Description Usage Arguments Details Assumptions Author(s) See Also
Skempton related changes in applied stress to changes in fluid pressure; this is the famous constant B.
1 |
Beta |
numeric; compressibility β |
Phi |
numeric; Φ |
Beta_u |
numeric; β[u] solid matrix - undrained |
Beta_f |
numeric; β[f] fluid |
Calculates Equation (4) from Rojstaczer and Agnew (1989)
As noted by Rice and Cleary [1976], this definition for B assumes that the rock matrix is homogeneous and all the pore space is interconnected.
Andrew J. Barbour <andy.barbour@gmail.com>
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