STOCHASTIC MODELING OF VARIABLY SATURATED TRANSIENT FLOW IN FRACTAL POROUS MEDIA

dc.contributor.authorGuarracino L.
dc.contributor.authorSantos Ju.E.
dc.date.accessioned2022-09-21T01:18:35Z
dc.date.available2022-09-21T01:18:35Z
dc.date.issued2004
dc.description.abstractThis work presents the application of a Monte Carlo simulation method to perform an statistical analysis of transient variably saturated flow in an hypothetical random porous media. For each realization of the stochastic soil parameters entering as coefficients in Richards' flow equation, the pressure head and the flow field are computed using a mixed finite element procedure for the spatial discretization combined with a backward Euler and a modified Picard iteration in time. The hybridization of the mixed method provides a novel way for evaluating hydraulic conductivity on interelement boundaries. The proposed methodology can handle both large variability and fractal structure in the hydraulic parameters. The saturated conductivity Ks and the shape parameter αvg in the van Genuchten model are treated as stochastic fractal functions known as fractional Brownian motion (fBm) or fractional Gaussian noise (fGn). The statistical moments of the pressure head, water content, and flow components are obtained by averaging realizations of the fractal parameters in Monte Carlo fashion. A numerical example showing the application of the proposed methodology to characterize groundwater flow in highly heterogeneous soils is presented.
dc.identifierhttps://elibrary.ru/item.asp?id=5999067
dc.identifier.citationMathematical Geology, 2004, 36, 2, 217-238
dc.identifier.issn0882-8121
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/38676
dc.subjectUNSTEADY UNSATURATED FLOW
dc.subjectFINITE ELEMENTS
dc.subjectHETEROGENEOUS SOILS
dc.titleSTOCHASTIC MODELING OF VARIABLY SATURATED TRANSIENT FLOW IN FRACTAL POROUS MEDIA
dc.typeСтатья

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