Solute Transport In Heterogeneous Porous Media
Name
1994.12 Zhao_Toksoz.pdf
Size
1.1 MB
Format
Adobe PDF
Checksum (MD5)
46041233d12f4bcd380f0eb44194377e
Author(s)
Zhao, Xiaomin
Toksoz, M. Nafi
Date Issued
1994
Publisher
Massachusetts Institute of Technology. Earth Resources Laboratory
Series/Report no.
Earth Resources Laboratory Industry Consortia Annual Report;1994-12
Abstract
Solute mass transport in porous media is strongly correlated with pore fluid flow. The
analysis of solute transport is an effective means for studying medium heterogeneities.
In this study, we discuss the effects of heterogeneity on the tracer transport. Assuming
steady fluid flow, we have simulated tracer transport in various permeability heterogeneities. The results show that the tracer distribution is very closely correlated with the medium heterogeneity, and anisotropy in tracer transport exists when there is permeability lineation and large permeability contrast between low- and high-permeability regions. An important feature by which the tracer transport differs from the fluid flow field is that the tracer transport tends to smear the effects of a thin non-permeable layer (or small permeability barriers) through diffusion into the low-permeability layer, while the fluid flow cannot penetrate the low-permeability layer. In addition, the modeling results also show that the tracer transport strongly depends on the tracer source dimension, as well as the flow source dimension.
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