| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4546976 | Journal of Contaminant Hydrology | 2011 | 13 Pages |
Abstract
⺠We measured diffusion coefficients for intact saturated redbed sandstone samples. ⺠Tracers were amino-G-acid and calcium bromide solutions, and inert. ⺠Diffusibilities were â¤Â 4x those reported previously for other redbed sandstones. ⺠We suggest an open fabric, a result of the shallow depth of the sandstone. ⺠We speculate that other shallow sandstones may have similarly high diffusibilities.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Khairul Bashar, John H. Tellam,