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In heterogeneous porous media, transmissivity can be regarded as a spatial stochastic variable. Transmissivity fluctuations induce stochasticity in the groundwater velocity field and transport features. In order to model subsurface phenomena, it is i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a97fd13d464976420351f1e50595e476
http://hdl.handle.net/11583/2742271
http://hdl.handle.net/11583/2742271
