Biot Critical Frequency Applied as Common Friction Factor for Pore Collapse and Failure of Chalk With Different Pore Fluids and Temperatures
Keyword(s):
Summary A fluid effect toward higher strengths for oil-saturated chalk compared with water-saturated chalk has previously been identified and labeled the "water-weakening phenomenon," but has not been further characterized physically. The hypothesis of this paper is that the Biot critical frequency with a strain or stress-rate dependence can be used to explain this behavior on the pore scale and can be extrapolated to the macroscale failure and pore-collapse properties. A large set of previously published laboratory test results on chalk with different pore fluids was collected, and as a supplement we present a new test series on Stevns chalk with unconfined compression and Brazilian strength results.
1983 ◽
Vol 40
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pp. 1025-1034
1978 ◽
Vol 69
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pp. 32-35
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pp. 307-316
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1969 ◽
Vol 52
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pp. 666-670
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1977 ◽
pp. 287-317
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