Journal
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL
Volume 67, Issue 6, Pages 1701-1702Publisher
SOIL SCI SOC AMER
DOI: 10.2136/sssaj2003.1701
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It was recently shown that the solute diffusion coefficient tends to zero at some threshold water content. We examine this phenomenon in light of recent simulation results from a network diffusion model. The experimental and simulation results agree, inviting an explanation from continuum percolation theory.
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