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Keywords: intensity
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Proceedings Papers

Paper presented at the ISRM International Symposium, November 19–24, 2000
Paper Number: ISRM-IS-2000-443
...NUMERICAL MODELING OF LANDSLIDE IN INTENSIVE SEISMIC ZONE Tao Lianjin1 , Zhang Zhuoyuan2, Liu Hanchao2, Chai Hejun2, Deng Ronggui3 ABSTRACT Landslide in intensive seismic zone has its peculiar features. Some slope may be stable under static load (normal state). When the slope is in limit...
Proceedings Papers

Paper presented at the ISRM International Symposium, November 19–24, 2000
Paper Number: ISRM-IS-2000-478
... the quantitative evaluations of the effects of vegetation on a face of slope. As the results of the experiments, we could obtain the quantitative relationship between a intensity of rainfall and a ratio of partial interception loss by vegetation, and also the evaporation and evapo-transpiration ratios...
Proceedings Papers

Paper presented at the ISRM International Symposium, November 19–24, 2000
Paper Number: ISRM-IS-2000-519
... is not appropriate because among the field experts (consultant and decision makers) the term "hazard" is instinctively connected to the real danger, which is related not only to the occurrence probability of a landslide phenomenon, but also to its intensity. It is therefore considered more correct...
Proceedings Papers

Paper presented at the ISRM International Symposium, November 19–24, 2000
Paper Number: ISRM-IS-2000-492
... period for which antecedent rainfall affects the groundwater level at any given time. It is not considered that the vertical scales should necessarily be similar. One might expect the moving-average rainfall curve to have a greater vertical exaggeration than the groundwater, as increasing intensity...
Proceedings Papers

Paper presented at the ISRM International Symposium, November 19–24, 2000
Paper Number: ISRM-IS-2000-033
.... (Photo by J. Hango) 8 ". soe ft . 10"n 150eft 2500 ft ~. '. SALT 0 2kJD. "younger fault set, N2 Figure 11. Cross Section of the Reitbroo~Salt Dome, Genn·any, Showing Intense Network of Nonnaland Reverse Faults in the Overlying Sediments. (from De Sitter, 1956) Figure 12. Block Diagramlliustratingthe...
Proceedings Papers

Paper presented at the ISRM International Symposium, September 10–12, 1990
Paper Number: ISRM-IS-1990-033
.... Seismic data recorded from this area supports the observations that some pillars failed violently. Investigations undertaken suggest that the presence and intensity of jointing is one of the controlling factors influencing pi lIar behaviour. 1 INTRODUCTION Impala workings are supported with a pillar...
Proceedings Papers

Paper presented at the ISRM International Symposium, September 12–16, 1988
Paper Number: ISRM-IS-1988-005
...Rock Mechanics and Power Plants, Romana (ed.) @ 1988Ba/kema, Rotterdam./SBN9061918278 About the joint set intensity Nuno Feodor Grossmann Laboratorio Nacional de Engenharia Civil, Lisboa, Portugal ABSTRACT: The intensity of a joint set quantifies the amount of rock mass fracturing due to that set...
Proceedings Papers

Paper presented at the ISRM International Symposium, August 31–September 3, 1986
Paper Number: ISRM-IS-1986-035
... stability condition. Several examples have made it possible to assess the influence of various parameters (Young''s modulus, surface energy and porosity) on the intensity of the microcraking. Finally, experimental results make it possible to confirm the model and establish a regional state of stress in the...
Proceedings Papers

Paper presented at the ISRM International Symposium, August 31–September 3, 1986
Paper Number: ISRM-IS-1986-052
... fracturing orientation relaxation reservoir simulation stationary stress level stress relaxation behaviour Reservoir Characterization prestressed hard inclusion borehole rock mass stress relaxation salt rock hydraulic pressure cell strain rate pressure cell Mortar intensity cylindrical steel...
Proceedings Papers

Paper presented at the ISRM International Symposium, August 31–September 3, 1986
Paper Number: ISRM-IS-1986-066
..., exhibit severe spalling in roof and floor. Mapping of exfoliation show that intensity of exfoliation is depending on stress level, orientation and stress anisotropy. Resume: La distribution regionale des tensions a été établie pour la région précambrienne de la culmination de Tysfjord dans le nord de...

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