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A geostatistically based inverse model for three-dimensional variably saturated flow - MaRDI portal

A geostatistically based inverse model for three-dimensional variably saturated flow

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Publication:1291915

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DOI10.1007/S004770050022zbMath0940.76074OpenAlexW2135803164MaRDI QIDQ1291915

T.-C. Jim Yeh, D. L. Hughson

Publication date: 24 July 2000

Published in: Stochastic Hydrology and Hydraulics (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1007/s004770050022

zbMATH Keywords

heterogeneity moisture content adjoint state sensitivity method cokriging estimator geostatistically based inverse model perturbations in hydraulic parameters pore size distribution parameter pressure content unsaturated hydraulic conductivity

Mathematics Subject Classification ID

Hydrology, hydrography, oceanography (86A05) Flows in porous media; filtration; seepage (76S05) Stochastic analysis applied to problems in fluid mechanics (76M35)

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