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On an estimation of the hydraulic conductivity in a three-dimensional anisotropic confined aquifer. (Russian. English summary) Zbl 1087.76560
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.
MSC:
76S05 Flows in porous media; filtration; seepage
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