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On the relationship between microstructure and electrical and hydraulic properties of sand‐clay mixtures
Author(s) -
Wildenschild Dorthe,
Roberts Jeffery J.,
Carlberg Eric D.
Publication year - 2000
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2000gl011553
Subject(s) - porosity , thermal conduction , quartz , permeability (electromagnetism) , materials science , electrical resistivity and conductivity , microstructure , mineralogy , electrical conduction , montmorillonite , hydraulic conductivity , clay minerals , conductance , composite material , geology , soil science , soil water , chemistry , condensed matter physics , membrane , biochemistry , electrical engineering , engineering , physics
A series of laboratory experiments, including measurements of electrical properties, permeability, and porosity, were performed on saturated sand‐clay mixtures. Different mixtures and packing geometries of quartz sand and 0 to 10% Na‐montmorillonite clay were investigated using solutions of CaCl 2 and deionized water. Two main regions of electrical conduction exist: a region dominated by surface conduction and a region where the ionic strength of the saturating fluid controlled conduction. For low fluid conductivities, the sample geometry was found to greatly affect the magnitude of the surface conductance. The influence of the microstructural properties on the electrical properties was quantified by estimating formation factors, Λ‐parameters, and surface conductances. The surface conductances estimated using the theory of Johnson et al. [1986] agreed well with measured values. We suggest that high and low bounds on the expected surface and bulk conductances in a natural system can be derived from the measurements on these artificial geometries.