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Geological hazards

NASGLP for predicting areas of potential natural geologic hazards. [Pg.175]

Howe, S.J., Nanchary, N.R., Patil, S.L., Ogbe, D.O., Chukwu, GA., Hunter, R.B., Wilson, S.J., in Proc. Hedburg Conference on Gas Hydrates Energy Resource Potential and Associated Geologic Hazards, Vancouver, BC, September 12-16 (2004). [Pg.634]

Duan Y. 1998. Research status on land subsidence and sustainable development in the 21 century of China. Chinese J. of Geological Hazard and Control, 9(2), pp. 1-5. [Pg.45]

Ran Q and Gu X. 1998b. A coupled model for land subsidence computation with consideration of rheological property. Chinese J. of Geological Hazards and Prevention, 9(2), pp. 99-103. [Pg.46]

Wu Y. 1996. The coupled stress-ground water flow-model for jointed rock mass. J. of Geological Hazards Environmental... [Pg.47]

Zhan Z, Wen J, Wu G and Liao Y. 1998. Research on constitutive model of wet swellling rock and soil masses. J. of Geological Hazards Environmental Preservation, 9(2), pp. 49-54. [Pg.47]

Natural gas hydrates in sediments are widely distributed in offshore continental margins and in polar regions. The amount of methane contained in gas hydrates is currently estimated to be between 10 and 10 m (Kvenvolden, 2000), considered an important natural resource in the future. Natural gas hydrates are also believed to be a factor in global climate changes (Haq, 2000) and submarine geologic hazards (Paull et al, 2000b). [Pg.377]

Sand inrush or water sand is a kind of properties and casualties mine geology hazard when excavating nearly at unconsolidated layers sand content of high water sand mixed fluid in the mining face... [Pg.795]

The physical defects have existed widely in the natural rock, such as fracture, joint and fault and other discontinuous structural plane. The physical and mechanical characteristics of the rock have been influenced seriously by the structural plane, and also the seepage and thermodynamic features and other characteristics have been determined mostly according to the structural plane. It involves mine excavation, environment protection, water conservancy construction, radioactive waste disposal and reservoir induced geologic hazard etc. [Pg.927]

Zhang Dongming Liu Jianzhong. 2003. Regularity on the distribution of gas moving in gob area of cod mine. The Chinese Journal of Geological Hazard and Control, 14(l) 81-84. [Pg.1086]

Wang GC, et al. 2000. Hydro-geochemical exploratory method in mine groundwater hazard control (in Chinese). The Chinese Journal of Geological Hazard and Contra/ll(l) 33-37. [Pg.1285]

Regional and local geology (hazards, rock type and stmcture, soil types, and ground water characteristics)... [Pg.20]

Description of subsurface conditions, including any information on groundwater, from study of geological maps and memoirs, previous site investigation reports and any features or outcrops observed during site walkover. Identification of possible geological hazards, e.g. buried channels in alluvium, solution holes in chalk and limestone, swelling/shrinkable clays... [Pg.314]

Geological hazards vary in their nature and can be complex. One type of hazard, for example, an earthquake, can be responsible for the generation of others such as liquefaction of sandy or silty soils, landslides or tsunamis. Certain hazards such as earthquakes and landslides are rapid onset hazards and so give rise to sudden impacts. Others such as soil erosion and subsidence due to the abstraction of groundwater may take place gradually over an appreciable period of time. Furthermore, the effects of natural geohazards may be difficult to separate from those attributable to human influence. In fact, modification of nature by humans often increases the frequency and severity of natural geohazards, and, at the same time, these increase the threats to human occupancy. [Pg.380]

Bell, F.G. 1999. Geological Hazards Their Assessment, Avoidance and Mitigation. Spon Press, London. Beven, K. and Carling, F. (Eds.). 1989. Floods Hydrological, Sedimentological and Geomorphological Implications. Wiley, Chichester. [Pg.552]

Bolt, B.A., Horn, W.L., McDonald, G.A. and Scott, R.F. 1975. Geological Hazards. Springer-Verlag, New York. [Pg.552]

Griggs, G.B. and Gilchrist, J.A. 1983. Geologic Hazards, Resources and Environmental Planning. Wadsworth, Belmont, California. [Pg.556]

Soule, J.M. 1980. Engineering geologic mapping and potential geologic hazards in Colorado. Bulletin International Association of Engineering Geology, 21,121-131. [Pg.572]

Yin, YP. 2003. Seepage pressure effect on landslide stability at the Three Gorges Reservoir area. The Chinese J. of Geological Hazard Control, 14(3) l-8. (in Chinese)... [Pg.65]

Han L.F. 2010. Research on the development regular and triggering mechanism of geological hazards in... [Pg.78]

The risk indexes of debris flow are evaluated by geological hazard analysis assessment method. The risk indexes of Zhiyang valley are analyzed and the risk analysis structure model of debris flow is established. [Pg.126]

Zliang Liang, Zhang Yecheng. 1998. Theory and practice of Geological hazard assessment. Beijing Geology Press. [Pg.128]


See other pages where Geological hazards is mentioned: [Pg.537]    [Pg.634]    [Pg.42]    [Pg.121]    [Pg.71]    [Pg.21]    [Pg.13]    [Pg.35]    [Pg.35]    [Pg.42]    [Pg.296]    [Pg.295]    [Pg.376]    [Pg.380]    [Pg.380]    [Pg.381]    [Pg.383]    [Pg.383]    [Pg.59]    [Pg.97]    [Pg.100]    [Pg.104]    [Pg.128]   
See also in sourсe #XX -- [ Pg.295 ]




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