| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 9458213 | Applied Geochemistry | 2005 | 12 Pages |
Abstract
The Stokes-Einstein relationship, based on the temperature dependency of the viscosity of bulk water, could not be used to describe the temperature dependence of the diffusion of HTO in OPA. This additionally indicates the slightly different structure of the pore water in OPA.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
L.R. Van Loon, W. Müller, K. Iijima,