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- Author
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TSUTSUMI, Daizo, FUJITA, Masaharu, SIDLE, Roy C., HAYASHI, Yujirou, 40372552, 60181369, TSUTSUMI, Daizo, FUJITA, Masaharu, SIDLE, Roy C., HAYASHI, Yujirou, 40372552, and 60181369
- Abstract
Numerical experiments were conducted to assess the effect of preferential flow through pipes and cracks within weathered bedrock on slope stability, using hydrological model in which water flows within both the matrix and macropores. The hillslope consists of soil and weathered bedrock layers. Hydraulic properties were assigned to the weathered bedrock as well as the soil layer, and the regolith flow calculations were conducted within the slopes. Results demonstrated that the preferential flow pathway rapidly transported rainwater to the deeper layer of the slope, and if the outlets of the preferential flow pathway remained within the slope, the pressure head increased around these points. This increase in pressure head caused a decrease in the factor of safety at the deeper layer of the slope.
- Published
- 2005