Engineering geological advances in Japan for the new millennium
著者
書誌事項
Engineering geological advances in Japan for the new millennium
(Developments in geotechnical engineering, 84)
Elsevier Science B.V., 2000
大学図書館所蔵 全10件
  青森
  岩手
  宮城
  秋田
  山形
  福島
  茨城
  栃木
  群馬
  埼玉
  千葉
  東京
  神奈川
  新潟
  富山
  石川
  福井
  山梨
  長野
  岐阜
  静岡
  愛知
  三重
  滋賀
  京都
  大阪
  兵庫
  奈良
  和歌山
  鳥取
  島根
  岡山
  広島
  山口
  徳島
  香川
  愛媛
  高知
  福岡
  佐賀
  長崎
  熊本
  大分
  宮崎
  鹿児島
  沖縄
  韓国
  中国
  タイ
  イギリス
  ドイツ
  スイス
  フランス
  ベルギー
  オランダ
  スウェーデン
  ノルウェー
  アメリカ
注記
Includes bibliographical references
内容説明・目次
内容説明
The geology of the Japanese Islands is enormously complicated because of the active tectonism that has taken place on the boundary between the Pacific and Eurasian plates. Geological formations there are intricately deformed and displaced by many active faults. Hence, in planning for and siting large construction projects, such as nuclear power stations, underground power stations, and the underground facility for High-Level Radioactive Waste (HLW), more detailed investigations are necessary than in more stable parts of the world. Only then can assessments be made as to the long-term stability, hydrological characteristics and mechanical characteristics of geological conditions. This book offers research studies in engineering geology in Japan. It contains 27 papers, which should be of scope and importance sufficient to allow engineering geologists throughout the world to understand more of the present state of research and study in Japan.
The title also includes a number of current topics in which Japanese engineering geologists have participated: the planning for and siting of large construction, such as nuclear power stations, underground power stations, and the underground facility for High-Level Radioactive Waste (HLW); the construction project of highways and nuclear power stations and new energy developments such as those for geothermal energy; the countermeasures for natural hazards caused by earthquakes, landslides, and slope, and stone deterioration; and alteration because of weathering at and near the Earth's surface.
目次
- New Technology and its Application: Three-dimensional miarolitic cavity distribution in the Kakkonda granite from borehole WD-1a using X-ray computerized tomography
- The use of X-ray CT to measure the diffusion coefficients of heavy ions in water-saturated porous media
- Detection of hydraulic pathways in fractured rock masses and estimation of conductivity by a newly developed TV equipped flowmeter
- Case studies of electrical and electromagnetic methods applied to mapping active faults beneath the thick Quaternary
- A new technique for rapid and non-destructive measurement of rock-surface moisture content
- preliminary application to weathering studies of sandstone blocks
- In-situ Experiments
- Stress estimated by using microseismic clusters and its relationship to the fracture system of Hijiori hot dry rock reservoir
- Strain monitoring of borehole diameter changes in heterogeneous jointed wall rock with chamber excavation, estimation of stress redistribution. Non-sorbing tracer migration experiments in fractured rock at the Kamaishi mine, Northeast Japan
- In-situ experiments on an excavation disturbed zone induced by mechanical excavation in Neogene sedimentary rock at Tono mine, central Japan. Site Characterization: Seismic risk assessment of an active fault system - the example of the Tsurugawan-Isewan tectonic line
- Geotechnical evaluation of conglomerate for compressed air energy storage - the influence of the sedimentary cycle and filling minerals in the rock matrix
- Time-dependent ground motion amplification characteristics at reclaimed land after the 1995 Hyogoken Nambu Earthquake
- Overview of the stability and barrier functions of the granitic geosphere at the Kamaishi mine - relevance to radioactive waste disposal in Japan
- Rates of weathering and temporal changes in strength of bedrock of marine terraces in Boso Peninsula, Japan
- Weathering distribution in a steep slope of soft pyroclastic rocks as an indicator of slope instability. (Part contents).
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