R. Mustata et al., An inverse boundary element method for determining the hydraulic conductivity in anisotropic rocks, CMES-COMP M, 1(3), 2000, pp. 107-116
An inverse boundary element method is developed to characterise the compone
nts of the hydraulic conductivity tensor K of anisotropic materials. Surfac
e measurements at exposed boundaries serve as additional input to a Genetic
Algorithm (GA) using a modified least squares functional that minimises th
e difference between observed and BEM-predicted boundary pressure and/or hy
draulic flux measurements under current hydraulic conductivity tensor compo
nent estimates.