STOCHASTIC MODELING OF VARIABLY SATURATED TRANSIENT FLOW IN FRACTAL POROUS MEDIA

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dc.contributor.author Guarracino L.
dc.contributor.author Santos Ju.E.
dc.date.accessioned 2022-09-21T01:18:35Z
dc.date.available 2022-09-21T01:18:35Z
dc.date.issued 2004
dc.identifier https://elibrary.ru/item.asp?id=5999067
dc.identifier.citation Mathematical Geology, 2004, 36, 2, 217-238
dc.identifier.issn 0882-8121
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/38676
dc.description.abstract This 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.subject UNSTEADY UNSATURATED FLOW
dc.subject FINITE ELEMENTS
dc.subject HETEROGENEOUS SOILS
dc.title STOCHASTIC MODELING OF VARIABLY SATURATED TRANSIENT FLOW IN FRACTAL POROUS MEDIA
dc.type Статья


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