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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