This paper provides a proof of the symmetry of the equivalent transmissivity tensor computed with a method based on the solution of the balance equation at the fine scale with integrated finite differences. The basic hypotheses are that the balance equation is solved on a block assigning Dirichlet boundary conditions that vary linearly with the space coordinates and the equivalent transmissivity tensor is computed as the linear tensor relating average flux and hydraulic gradient.

About the symmetry of the upscaled equivalent transmissivity tensor / M. Giudici, C. Vassena. - In: MATHEMATICAL GEOLOGY. - ISSN 0882-8121. - 39:4(2007), pp. 399-408.

About the symmetry of the upscaled equivalent transmissivity tensor

M. Giudici
Primo
;
C. Vassena
Ultimo
2007

Abstract

This paper provides a proof of the symmetry of the equivalent transmissivity tensor computed with a method based on the solution of the balance equation at the fine scale with integrated finite differences. The basic hypotheses are that the balance equation is solved on a block assigning Dirichlet boundary conditions that vary linearly with the space coordinates and the equivalent transmissivity tensor is computed as the linear tensor relating average flux and hydraulic gradient.
Settore GEO/12 - Oceanografia e Fisica dell'Atmosfera
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Utilizza questo identificativo per citare o creare un link a questo documento: http://hdl.handle.net/2434/38145
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