Computational Geomechanics. Manuel Pastor
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Equation (3.13) is scalar.
Equation (3.14) is scalar.
(3.15b)
Equation (3.16) is scalar
(3.17b)
and
(3.18b)
and assuming isotropic permeability
(3.19b)
The summation range for the upper‐case indices will depend on the number of nodes with solid displacement and pore water pressure degrees‐of‐freedom (dofs), respectively.
Applying Green’s identity to the internal force term (first term on the left‐hand side)
Rearranging
(3.20)
The definition of the B matrix in Equation (3.21) is not needed in tensorial form.
(3.23b)
(3.24b)
(3.25b)
(3.26b)