Title

Electrolyte-Induced Solute Permeability Effects in Compacted Smectite Membranes

Abstract

Experiments suggest that increasing electrolyte flux into a compacted smectite membrane may result in greater permeability of the membrane to the electrolyte. The influx of electrolyte into the membrane pores decreases the double layer thickness, therefore reducing the clay's ability to exclude anions. As a result, solute previously accumulated in the concentration polarization layer (CPL) may be able to dissipate through the membrane, producing a temporary situation where the effluent is more concentrated than the feed solution. Of course, at some juncture the CPL will diminish sufficiently so that the effluent concentration will be the same as that of the feed solution and a true state will be reached. The fact that increasing electrolyte concentration within the clay membrane decreases the membrane efficiency implies that the result of solute accumulation in geological basins, even though a portion of such accumulation is attributable to the solute filtering ability of low permeability rocks, is the ultimate cessation of membrane effects. At the start of the cycle, shale membranes have low solute concentrations and thus high rejection capabilities. The largest amount of solute accumulates deep in the basin center, where vertical flux rates are high. Because of greater solute concentration within the aquifer, the solute concentration in the centrally located membranes rises more quickly than that of those located near the basin margins. Therefore, the cessation of membrane effects occurs first in the deep center of the basin and gradually moves upward and outward toward the basin margins. The fact that membrane efficiency decreases as pore solute concentration increases might help explain why conclusive trends attributable to membrane effects have not been more commonly observed in the subsurface.

Department(s)

Geosciences and Geological and Petroleum Engineering

Keywords and Phrases

Aquifers; Effluents; Electrolytes; Filtration; Mechanical Permeability; Polarization; Rocks; Concentration Polarization Layer; Electrolyte Flux; Geological Basin; Smectite Membranes; Clay Minerals, Electrolyte Flux; Membranes

International Standard Serial Number (ISSN)

8832927

Document Type

Article - Journal

Document Version

Citation

File Type

text

Language(s)

English

Rights

© 1994 Elsevier, All rights reserved.

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