| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 10113922 | Applied Geochemistry | 2018 | 16 Pages |
Abstract
Two reactive transport modelling examples show that equilibration time of bentonite with different ionic strength waters varies significantly. The redistribution of porosity slows down or accelerates diffusive transport.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
A. Jenni, U. Mäder,