| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 9529128 | Chemical Geology | 2005 | 19 Pages |
Abstract
Aerobic degradation during sediment deposition appears to control the molecular composition and reactivity of SOM in aquifer sediments and to affect the potential of subsequent diagenetic pyrite formation. In addition, (paleo)hydrological conditions may result in the accumulation of a ferrous iron-bearing carbonate phase precipitated during the exfiltration of Fe(II)-containing anoxic groundwater.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
N. Hartog, J. Griffioen, P.F. van Bergen,