| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4740756 | Journal of Applied Geophysics | 2010 | 10 Pages |
Abstract
âºHysteresis between fluid and bulk apparent electrical conductivity can be caused by both large-scale heterogeneity and subscale heterogeneity described by dual-domain mass transfer. âºThe shape and magnitude of the observed hysteresis is controlled by the spatial distribution of hydraulic heterogeneity, mass transfer rate between domains, and ratio of mobile to immobile porosity. âºThe shape of the hysteresis curve is indicative of the length scale over which mass transfer is occurring.
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Authors
Daniel D. Wheaton, Kamini Singha,