Data Exchange (ETDEWEB)

    Tamagawa, T.; Matsuoka, T.; Sato, T. [Japan Petroleum Exploration Corp., Tokyo (Japan); Minegishi, M.; Tsuru, T. [Japan National Oil Corp., Tokyo (Japan)

    1996-05-01

    A large amplitude event difficult to interpret was discovered in the overlap section in offset data beyond 10km targeting at deep structures, and the event was examined. A wave field modeling was carried out by use of a simplified synclinal structure model because it had been estimated that the large amplitude event had something to do with a synclinal structure. A pseudospectral program was used for modeling the wave field on the assumption that the synclinal structure model would be an acoustic body and that the surface would contain free boundaries and multiple reflection. It was found as the result that a discontinuous large amplitude event is mapped out in the synclinal part of the overlap section when a far trace is applied beyond the structure during a CMP overlap process. This can be attributed to the concentration of energy produced by multiple reflection in the synclinal part and by the reflection waves beyond the critical angle. Accordingly, it is possible that phenomena similar to those encountered in the modeling process are emerging during actual observation. 2 refs., 8 figs.

  14. 2D resistivity survey in complex geological structure area. Application to the volcanic area; Fukuzatsuna chishitsu kozo chiiki ni okeru hiteiko nijigen tansa. Kazangan chiiki deno tekiorei

    Energy Technology Data Exchange (ETDEWEB)

    Asakawa, S.; Ikuma, T.; Tanifuji, R. [DIA Consultants Co. Ltd., Tokyo (Japan)

    1996-05-01

    Introduced herein is an application of 2D resistivity survey to a volcanic rock area where the survey result is difficult to interpret because of its complex geological structure. In a dam site survey, main problems involve the permeability of water through faults and weathered, altered zones. At this site, a 2D resistivity survey was conducted, a 2D geological structure was deduced from the resistivity section, and the result was examined. It was found that resistivity distribution was closely related to hydrographic factors, but no obvious correlation was detected between rock classes and R, Q, and D. In conducting investigations into a section planned for a highway tunnel, it was learned that the problem was a volcanic ash layer to collapse instantly upon absorbing water, and the distribution of the ash layer, not to be disclosed by boring, was subjected to a 2D resistivity survey. The survey was conducted into the structure above where the tunnel would run, and further into the face, and studies were made about what layer was reflected by the resistivity distribution obtained by analysis. The result of the analysis agreed with the details of the layer that was disclosed afterward. 4 figs., 1 tab.

  15. Seismic refraction analysis with high accuracy based on traveltime modeling; Basu keisan wo base to shita kussekiho jishin tansa kaiseki no koseidoka

    Energy Technology Data Exchange (ETDEWEB)

    Saito, H.; Hayashi, K. [OYO Corp., Tokyo (Japan)

    1996-05-01

    For the purpose of enhancing the efficiency of analytical processes so that those not equipped with high skill may perform a certain level of analysis and that analysis precision may be improved, some analytical techniques based on path calculation were examined. As the result, a flow of work has become feasible, wherein an early model is constructed by use of a tomography-assisted analysis to be accomplished automatedly and the result is then converted into a layer system with the velocity and thickness to be automatically corrected for the determination of the ultimate velocity layer section. Following this flow of work, almost all the parts of the work may be accomplished automatically once the travel time curve is completed. Furthermore, the calculated travel time obtained by this method can be easily compared with the observed travel time creating an opportunity to show the high reliability of this method, for this to be accepted as a standard for evaluating the accuracy of exploration. It has also been found that this method may be applied to more complicated structures which fail to satisfy the conditions for a structure to be treated by other methods such as `Hagiwara`s method.` 3 refs., 5 figs.

  16. Fiscal 1995 verification survey of geothermal exploration technology. Report on a deep geothermal resource survey; 1995 nendo chinetsu tansa gijutsu nado kensho chosa. Shinbu chinetsu shigen hokokusho

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    1996-06-01

    For the purpose of reducing the risk of deep geothermal resource development, the paper investigated three factors for the formation of geothermal resource in the deep underground, that is, heat supply from heat source, supply of geothermal fluids, and the developmental status of fracture systems forming reservoir structures. The survey further clarified the status of existence of deep geothermal resource and the whole image of the geothermal system including shallow geothermal energy in order to research/study usability of deep geothermal resource. In the deep geothermal resource survey, drilling/examination were made of a deep geothermal exploration well (`WD-1,` target depth: approximately 3,000-4,000m) in the already developed area, with the aim of making rationalized promotion of the geothermal development. And the status of existence of deep geothermal resource and the whole image of the geothermal system were clarified to investigate/study usability of the geothermal system. In fiscal 1995, `WD-1` in the Kakkonda area reached a depth of 3,729m. By this, surveys were made to grasp the whole image of the shallow-deep geothermal system and to obtain basic data for researching usability of deep geothermal resource. 22 refs., 531 figs., 136 tabs.

  17. Interface physical chemistry of enamels (Part 1). Examination of cobalt and nickel behevior and adhesion of enamel; Hourou ni kansuru kaimen butsuri kagakuteki kenkyu (1). Micchakusei ni oyobosu cobalt to nickel no kyodo no kento

    Energy Technology Data Exchange (ETDEWEB)

    Shimizu, T.; Shirasaki, M.; Kozuka, T. [Chiba Inst. of Tech., Narashino (Japan)] Zhaohua, J. [Harbin Institute of Technology Harbin (China). Applied Chemisty] Kawashima, T. [Ikebukuro Horo Kogyo Co. Ltd., Saitama (Japan)

    1998-02-01

    Observation of the enameles interface with SEM, EPMA and ESCA, and measurement of adhesive strength of the enameles were done. Simultaneously, cobalt and nickel in the enamel layer examined a given influence at the interface and the adhesive strength. As a result, the relationship between iron-oxygen, cobalt-oxygen and nickel-oxygen, at the reaction of enamel process was explained by the interface thermodynamics. Furthermore, characteristics and differences of reaction of cobalt and nickel were clarified. (1) The adhesive ability of Co-enamel was larger than that of Ni-enamel. (2) The adhesive behavior of cobalt changes at about 730degC, but that of nickel remains unchanges. Consequently, cobalt has an adhesion with the high temperature (over 730degC) but nickel does not have an influence on the temperature. (3) At high firing temperature, the Co-enamel can create FeO easily compared with Ni-enamel, and dissolve Fe{sub 2}O{sub 3} of steel surface into glass. (4) Cobalt spreads for a vertical direction of interface, but nickel tends deposition on the interface surface. And the diffusion capability of cobalt into the steel was considerably greater than that of nickel. 18 refs., 7 figs., 3 tabs.

  18. Physical model experiment for wave field measurements by means of laser Doppler vibrometer. Measurement of three components; Laser Doppler shindokei ni yoru butsuri model jikken. Hado sanseibun no kenshutsu

    Energy Technology Data Exchange (ETDEWEB)

    Nishizawa, O.; Sato, T. [Geological Survey of Japan, Tsukuba (Japan); Lei, X. [DIA Consultant Co. Ltd., Tokyo (Japan)

    1997-05-27

    In this experiment, a beam incident from an oblique direction is reflected by a spherical lens toward the direction of incidence. When the surface of a matter is vibrated by elastic waves, the spherical lens comes into a translation motion that accompanies the vibration. It follows accordingly that the vibration on the surface of the matter may be detected by sensing the spherical lens travelling speed. Three components of the vibration may be determined if beams are focused at one spot from three directions. Detection of the S-wave component by LDV (laser Doppler vibrometer) discloses the complicated wave field in a heterogeneous material, and this physical model experiment may be utilized in various fields of study. For instance, information about problems that may surface in the field work may be collected beforehand in a physical model experiment for developing an S-wave-aided probing method. For the study of seismic wave propagation in a complicated three-dimensional ground structure, a numerical model is not enough, and a physical model experiment will be an effective method to fulfill the purpose. In the monitoring of cracks in a rock, again, not only elastic wave velocity but also waveform information collected from a physical model experiment should be fully utilized. 6 refs., 6 figs.

  19. Post-disaster recovery and support in Japan

    Directory of Open Access Journals (Sweden)

    Kimiaki Kawai

    2014-11-01

    Full Text Available As a locally based faith-based organisation, there were several aspects that enabled Soka Gakkai to contribute effectively to the relief effort following the March 2011 earthquake and tsunami in Japan, responding to both physical and psychological needs.

  20. On Attitudes toward Education: The Attitude toward Guiding Learning and the Attitude toward Learning [1936

    Science.gov (United States)

    Makiguchi, Tsunesaburo

    2015-01-01

    This "From the Archives" article was originally published in Japanese in v6 n3 Mar 1936 of the Japanese-language journal "Shinkyo" (New Teachings), a periodical publication of the Soka Kyoiku Gakkai, the Society for Value-Creating Education, established by Tsunesaburo Makiguchi in 1930. This installment of "On Attitudes…

  1. FY 1995 report on verification of geothermal exploration technology. Development of fracture reservoir exploration technology (development of seismic exploration); 1995 nendo chinetsu tansa gijutsunado kensho chosa. Danretsugata choryuso tansaho kaihatsu (danseiha riyo tansaho kaihatsu) hokokusho

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    1996-03-01

    This report provides the development of new exploration technology using elastic waves, such as reflection seismic survey, VSP, and seismic tomography, for precisely characterizing subsurface fractures in geothermal reservoirs. In order to investigate and improve the effective data acquisition and analysis methods for detecting a fault type of fractures, an experiment of a seismic tomography method was conducted using wells drilled in the Ogiri geothermal field, Aira-gun, Kagoshima Prefecture. An experiment of propagation characteristics of piezo type underground seismic source in the volcanic field was also conducted as a trend survey of underground seismic sources. The fracture type in the model field was systematically analyzed by measuring the core samples obtained in the demonstration test field through remanence measurement, fluid inclusion measurement, and zircon measurement using test equipment, and by analyzing results obtained from cores and results of seismic tomography obtained from the wells. Based on these results, the effectiveness and practical application of exploration methods using elastic waves were investigated. 80 refs., 250 figs., 49 tabs.

  2. Fiscal 1996 verification survey of geothermal exploration technology. Development of the fracture type reservoir exploration method (development of the elastic wave use exploration method); 1996 nendo chinetsu tansa gijutsu nado kensho chosa. Danretsugata choryuso tansaho kaihatsu (danseiha riyo tansaho kaihatsu)

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    1997-03-01

    For the purpose of exploring accurately fracture groups greatly restricting the fluid flow of geothermal reservoirs, technical development was made for applying the elastic wave exploration technology such as the high precision reflection method, VSP, elastic wave tomography to the geothermal exploration. The Okiri area, Kagoshima prefecture was selected as a demonstrative field of a typical type where the steep and predominant fracture rules the geothermal reservoir, and experiments were conducted using the high precision reflection method and VSP. Fracture models were made, and the analysis results were studied by a survey using the array CSMT/MT method and by a comparison with existing data. Reformation of the underground receiving system used for VSP and elastic tomography is made for improvement of its viability, and was applied to the VSP experiment. The treatment/analysis system of the core analyzer was improved, and cores of the demonstrative field were analyzed/measured. Further, the exploration results, core analysis results and existing data were synthetically analyzed, and fracture models of the demonstrative field were constructed. Also, effectiveness and viability of the elastic wave use exploration method were studied. 90 refs., 418 figs., 24 tabs.

  3. Modified spatial autocorrelation method using autoregressive model for estimating underground velocity structure from microtremor array observation; Bido array tansa ni okeru kukan jiko sokanho no jiko kaiki model wo mochiita kairyo

    Energy Technology Data Exchange (ETDEWEB)

    Yamamoto, H.; Saito, T. [Iwate University, Iwate (Japan). Faculty of Engineering; Obuchi, T. [Kawasaki Geological Engineering Co. Ltd., Tokyo (Japan)

    1998-02-01

    Spatial autocorrelation method (SAC) is an effective analysis for estimating underground S-wave velocity structure from microtremor phase velocity dispersion relation because it has larger detectable range of microtremor wavelength than frequency-wavenumber analysis. However, phase velocities estimated by conventional SAC methods such as band-pass filtered method or Fast Fourier Transform method were not precise if suitable band width was not selected for analysis. We proposed a new technique for SAC using autoregressive model which estimated spectra with high resolution because the best fitting model can be selected using AIC. We apply the new method to calculate phase velocities of microtremors which were observed at a ground of Morioka Technical High School with arrays. As a result, phase velocities calculated by the new method were continuous with frequency although those calculated by the conventional methods were scattered. This indicates that SAC functions calculated by the new method are estimated better than those by conventional SAC methods. 13 refs., 7 figs.

  4. Reduction of artificial source effect in the high-resolution aeromagnetic survey in the Hanshin region; Hanshin chiiki no komitsudo kuchu jiki tansa ni okeru jinko noise source no eikyo no jokyo

    Energy Technology Data Exchange (ETDEWEB)

    Nakatsuka, T.; Makino, M.; Morijiri, R.; Okuma, S. [Geological Survey of Japan, Tsukuba (Japan)

    1997-05-27

    A high-resolution aeromagnetic survey was carried out in December 1995 on areas from Kobe City to Kyoto City in relation to the Hyogoken-nanbu Earthquake in 1995. It was found in the survey that effects of electric trains driven by direct current and man-made structures cannot be avoided, working as a large noise factor in extraction and analysis of geological information. This paper describes a quantitative analysis on magnetic anomaly suspected to have been caused from artificial sources seen in the magnetic map of the Hanshin area obtained from the above exploration data. The paper also gives considerations on methods to remove the effects therefrom. It then describes a quantitative analysis and the result of attempts on removal of the anomaly, taking up the following factors: (1) distribution of specific and remarkable magnetic anomalies which correspond to railroad positions of the Hanshin Railways running through the Nishinomiya-Toyonaka area, (2) the magnetic anomaly trend in positive and negative pair seen in the seafront area of Kobe City, and (3) typical bipolar isolated type magnetic anomaly in the north-west part of Kobe City. The cause for (1) was loop current flown for the railway operation, that for (2) was man-made structures in the improved seafront area, and that for (3) was a provisionally built metal waste storage yard. 9 figs.

  5. Generation of seismic base map using satellite images in the southern deltaic area, People`s Republic of Bangladesh; Eisei data ni motozuku jishin tansa base map no sakusei (Bangladesh nanbu delta no rei)

    Energy Technology Data Exchange (ETDEWEB)

    Kotera, Y. [Japan Energy Corp., Tokyo (Japan); Ochi, M. [Nikko Exploration and Development Co. Ltd., Tokyo (Japan); Hato, M. [Earth Remote Sensing Data Analysis Center, Tokyo (Japan)

    1997-05-27

    Assuming a two-dimensional seismic survey in a mangrove jungle in the southeast part of People`s Republic of Bangladesh and trially making a basemap for the survey plan from images of satellites such as LANDSAT, the paper considered the use and marginal use in the case of using satellite remote sensing for such a use field. When utilizing water channels in the mangrove jungle in the southwest of Bangladesh and using the seismic survey method for shallow sea, it is important to grasp the distribution of channels in the planning stage of the survey. Satellite remote sensing data are extremely important for knowing the wide-regional information including factors of hourly variations. In the area for this survey, for directly recognizing the channel, it is good only if the difference in reflectance between water and substances except water is indicated in the image because of flatness of the topography. There was seen few difference in accuracy between the passive multispectral image and the active SAR image which is sensitive to topographical changes. 2 figs.

  6. Geological and geochemical survey of gas hydrate deposits. Present status and future problems of R/D program; Gasuhaidoredo kosho no chishitsu {center_dot} chikagaku tansa. Genjo to kadai

    Energy Technology Data Exchange (ETDEWEB)

    Matsumoto, R. [The Unibersity of Tokyo, Tokyo (Japan)

    1999-11-25

    Recent development of marine geological/geophysical investigations have revealed that (1) gas hydrates are widely distributed in deep shelf to slope sediments and (2) gas-hydrate-bearing sediments are underlain by a relatively thick free gas zone. This implies that [gas hydrate deposits] should be considered as a package of soild hydrate and free gas. An important parameter in resource evaluation is volume assessment of methane reserves, however, there are a number of issues to estimate even the total amount of methane trapped in gas hydrate deposits. There are a number of issues to be solved to estimate recoverable reserves of gas hydrate deposits. The issues include the discrepancy between BSR and BGHS and the nature and origin of double BSRs. Also another urgent and important theme is the generic link between gas hydrate formation and bacterial activity of deep biosphere. Stratigraphic Drilling of [Nankai Trough] by JNOC in 1999 and planned ODP drilling in the western Nankai Trough in 2000 are[expected to give clues to solve these problems. (author)

  7. Fiscal 1996 verification survey of geothermal exploration technology. Development of the fracture type reservoir exploration method (development of the elastic wave use exploration method); 1996 nendo chinetsu tansa gijutsu nado kensho chosa. Danretsugata choryuso tansaho kaihatsu (danseiha riyo tansaho kaihatsu)

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    1997-03-01

    For the purpose of exploring accurately fracture groups greatly restricting the fluid flow of geothermal reservoirs, technical development was made for applying the elastic wave exploration technology such as the high precision reflection method, VSP, elastic wave tomography to the geothermal exploration. The Okiri area, Kagoshima prefecture was selected as a demonstrative field of a typical type where the steep and predominant fracture rules the geothermal reservoir, and experiments were conducted using the high precision reflection method and VSP. Fracture models were made, and the analysis results were studied by a survey using the array CSMT/MT method and by a comparison with existing data. Reformation of the underground receiving system used for VSP and elastic tomography is made for improvement of its viability, and was applied to the VSP experiment. The treatment/analysis system of the core analyzer was improved, and cores of the demonstrative field were analyzed/measured. Further, the exploration results, core analysis results and existing data were synthetically analyzed, and fracture models of the demonstrative field were constructed. Also, effectiveness and viability of the elastic wave use exploration method were studied. 90 refs., 418 figs., 24 tabs.

  8. Experiment for detecting metallic-bars in concrete using new 1.5 GHz antenna; Shingata no 1.5 GHz antena wo mochiita konkureto nai no tekkin tansa jikken

    Energy Technology Data Exchange (ETDEWEB)

    Nakabayashi, Yuko; Toshioka, Tetsuma; Goebuchi, Toru [Oyo Corp., Tokyo (Japan)

    1999-02-01

    In recent years, maintenance was increasingly needed with the aging of the concrete structures. It has been paid attention to the underground radar detection as a non-destructive detection methods in order to confirm the bar arrangement situation inside concrete. However, in the metallic bar detection using the common underground radar, it was difficult to identify the metallic bar position and concrete cover thickness when an interval of metallic bars was dense or arrangement of metallic bars was overlapped, in a case of which the metallic bars were buried in extremely shallow areas such as metallic bar concrete wall. In the application experiments of this time, it was confirmed by using the new and high frequency antenna with central frequency of 1.5 GHz that the metallic bar position and concrete cover thickness could be identified which position and concrete cover thickness were difficultly identified by the common methods by the underground radar detection in arrangement of metallic bars. (translated by NEDO)

  9. Development of buried cable location survey system by underground rader for power distribution cables under pavements. Haiden chichuka no tame no chika radar ni yoru maisetsukan tansa system no kaihatsu

    Energy Technology Data Exchange (ETDEWEB)

    Suzuki, K.; Kitano, K.

    1990-06-01

    To execute construction work for power distribution cables under pavements reasonably, it is important to develop a technology capable of non-destructive detection of the location of existing buried cables from the ground surface. This study is to clarify the principle, measurement method, effectiveness, and limitation of the underground radar system which is at present considered as the most effective survey method for buried cables. In this system, accuracy in measuring the depth of underground cable location by a separated type antenna has been improved, software to improve resolution by a migration process has been developed, and a compact survey system which can analyze the data on the site has been realized. As aresult of the survey at city areas, all pipes buried less than 1m in depth with the resistivity value of more than 100 {Omega} m were detected as well as those less than 2m in depth with more than some 100 {Omega} m. However, non-metal pipes buried deeper than 1m in the ground of less than 100 {Omega} m were not detected. Consequently, improvement of the system is necessary in future. 7 refs., 23 figs., 6 tabs.

  10. Practical use of technology for exploring obstacles and soil collapse state around shield machine using underground radar; Chichu reda wo mochiita shirudo ki shuhen no shogaibutsu to dosha hokai jotai tansa gijutsu no jitsuyoka

    Energy Technology Data Exchange (ETDEWEB)

    Tanimoto, K. [Mitsubishi Heavy Industries Ltd., Tokyo (Japan)

    1995-04-25

    A report is made on the outline and the used result of a newly developed `underground radar.` The objects for underground exploration in shield tunneling methods are divided broadly into obstacles, state of the peripheral ground, and geological change in the working place. Electromagnetic method is employed for the exploration method of this system which can explore the ground conditions very accurately and in real time although the explorable distance is a little limited. As to antennas, there are two types, i.e. the separate transmitter and receiver antenna and the integrated transceiver antenna. The antennas are mounted at the side of cutter face, at the shield machine fixed side, and at the front of the cutter face. The system configuration varies according to the type of antenna and the displaying location of the explored result. The system introduced in this report consists of a radar antenna, antenna control device, slip ring, measurement control computer, and monitoring computer. A report is made on the condition of an existing buried pipe found accidentally during drilling with a shield machine. 12 figs., 1 tab.

  11. Utilization of two-way multicore cables and comparison of various electrode configurations in electrical prospecting; Denki tansa ni okeru sohokogata tashin cable no riyo to kakushu dekyoku haichi no hikaku

    Energy Technology Data Exchange (ETDEWEB)

    Takakura, S. [Geological Survey of Japan, Tsukuba (Japan); Matsushima, J. [The University of Tokyo, Tokyo (Japan). Faculty of Engineering

    1996-10-01

    For more precise electrical prospecting, the new multicore cable was developed to allow high-density measurement by conventional equipment. Since conventional multicore cables are inferior in cost, length and weight, the new cable is composed of an n-conductor cable, two n-conductor male connectors and n lead wires. For connection of the multi-conductor cable and lead wires, cable sheath is peeled at n points at specific intervals. Sheath of the k-th conductor is peeled at k-th point from the terminal, and restored for insulation after connection of the conductor and lead wire. The male connectors are attached to the both ends of the multi-conductor cable. Since this two-way type cable can be used at every end, the measuring equipment can measure at one divisional point after another of a long measuring line while shifting the equipment from one point to another. All measurements are perfected only with two short cables. Resistivities were successfully measured along the long measuring line of 480m long with 97 electrodes arranged at intervals of 5m. Various electrode configurations were also compared. 1 ref., 4 figs., 2 tabs.

  12. Investigation of data acquisition parameters for Minami Noshiro 3D experiment using 3D seismic modeling; Sanjigen hado denpa modeling wo riyoshita Minami Noshiro sanjigen jishin tansa data shutoku parameter no kento

    Energy Technology Data Exchange (ETDEWEB)

    Tanaka, H.; Nakagami, K.; Minegishi, M. [Japan National Oil Corp., Tokyo (Japan). Technology Research Center; Kano, R. [Teikoku Oil Co. Ltd., Tokyo (Japan)

    1996-10-01

    This paper describes how to grasp the characteristics of reflected waves which means how the reflected wave can be received in its magnitude depending on the complicated subsurface structure. Data acquisition parameters were also investigated, as to offset distance distribution and mute setting during the HMO correction. A velocity structure model was prepared for an area of 9km{times}8km including the given 3D seismic exploration area at Minami Noshiro, Akita Prefecture. For the geological sequence used for the velocity structure model, three formations, i.e., Katsurane Formation, Funakawa Formation, and Onagawa Formation, were inputted in an order from the shallower depth on the basis of the depth structure profile obtained from the previous data. Ray tracing was calculated by means of the two-dot dashed line tracing method. For this method, amplitude as well as travel time of waves can be calculated at the same time. This was effective for grasping the magnitude of reflected wave on simulating the traced data. For the velocity structure model used in this study, existing data inputted were old, which limited the quantity of information. However, this model would sufficiently contribute to the verification of survey design and the determination of optimal layout. 1 ref., 3 figs.

  13. Fiscal 1998 overseas geological structure survey. Japan-China joint coal survey Mei-Xian project; 1998 nendo kaigai chishitsu kozo nado chosa hokokusho. Nippon Chugoku sekitan kyodo tansa Mei-Xian project

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    1999-03-01

    Japan-China joint coal survey was made through seismic prospecting by Japanese group and drilling prospecting by Chinese group. Mei-Xian mine property includes coal seams of the Jurassic period, and is covered with the quaternary period stratum without any coal seam. The base of the quaternary period stratum exists at depth of 50-400m, while the coal seams at depth of 300-700m. Among 11 existing seams, the 1st and 5th seams are main objects for prospecting. The 5th seam of 0.2-8.96m (2.95m in average) thick is the most expected important one, distributing all over the mine property. The 5th seam also has branch seams spreading over 2.5km from east to west and 1.2km from south to north in the center part of the mine property. The 1st seam of 0-8.62m (2.90m in average) thick is most thick in the south part of the mine property. The theoretical amount of coal deposits in the whole coal seam is estimated to be nearly 290,000,000t by Chinese group (nearly 50% of it in the 5th seam). That is also estimated to be nearly 346,000,000t by Japanese group (155,000,000t in the 5th seam). Both 1st and 5th seams are composed of sub-bituminous coal. (NEDO)

  14. Verification survey of geothermal exploration technology, etc. Report on the result of the developmental research on the development of the fracture type reservoir exploration method; Chinetsu tansa gijutsu nado kensho chosa. Danretsugata choryuso tansaho kaihatsu kenkyu kaihatsu seika sokatsu hokokusho

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    1997-03-01

    For the purpose of grasping fracture groups forming geothermal reservoirs with accuracy, the development of the fracture type reservoir exploration method has advanced the technical development of exploration methods of seismic wave use, electromagnetic induction use, and micro-earthquake use. This paper summarized main results of the development and problems to be solved in the future. In the development of the seismic wave use exploration method, the high accuracy reflection method using seismic wave, VSP and seismic tomography were adopted to the geothermal field, and technology effective for the exploration of fracture type reservoirs was developed. In the development of the electromagnetic induction use exploration method, the array CSMT method which can measure multiple stations along the traverse line at the same time was developed with the aim of grasping effectively and accurately fracture groups forming geothermal reservoirs as changes of resistivity in the shallow-deep underground. In the fracture group forming geothermal reservoirs, micro-earthquakes are generated by movement of thermal water and pressure variations. In the development of the micro-earthquake use exploration method, developed was the micro-earthquake data processing and analysis system (MEPAS). 179 refs., 117 figs., 28 tabs.

  15. Confirmation study of the effectiveness of prospect techniques for geothermal resources. Deep-seated geothermal resources survey report (Fiscal year 1994); 1994 nendo chinetsu tansa gijutsu nado kensho chosa. Shinbu chinetsu shigen chosa hokokusho

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    1996-03-01

    Drilling and survey of deep geothermal exploration wells were conducted to grasp the existing situation of deep geothermal resource and the whole image of geothermal systems in the area where geothermal resource was already developed. In the drilling work in fiscal 1994, 4000m-class rigs and the top drive system were planned to be used for drilling of 12-1/4 inch wells, but 9-5/8 inch liners were used for drilling down to depths of 2550m or deeper since the amount of lost circulation is large and the withdrawal of devices may be very difficult. And in 8-1/2 inch wells, the well was drilled down to a depth of 2950m. As to the deep resistivity exploration technology using electromagnetic method, studies were made of a multiple-frequency array induction logging (MAIL) method, a vertical electromagnetic profiling (VEMP) method, a joint analysis method, etc. Concerning the synthetic fluid inclusion logging technology, containers were lowered into the well and a comparison was made between data of the homogenization temperature analysis of the formed fluid inclusion and those of the temperature log analysis. With relation to the making of deep geothermal structural models, revision was made according to the determination of depths of Miocene formations, Pre-tertiary formations, and the Kakkonda granite. 65 refs., 268 figs., 79 tabs.

  16. Fiscal 1997 report on the survey of overseas geological structures, `the Tanjungenim Coal Exploration Project between Japan and Indonesia`; 1997 nendo kaigai chishitsu kozonado chosa `Nippon Indonesia sekitan kyodo tansa Tanjungenim project`

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    1998-03-01

    The basic survey for coal mine development was conducted in the Banjarsari area of Tanjungenim, Sumatra, Indonesia. In the survey, Japan deals with ground surface exploration, borehole physical survey, VSP survey and seismic survey, and Indonesia exploratory drilling, topographical mapping, measurement, hydrologic/hydraulic survey, access road formation, etc. The boreholes drilled are 35 in number and 4004m in total drilling length. The borehole physical survey was conducted in all 35 holes. The seismic survey was conducted on 5 traverse lines and in a total length of 10.19km, and the VSP survey in two boreholes. As a result of the survey, it was found out that there existed a large amount of coal reserve in a comparatively shallow area in the south-central part of the Banjarsari area. There exist faults, which has no great effects on the open pit mining. There is a high possibility of developing large-scale coal mines of open pit mining type with a comparatively low soil removing ratio. Concerning the coal quality, the heating value is comparatively low, the latter half of a 4000 kcal/kg level. It can be expected to realize a pit-mouth power plant which is low in coal carrying cost. 129 figs., 28 tabs.

  17. Estimation of subsurface structures in a Minami Noshiro 3D seismic survey region by seismic-array observations of microtremors; Minami Noshiro sanjigen jishin tansa kuikinai no hyoso kozo ni tsuite. Bido no array kansoku ni yoru suitei

    Energy Technology Data Exchange (ETDEWEB)

    Okada, H.; Ling, S.; Ishikawa, K. [Hokkaido University, Sapporo (Japan); Tsuburaya, Y.; Minegishi, M. [Japan National Oil Corp., Tokyo (Japan). Technology Research Center

    1997-05-27

    Japan National Oil Corporation Technology Research Center has carried out experiments on the three-dimensional seismic survey method which is regarded as an effective means for petroleum exploration. The experiments were conducted at the Minami Noshiro area in Akita Prefecture. Seismometer arrays were developed in radii of 30 to 300 m at seven points in the three-dimensional seismic exploration region to observe microtremors. The purpose is to estimate S-wave velocities from the ground surface to the foundation by using surface waves included in microtremors. Estimation of the surface bed structure is also included in the purpose since this is indispensable in seismic exploration using the reflection method. This paper reports results of the microtremor observations and the estimation on S-wave velocities (microtremor exploration). One or two kinds of arrays with different sizes composed of seven observation points per area were developed to observe microtremors independently. The important point in the result obtained in the present experiments is that a low velocity bed suggesting existence of faults was estimated. It will be necessary to repeat experiments and observations in the future to verify whether this microtremor exploration method has that much of exploration capability. For the time being, however, interest is addressed to considerations on comparison with the result of 3D experiments using the reflection method. 4 refs., 7 figs.

  18. Leading research report for fiscal 1998 on the super-survey (Next-generation underground exploration technology); 1998 nendo super survey (jisedai chika tansa gijutsu) no chosa kenkyu sendo chosa kenkyu hokokusho

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    1999-03-01

    Researches are conducted on innovative mineral resources exploration technologies which use seismic waves or scattered electromagnetic waves to grasp the 3-dimensional structure in the ground. In fiscal 1998, a concrete research and development program is formulated, under which the seismic method and electromagnetic method will deal with an approximately 1km{sup 2}-large area of metalliferous deposit seated approximately 500m deep. In addition, researches are conducted overseas on the trend of related technologies. At an NMR (nuclear magnetic resonance) workshop held at the Society of Exploration Geophysicist, U.S., application of the NMR method to water is suggested. At a European Geophysical Society of environmental research and civil engineering event, useful knowledge is acquired about a 4-dimensional sounding (monitoring) technique in which a time axis is added to the 3-dimensional sounding technique and a high-resolution high-efficiency sounding system for probing shallow layers. During visits at Australian institutes concerned with the electromagnetic sounding technology, the trend of probing technologies especially those using the superconducting quantum interface device (SQUID) is gasped. (NEDO)

  19. Time domain electromagnetic method for petroleum exploration. Part 3. Case study in Yoneyama area; Sekiyu tansa ni okeru TDEM ho data shutoku to kaiseki ni tsuite. 3. Niigataken Yoneyama chiiki deno tekiyorei

    Energy Technology Data Exchange (ETDEWEB)

    Ishikawa, H.; Mitsuhata, Y. [Japan National Oil Corp., Tokyo (Japan); Shiga, N. [Mitsui Mineral Development Engineering Co. Ltd., Tokyo (Japan)

    1996-05-01

    The result is reported of a TDEM method-based survey for oil exploration conducted in the Yoneyama district, Niigata Prefecture. The survey covered the southern part of the sedimentary basin in the prefecture, known for the poor quality of the seismic prospecting data that had been recorded. The purpose of the TDEM method-assisted survey was to probe the high-resistivity volcanic rock structure and low-resistivity sedimentary layer, and to know their details. The obtained data were subjected to interpretation by use of the 1D inversion method. A 4000m-deep level was subjected to interpretation, 34 data were inputted, and the early model consisted of 20 layers. As the result, it was found that there was a high-resistivity layer ranging from the ground surface down to a depth of approximately 500m, that a low-resistivity layer 2500-3000m in thickness lay thereunder, and that the lowest layer had a high resistivity of approximately 100 Ohm m. By comparing these data with the geological structure, structures were disclosed corresponding to the rock bed depth, Ukawa syncline, Ishiguro anticline, and Yoneyama mountain mass. 3 refs., 10 figs., 1 tab.

  20. Joint analysis of refraction seismic survey with multilevel hydrophone measurement (application for detecting the high velocity thin lid); Kussekiho jishin tansa data to kochu hydrophone data no fukugo kaiseki no rei

    Energy Technology Data Exchange (ETDEWEB)

    Mori, S.; Harada, T.; Hayashi, K. [OYO Corp., Tokyo (Japan)

    1996-05-01

    During a refraction seismic survey conducted at a spot where a high-speed lava layer is supposedly concealed, the distribution of lava layer was estimated, and a composite analysis involving the vibration data received via hydrophones arranged in a bore hole was accomplished using a high-speed model based on an assumed geological section. The refraction survey centered on the bore hole and was accomplished using 250m-long traverse lines extending therefrom, one to the upstream and the other to the downstream of a river, producing a total length of 500m. The hydrophones were installed in the bore hole, and the measurement was carried out in an offset VSP-like observation pattern. In the analysis, the velocities obtained by the refraction survey and velocity logging were assigned to each layer on the basis of the assumed geological section for the construction of a velocity distribution model, which served as the early model for the repetition of calculation. Calculation was repeated with help of the said model, and a geological structure, capable of explaining the travel time data collected during the refraction survey and velocity logging, was successfully estimated. 1 ref., 5 figs.

  1. Processing of the reflection seismic data which were acquired in the continental shelf off the north-west Australia; Australia hokusei tairikudana chiiki ni oite shutokusareta hanshaho chishitsu tansa data no shori ni tsuite

    Energy Technology Data Exchange (ETDEWEB)

    Amano, H. [Japan National Oil Corp., Tokyo (Japan)

    1996-05-01

    Reflection exploration of earthquakes was conducted in the continental shelf off the north-west Australia, and a report is made concerning the processing of the acquired data. A GI gun was used as the vibration source, and a wave quite similar to a pulse was generated. Hydrophones were arranged with group intervals of 12.5m, and high-resolution field data were acquired. An analog low cut filter was used to suppress the large-amplitude swell noise attributable to sea conditions. A digital filter was designed for the purpose of eliminating coherent noises from other survey ships. At the ultimate stage the f-k filter was applied to each of the shot records, and the effectiveness was verified. The traverse line was as long as 6700km and therefore the design window was set relatively long at 2.0-4.0s in the residual static correction phase. It was found that this setup is effective in improving the continuity of the reflection surface. 5 figs., 1 tab.

  2. Model experiment on detection and monitoring of fractures by using air as a tracer for seismic wave. 2; Kitai wo tracer to shita kiretsu no danseiha tansa no model jikken. 2

    Energy Technology Data Exchange (ETDEWEB)

    Watanabe, T.; Takami, Y.; Ishiga, T.; Sassa, K. [Kyoto University, Kyoto (Japan). Faculty of Engineering

    1996-05-01

    Clearance provided between two flat resin blocks (being stacked) used as a model of a crack in rocks was subjected to an experiment to investigate elastic wave propagation characteristics when the crack is filled with water and when injected with air. This paper reports the result of the experiment. The experiment was carried out on a case where a parallel flat layer of water (with a thickness of 2 mm) was used as a crack and a case where crack faces are contacted (small resin pieces are inserted into the crack). The experiment was conducted by injecting air bubbles (air) into the water saturated crack from its side to gradually expand the air bubble existing region. Seven ceramic piezoelectric elements (one is a vibration source) were arranged on top of a resin block and six elements beneath the block to measure a wave reflected from the crack face and a wave permeated through the crack. It was found that as the air bubble existing region is expanded, the amplitude of the permeated wave decreases remarkably (however, only to a certain level when the crack faces are contacted), and the amplitude of the reflected wave increases. 3 refs., 9 figs.

  3. Time domain electromagnetic method for petroleum exploration. Part 3. Case study in Yoneyama area; Sekiyu tansa ni okeru TDEM ho data shutoku to kaiseki ni tsuite. 3. Niigataken Yoneyama chiiki deno tekiyorei

    Energy Technology Data Exchange (ETDEWEB)

    Ishikawa, H.; Mitsuhata, Y. [Japan National Oil Corp., Tokyo (Japan); Shiga, N. [Mitsui Mineral Development Engineering Co. Ltd., Tokyo (Japan)

    1996-05-01

    The result is reported of a TDEM method-based survey for oil exploration conducted in the Yoneyama district, Niigata Prefecture. The survey covered the southern part of the sedimentary basin in the prefecture, known for the poor quality of the seismic prospecting data that had been recorded. The purpose of the TDEM method-assisted survey was to probe the high-resistivity volcanic rock structure and low-resistivity sedimentary layer, and to know their details. The obtained data were subjected to interpretation by use of the 1D inversion method. A 4000m-deep level was subjected to interpretation, 34 data were inputted, and the early model consisted of 20 layers. As the result, it was found that there was a high-resistivity layer ranging from the ground surface down to a depth of approximately 500m, that a low-resistivity layer 2500-3000m in thickness lay thereunder, and that the lowest layer had a high resistivity of approximately 100 Ohm m. By comparing these data with the geological structure, structures were disclosed corresponding to the rock bed depth, Ukawa syncline, Ishiguro anticline, and Yoneyama mountain mass. 3 refs., 10 figs., 1 tab.

  4. 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.

  5. 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.

  6. 3D seismic survey in Honjo, Akita. Problems and struggles in acquisition and processing; Akitaken Honjo koku ni okeru sanjigen jishin tansa. Genba sagyo to data shori ni okeru mondaiten

    Energy Technology Data Exchange (ETDEWEB)

    Imahori, S.; Kotera, Y.; Nakanishi, T. [Japan Energy Development Co. Ltd., Tokyo (Japan)

    1997-05-27

    Honjo mining area where investigations are conducted is hilly and has a complicated terrain with gas pipes buried in the ground just under the access road disabling the proper positioning of shock-generating large excavators or vibrators. Auger`s shallow hole shooting method is used in this survey to execute blastings at 639 points. In this method using charge depths of 4m, different from the conventional method using deeper charge depths (20-25m), surface waves prevail in the shot records giving rise to a new problem of removing them in the stage of data processing. The 2D filter that is a powerful tool in 2D data processing is not available in a 3D-survey where the tracing intervals are irregular in the shot records. In the effort of this time, a window length as a parameter in the direction of time is specified, and the F-X dip filtering method is employed in which any event that linearly continues beyond a certain number of traces in the said window is eliminated as a linear noise. It is recommended that the weighting function be changed in the direction of space since surface wave velocities are different at different locations. 1 fig., 1 tab.

  7. Confirmation study of the effectiveness of prospect techniques for deep geothermal resources. Deep-seated geothermal resources survey report (Fiscal year 1993); 1993 nendo chinetsu tansa gijutsu nado kensho chosa. Shinbu chinetsu shigen chosa

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    1995-03-01

    Drilling and survey of deep geothermal exploration wells were conducted in order to grasp the existing situation of deep geothermal resource and the whole image of geothermal systems in the area where geothermal resource was already developed. Following fiscal 1992, the well was drilled in fiscal 1993 down to depths of 605m-1505m, and a 13-3/8 inch casing was inserted down to a depth of 1500m. In the drilling, four cores including oriented cores were sampled, and microscopic observation, X-ray diffraction analysis, fluid inclusion survey, core property test, etc. were conducted. In the FMI logging, detected were 273 bedding planes, 483 fractures, etc. Further made were a velocity structure survey, a gravity survey in the area of 270 km{sup 2} including deep exploration wells, a quality survey of the Kakkonda river water, etc. As to geothermal structure models in the Kakkonda area, results of the drilling were added to prediction models before drilling deep exploration wells, but the revision was not very much. Besides, studies were made of a survey method using microearthquakes, a survey technique using resistivity, etc. 61 refs., 259 figs., 95 tabs.

  8. Topics on chemistry and industries. Physico-chemistry/analytical chemistry, inorganics related chemistry, organic chemistry/organics industrial chemistry/polymer chemistry, living organism related chemistry, resources and energy/environment and earth chemistry/chemical engineering; Kagaku to topics. Butsuri kagaku/bunseki kagaku, muki kanren kagaku, yuki kagaku/yuki kogyo kagaku/kobunshi kagaku, seitai kanren kagaku, shigen energy/kankyo chikyu kagaku/kagaku kogyo

    Energy Technology Data Exchange (ETDEWEB)

    Yamaguchi, Y. [The University of Tokyo, Tokyo (Japan); Okumura, A. [Hitachi, Ltd., Tokyo (Japan); Tsukui, H. [Ibaraki Univ., Ibaraki (Japan); Kawamoto, T. [Osaka University, Osaka (Japan); Yamashita, H. [Ehime University, Ehime (Japan); Yuasa, H.; Shimizu, M.; Matsukawa, S. [Tokyo Inst. of Technology, Tokyo (Japan); Okita, M. [Hokkaido University, Sapporo (Japan); Matsuura, N. [Toyama Prefectural University, Toyama (Japan); Sato, N. [Tokyo College of Pharmacy, Tokyo (Japan); Yoneda, Y.; Aoki, Y. [National Inst. for Environmental Studies, Tsukuba (Japan)

    1996-05-01

    This paper takes up and explains recent topics on chemistry and technology. Phase of electron transition in molecules in aqueous solution alleviates very quickly, of which observation technology using femto-second photon echo is introduced in the paper. A description is given on chemical imaging of individual atoms and molecules on surfaces by using a scanning force microscope. Cytochrome C-oxidized enzymes get involved in respiration chain reaction to reduce oxygen molecules into water, whereas structural analyses would move forward studies on mechanisms for proton moving process associated with electron movement. Researches by Milstein et al resulted in success of selective severing of strong carbon-carbon bond by using an Rh-complex. The paper describes the following items: random glycosidation intended of structuring an oligosaccharide library, application of photochromic molecules to next generation photomemory materials, and temperature response and shape memory characteristics of polymer gels having a crystalline structure. The paper takes up in the field of molecular biology the salt resistance donation to plants by using gene engineering, and appearance and diffusion of C{sub 4} plants as seen from carbon isotope ratio. 39 refs.

  9. 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.

  10. Exploration of underground basement structures in Kanto plain using the spatial autocorrelation method. 1. S-wave velocity structure along the line from Hatoyama, Saitama to Noda, Chiba; Kukan jiko sokanho ni yoru Kanto heiya no kiban kozo tansa. 1. Saitamaken Hatoyama machi - Chibaken Nodashi kan no S ha sokudo kozo

    Energy Technology Data Exchange (ETDEWEB)

    Matsuoka, T.; Umezawa, N.; Shiraishi, H. [Saitama Institute of Environmental Pollution, Saitama (Japan)

    1997-05-27

    The Saitama prefectural government has been conducting basement structure exploration using the spatial autocorrelation method by dividing the entire plain area into meshes, for the purpose of improving the accuracy of estimating large-scale seismic damages. This paper reports the result of explorations on meshes in the east-west direction in the central part of Saitama Prefecture. The present exploration was intended on ten meshes in the east-west direction along the north latitude 36-degree line. The number of exploration points is 13 comprising three points on the hilly area bordering on the eastern edge of the Kanto mountainous area and ten points on the plain area. The arrangement constitutes a traverse line with a total distance of about 33 km from the west edge (Hatoyama-machi in Saitama Prefecture) to the east edge (Noda City in Chiba Prefecture). The phase velocities were estimated from the result of the array microtremor observations using the spatial autocorrelation method applied with the FET. The phase velocities were used to estimate underground structures by using an inverse analysis. As a result, detailed two-dimensional S-wave velocity structures were revealed on the traverse line. The velocity cross section expresses change in the basement structures with sufficient resolution, and at the same time the information is judged highly harmonious with existing deep boring data and the result of artificial earthquake exploration. 15 refs., 6 figs.

  11. Fiscal 1997 report on the verification research on geothermal prospecting technology. Theme 3. Development of a reservoir variation prospecting method (development of electric/electromagnetic prospecting methods); 1997 nendo chinetsu tansa gijutsu nado kensho chosa. 3. Choryuso hendo tansaho kaihatsu (denki denjiki tansaho kaihatsu) hokokusho

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    1998-03-01

    To evaluate geothermal reservoirs in the initial stage of development and keep stable output in service operation, measurement of self-potential and resistivity changes due to production and reinjection of geothermal fluid has been made. This paper describes the result in fiscal 1997. To study the placing method and stability of electrodes for continuous self-potential monitoring network in fiscal 1998, continuous monitoring of potential differences started in an experimental field. The placing condition and electrode will be selected by July. By surveying self-potentials after the beginning of operation of Oogiri geothermal power plant, a distribution range of negative and positive potential anomalies was clarified. To predict the resistivity change, long-term change in salinity concentration in a reservoir was estimated by a hydrothermal flow concept model. The resistivity change caused by reservoir variation due to plant operation was also predicted to study its detection by MT method on the ground. The salinity concentration change due to reinjection, and resistivity change due to a two-phase region in the top of a reservoir were considered. 17 refs., 56 figs., 19 tabs.

  12. Fiscal 1997 basic research on coal resource development (equipment development). Report on R and D of new exploration technology (exploration of medium-depth coal deposits in water areas); 1997 nendo sekitan shigen kaihatsu kiso chosa (kiki kaihatsu hen) hokokusho. Shintansa gijutsu chosa kaihatsu (suiiki chushindoso tansa)

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    1999-03-01

    This report summarizes the research result on development of new coal exploration technology. For a high-precision and high-resolution reflective seismic exploration system, R and D was made on the exploration technology of several meter in resolution for medium-depth (800m) coal deposits under a lake of 2m deep. As a result, the high-frequency and high-power source (150-200Hz in dominant frequency, 700-800m in penetrability) and the high-frequency and high sensitivity receiver (10-1000Hz in frequency band, 35V/PA in sensitivity) were developed successfully, and the positioning system was improved. The final evaluation of these elementary technologies was carried out through demonstration tests, resulting in satisfactory results. For a high-efficiency trial drilling system, the in-bore trouble prevention system for measurement, processing and analysis of drilling data (drilling length, drilling rate, revolution, bit load, torque) and drilling mud data (charge water pressure, charge/discharge water, density, pH, viscosity) was constructed. The outlook for low-cost measurement and a safety during drilling was thus obtained. (NEDO)

  13. Fiscal 1997 report on the verification survey of geothermal exploration technology. 5-1. Development of the reservoir variation survey method (technology of prediction of reservoir variation); 1997 nendo chinetsu tansa gijutsu nado kensho chosa. Choryuso hendo tansaho kaihatsu (choryuso hendo yosoku gijutsu) hokokusho

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    1998-03-01

    For the reservoir evaluation at an initial developmental stage and stabilization/maintenance of power after the start of operation, the fiscal 1997 result was described of the study of technology of prediction of reservoir variation. Using the conventional post processor, feasibilities were computed of reservoir models and behavior after the development, and gravity/self potential/resistivity variation. Variation in the seismic wave speed structure was large in travel time change distribution. The measuring accuracy of 1m sec is required to get enough detection resolving power. A conceptual design of the post processor development was conducted to study a system operated on Windows. Based on the reservoir numerical simulation technology, by taking in variation parameters such as gravity and self potentials as new model constraint conditions, the reservoir modeling technology which increased in accuracy by history matching was trially developed. Using the conventional reservoir model in the Oguni area, predictably computed were reservoir behaviors during 50 years which simulated a 20 MW development. Effectiveness of the post processor were able to be shown though influenced by characteristics such as permeability and resistivity. 74 refs., 95 refs., 12 tabs.

  14. Field experiment in jointed rock mass with electro-magnetic tomography. Challenge for 50m energy penetration and an interpretation with additional geological data; Denjiha tomography ni yoru setsurisei ganban no tansa. Kokan kyori 50m no sokutei to chishitsu kaishaku no kokoromi

    Energy Technology Data Exchange (ETDEWEB)

    Suzuki, K.; Koga, K.; Nishiyama, E.; Yamamoto, T. [Kawasaki Geological Engineering, Co. Ltd., Tokyo (Japan)

    1996-05-01

    With the purpose of extending an exploring distance in electromagnetic tomography, a prototype was made as a device to receive and transmit continuous waves in a borehole, so that a tomographic observation was carried out on a jointed rock mass that had a conventionally short exploring distance. The device consisted of a transmitter, receiver, antenna, cable and surface controller, with a personal computer used for displaying and storing data. The prototype antenna was provided with a size insertable into a VP50 vinyl chloride tube. In order to determine a relative permittivity of a rock, a boring core was shaped and an impedance was measured. The measurement of tomography was carried out at 1m spaces apart in the bore holes with a distance of 50m in between. The received waveforms were stored in a floppy disk built in the personal computer. As a result of the analysis, a tomographic cross-section of the electromagnetic wave velocity was obtained, showing the distribution of sandstone with a high electromagnetic wave velocity and little joints, shale with a low electromagnetic wave velocity, chart with a high electromagnetic wave velocity, etc. 2 refs., 4 figs., 1 tab.

  15. Fiscal 1997 report of the verification research on geothermal prospecting technology. Theme 5-2. Development of a reservoir change prospecting method (reservoir change prediction technique (modeling support technique)); 1997 nendo chinetsu tansa gijutsu nado kensho chosa. 5-2. Choryuso hendo tansaho kaihatsu (choryuso hendo yosoku gijutsu (modeling shien gijutsu)) hokokusho

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    1998-03-01

    To evaluate geothermal reservoirs in the initial stage of development, to keep stable output in service operation, and to develop a technology effective for extraction from peripheral reservoirs, study was made on a reservoir variation prediction technique, in particular, a modeling support technique. This paper describes the result in fiscal 1997. Underground temperature estimation technique using homogenization temperatures of fluid inclusions among core fault system measurement systems was applied to Wasabizawa field. The effect of stretching is important to estimate reservoir temperatures, and use of a minimum homogenization temperature of fluid inclusions in quartz was suitable. Even in the case of no quartz in hydrothermal veins, measured data of quartz (secondary fluid inclusion) in parent rocks adjacent to hydrothermal veins well agreed with measured temperature data. The developmental possibility of a new modeling support technique was confirmed enough through collection of documents and information. Based on the result, measurement equipment suitable for R and D was selected, and a measurement system was established through preliminary experiments. 39 refs., 35 figs., 6 tabs.

  16. Fiscal 1997 report on the verification research on geothermal prospecting technology. Theme 4. Development of a reservoir variation prospecting method (development of a micro-earthquake monitoring system (MEMS)); 1997 nendo chinetsu tansa gijutsu nado kensho chosa. 4. Choryuso hendo tansaho kaihatsu (jishinha tansaho kaihatsu) hokokusho

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    1998-03-01

    To evaluate geothermal reservoirs in the initial stage of development and keep stable output in service operation, the application of MEMS is under development. This paper describes the result in fiscal 1997. Installation of 3-component velocity type seismometers in bore holes is desirable for permanent monitoring sites. Their arrangement should be determined by detection ability simulation. Their locations at various elevations are effective to improve the accuracy of hypocenter determination. Digital seismic data at the permanent sites are transmitted to a center through cables, while temporary data are recorded on site. For poor MEPAS, a Windows program of basic functions was developed. 3-D seismic velocity analysis and array monitoring system were also studied. A P-wave velocity of rocks decreased by 25% by formed two-phase region, and increased by 10% by decrease in reservoir temperature from 200 to 100degC. The velocity can be detected by change in travel time of direct waves due to considerable variation in reservoir environment. VSP technique using a vibrator or air gun as artificial hypocenter is effective for MEMS. 67 refs., 64 figs., 19 tabs.

  17. Pure Land or Pure Mind?: Locus of Awakening and American Popular Religious Culture

    Directory of Open Access Journals (Sweden)

    Richard K. Payne

    2015-03-01

    Full Text Available This essay has two sections, each with its own distinct goal, forming an interrelated whole. The first introduces “locus of awakening,” and applies it to the relative success in America of Zen and Tibetan Buddhisms, compared to Pure Land Buddhism. The explanatory power of the concept is demonstrated by also considering Soka Gakkai. The difference between popular culture treatments of Zen and Tibetan Buddhisms, and Pure Land Buddhism was the problematic leading to identifying locus of awakening as an aspect of Buddhist thought. The second section locates it in the history of Buddhist thought, demonstrating that it is not a modern conceptualization of the path, not one created in response to Euro–American religio-therapeutic culture. Locus of awakening is, instead, part of the continuity of the Buddhist tradition, and does not fall on one side or the other of the sometimes overdrawn dichotomy between Asian and American Buddhisms.

  18. Cultivating Charisma: Ikeda Daisaku's Self Presentations and Transformational Leadership

    Directory of Open Access Journals (Sweden)

    Clark Chilson

    2015-02-01

    Full Text Available Although social scientific studies of leadership have progressed significantly since the 1960s, discussions of popular religious leaders remain grounded in Weberian ideas on "charisma." Because "charisma" in Weber's writings lacks conceptual clarity and analytical precision, it fails to illuminate how specific understandings of popular leaders develop or how leaders create affective ties with followers. Weber's discussions of charisma, however, can still lead to important questions. Using a Weberian statement on charisma as a departure point, this article argues on the basis of the published diary of Ikeda Daisaku, leader of the Nichiren Buddhist organization Soka Gakkai, that self-representations by a leader can influence how followers understand him or her in a way that cultivates charisma. More specifically it argues that by depicting the mentor-disciple relationship as empowering, Ikeda's diary can serve as a method for transformational leadership that fosters a sense of intimacy and nurtures affective ties with him.

  19. Mitochondrial DNA analysis of Sporothrix schenckii in India, Thailand, Brazil, Colombia, Guatemala and Mexico.

    Science.gov (United States)

    Ishizaki, Hiroshi; Kawasaki, Masako; Anzawa, Kazushi; Mochizuki, Takashi; Chakrabarti, Arunaloke; Ungpakorn, Rataporn; Torres Guererro, Haydee; Toriello, Conchita; Arenas, Robert

    2009-01-01

    Up to now, 30 mitochondrial DNA(mtDNA)and 4 rDNA types of Sporothrix schenckii strains have been identified. Here, seventy-six isolates of S. schenckii from Mexico, Guatemala, Brazil, Thailand and India were genotyped and studied epidemiologically by mtDNA restriction fragment length polymorphisms(RFLP)and internal transcribed spacer region(ITS)-RFLP analysis and two new mtDNA types, Type 31 and Type 32, were found. Type 30, previously reported by Mora-Cabrera et al. was confirmed to be Type 3 and designated as blank. Of 48 isolates from Mexico, 41 belonged to Group A wherein Type 2(13 isolates), Type 3(10)and Type 28(7)were dominant. All ten isolates from India and Thailand belonged to Group B. The 52 Group A and 24 Group B isolates corresponded to rDNA Type I and Type IV , respectively, reported by Watanabe et al.(Nippon Ishinkin Gakkai Zasshi 45: 165-175, 2004).

  20. Exhibition: Linus Pauling and the Twentieth Century

    CERN Document Server

    2003-01-01

    On April 28 the exhibit Linus Pauling and the Twentieth Century organised by UNIDIR (United Nations Institute for Disarmament Research) and SGI (Soka Gakkai International) as well as with the contributions of CERN and the University of Geneva, opened at the United Nations Office of Geneva. Linus Pauling is the only person to date to have won two unshared Nobel Prizes: Chemistry in 1954 and Peace in 1962. The first was awarded for his landmark research on the nature of the chemical bond and its application in understanding the structure of complex substances. The second one acknowledged his courageous protest against atmospheric nuclear testing and his championship of international peace. The exhibit, for audience of all ages, traces seven decades of Linus Pauling's life and influence on the 20th century. Before starting its European tour at the UNESCO headquarters in Paris, the exhibit opened in 1998 in San Francisco and then travelled within the United-States and to Japan with an attendance of more than one...

  1. Exhibition: Linus Pauling and the Twentieth Century

    CERN Multimedia

    2003-01-01

    On April 28 the exhibit Linus Pauling and the Twentieth Century organised by UNIDIR (United Nations Institute for Disarmament Research) and SGI (Soka Gakkai International) as well as with the contributions of CERN and the University of Geneva, opens at the United Nations Office of Geneva. Linus Pauling is the only person to date to have won two unshared Nobel Prizes: Chemistry in 1954 and Peace in 1962. The first was awarded for his landmark research on the nature of the chemical bond and its application in understanding the structure of complex substances. The second one acknowledged his courageous protest against atmospheric nuclear testing and his championship of international peace. The exhibit, for all ages' audiences, traces seven decades of Linus Pauling's life and influence on the 20th century. Before starting its European tour at the UNESCO headquarters in Paris, the exhibit opened in 1998 in San Francisco and then travelled within the United-States and to Japan with an attendance of more than one m...

  2. Spatiotemporal analysis of the effects of forest covers on water yield in the Western Ghats of peninsular India

    Science.gov (United States)

    Singh, Sunita; Mishra, Arabinda

    2012-06-01

    , the Tansa having over 52% forest cover of primary and mature secondary forests and nearly 60-70% of forest cover of Bhatsa and Upper Vaitarna being disturbed forests, the impact of forest cover on runoff coefficient did not vary significantly from one watershed to the other. However, when the forest cover was segregated into old forests (primary forest, mature secondary forest and undisturbed mature plantations) and mixed forests (disturbed forests and to lesser extent naturally occurring open forest (Open Forests: All lands with tree cover of canopy density between 10% and 40%)), the old forests were observed to positively and highly significantly (p forests exhibited negative trend that was not statistically significant. The change in water yield in relation to the changes in forest cover is quantified for three watersheds that face moderate to heavy biotic pressure.

  3. {sup 18}F-FDG PET for exploration of para-neoplastic syndromes with anti-h.u. antibodies and small cell lung cancer: clinical case and literature review

    Energy Technology Data Exchange (ETDEWEB)

    Ricard, F.; Giammarile, F.; Houzard, C. [Centre Hospitalier Lyon, Dept. of Nuclear Medicine, 69 - Pierre Benite (France); Giammarile, F.; Houzard, C. [Lyon-1 Univ., EA 3738, 69 (France); Didelot, A.; Mauguiere, F. [Hopital Neurologique, U 301, 69 - Bron (France)

    2008-02-15

    Introduction. - Small cell lung cancer (S.C.L.C.) is a neuroendocrine tumour representing 20% of bronchopulmonary cancers. Its metastatic potential is high, so 2/3 of diagnoses are made at disseminated stage. Anti H.u. antibodies are part of the anti neuronal antibodies, often associated to S.C.L.C.. However, 16% of cancers have positive anti H.u. with no para neoplastic syndrome (P.N.S.). (Graus, Brain, 2001). P.N.S. associated with anti H.u. are encephalomyelitis, sensitive neuropathy, chronic pseudo intestinal obstruction, cerebellar degeneration and limbic encephalitis. Case report. - A 75-year-old patient was hospitalized for exploration of an atypical tri-facial neuralgia. Anti H.u. antibodies were found and P.N.S. of a S.C.L.C. was therefore suspected. The biopsy of a thoracic parietal adenopathy confirmed the diagnostic of S.C.L.C. metastasis. Conventional imaging and {sup 18}F-FDG (Fluorodeoxyglucose) PET/CT (Positron Emission Tomography/Computed Tomography)) did not localize the primary tumour, despite advanced dissemination stage, only showing lymphatic secondary locations at the left axillary and under the diaphragm areas. Literature review. - Younes-Mhenni (Brain, 2004, 20 patients); and Linke (Neurology, 2004, 13 patients) studied patients presenting with anti H.u. antibodies (13 and eight respectively) and other anti neuronal antibodies (Y.o., Ri, C.V.2, Tr) associated with different cancers. PET sensitivity was respectively 83.3 and 90% with a specificity of 25 and 67%. In both series, specificity of anti H.u. antibodies for S.C.L.C. was estimated at 53% and 62.5%. Size is a limiting factor for S.C.L.C. detection and Watanabe (Nihon Kokyuki Gakkai Zasshi, 2001) showed that sensitivity for detection of less than 1 cm tumour was 0% in five patients. Moreover, P.N.S. can precess S.C.L.C. detection for many years and PET/CT has to be repeated. (Gaillard, Revue neurologique, 2005).In two other studies (Schumacher, EJNM, 2001, 30 patients; and Niho, Lung