On an estimation of the hydraulic conductivity in a three-dimensional anisotropic confined aquifer. (Russian. English summary) Zbl 1087.76560

Gabidullina, A. N.; Elesin, A. V.; Kadyirova, A. Sh.; Mazurov, P. A.

Mat. Model. 14, No. 9, 97-102 (2002).

One of the standard procedures of identification of hydrogeological parameters is the method of inverse coefficients. Inverse problems of such a type are related to the so-called incorrect problems. A regularizing algorithm stable to errors in the initial data is usually a basic method of solving incorrect problems. A regularization property of minimization algorithms is studied here in case of lacking information of the observation networks for hydrogeological parameter identification.

Reviewer: Sergei Georgievich Zhuravlev (Moskva)

MSC:

76S05

Flows in porous media; filtration; seepage

Keywords:

flows in porous media; filtration; identification of hydrogeological parameters