Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
9537797 | Engineering Geology | 2005 | 9 Pages |
Abstract
With this set-up, an extensive program of measurements of coupling phenomena like streaming potentials, electroosmosis, and membrane potentials in a sodium montmorillonite is started. Preliminary results of streaming potential measurements are presented and demonstrate that the build-up of a streaming potential due to a hydraulic gradient is a reproducible process that influences the water flow through the clay, and that the extent of the streaming potential depends on the salt concentration of the permeating solution.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geotechnical Engineering and Engineering Geology
Authors
Katja Heister, Pieter J. Kleingeld, Thomas J.S. Keijzer, J.P. Gustav Loch,