| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4700898 | Chemical Geology | 2007 | 12 Pages |
Abstract
The profiles demonstrate that, in addition to strong vertical redox related chemical changes, there is significant spatial heterogeneity. Whilst overall there is evidence for net reduction of sulfate within the peatland pore-waters, this can be reversed, at least temporarily, during periods of drought when sulfide oxidation with resulting acid production predominates.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Simon H. Bottrell, Robert J.G. Mortimer, Mike Spence, Michael D. Krom, Joanna M. Clark, Pippa J. Chapman,