1976
DOI: 10.2136/sssaj1976.03615995004000040014x
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Coupling Phenomena in Saturated Homo‐ionic Montmorillonite: I. Experimental

Abstract: A series of experiments was performed to observe the effects of salt concentration differences across a thin layer of homo‐ionic montmorillonite. The water pressure difference, concentration difference, and voltage difference measured with electrodes reversible to the anion were observed as functions of time. A qualitative explanation of the observations is proposed.

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Cited by 51 publications
(26 citation statements)
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“…Elrick et al (27) performed a series of experiments to observe the effects of salt concentration differences across a thin layer of a satured homo-ionic montmorillonite. These authors measured water pressure, concentration, and voltage differences as functions of time.…”
Section: Introductionmentioning
confidence: 99%
See 1 more Smart Citation
“…Elrick et al (27) performed a series of experiments to observe the effects of salt concentration differences across a thin layer of a satured homo-ionic montmorillonite. These authors measured water pressure, concentration, and voltage differences as functions of time.…”
Section: Introductionmentioning
confidence: 99%
“…These calculations were based on the electric double-layer theory and produced a symmetrical coupling matrix. Finally, the data presented in (27) were analyzed by Groenevelt et al (29) using the theoretical development of (28).…”
Section: Introductionmentioning
confidence: 99%
“…For typically non-ideal clay membranes ω should be greater than zero. Elrick et al (1976) measured ω for a Na-montmorillonite slurry with 90 % porosity and obtained a value of 3 x 10 -15 mole/dyne·s. Fritz and Marine (1983) suggested that for more compacted clays, the value of ω should be considerably lower than 3 × 10 -15 mole/dyne·s.…”
Section: Theoretical Experimentsmentioning
confidence: 99%
“…For example, in a clay-water-salt system, the application of a salt concentration gradient creates pore water pressure and electric potential gradients. Such a system was studied by Elrick et al [7]. Thermodynamically coupled flows in near-field regions of nuclear waste repositories have been studied by Carnahan [8].…”
Section: Introductionmentioning
confidence: 99%