Pore fluid frictional heating and stability of creeping landslides
Source abstract
Abstract
Abstract An examination of the effects of frictional heating of pore fluid in relation to long‐term slope stability is presented. It is found that increases in pore‐fluid pressure due to heat‐induced expansion may act to enhance creep rates and possibly lead to total loss of stability. Conditions for total stability loss are examined and an approximate critical value of average shear stress is determined. This value must be exceeded for a sufficiently long period of time in order to induce rapid failure.
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Research context
OpenAlex topics: Landslides and related hazards · Rock Mechanics and Modeling · Geotechnical Engineering and Analysis
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References (11)
Show source-provided references
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