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contributor authorFranco M. Francisca
contributor authorPedro Arduino
date accessioned2017-05-08T21:32:03Z
date available2017-05-08T21:32:03Z
date copyrightJuly 2007
date issued2007
identifier other%28asce%291532-3641%282007%297%3A4%28311%29.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/55117
description abstractImmiscible flow governs the macroscopic behavior of aqueous and non-aqueous phase liquids inside the porous media. Ganglia generation and movement of the advancing front during fluid displacement can only be described by means of microscopic models. In this study, a pore network cellular automata is used to simulate the displacement of a nonaqueous phase liquid by water inside a porous media. Pore sizes are generated using random and stochastic fields. The numerical model captures the evolution of interfaces and fluid movement for each pressure applied to the displacing fluid. Observed trends suggest that ganglia size and shape, and fingering are directly related to anisotropy, pore size spatial variability and correlation length. The results show that micro- and mesoscale porous media properties control the nonaqueous phase residual saturation and observed macoscopic behavior.
publisherAmerican Society of Civil Engineers
titleImmiscible Displacement Model for Anisotropic and Correlated Porous Media
typeJournal Paper
journal volume7
journal issue4
journal titleInternational Journal of Geomechanics
identifier doi10.1061/(ASCE)1532-3641(2007)7:4(311)
treeInternational Journal of Geomechanics:;2007:;Volume ( 007 ):;issue: 004
contenttypeFulltext


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