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Bidirectional sulfate diffusion in saline-lake sediments: evidence from Devils Lake, northeast North Dakota

Geology

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Abstract

Chemical and isotopic gradients in pore water in Devils Lake indicate that maximum rates of sulfate reduction occur between 1 and 3 cm depth in the bottom sediments. The abundance of electron acceptors enables sulfate-reducing bacteria to outcompete methanogenic bacteria for organic material and thereby suppress methane production. Suppression of methanogenesis may be widespread in sulfate-rich lakes and wetlands and may limit methane fluxes from these water bodies to the atmostphere. -from Author

Additional Publication Details

Publication type:
Article
Publication Subtype:
Journal Article
Title:
Bidirectional sulfate diffusion in saline-lake sediments: evidence from Devils Lake, northeast North Dakota
Series title:
Geology
Volume
20
Issue:
4
Year Published:
1992
Language:
English
Larger Work Type:
Article
Larger Work Subtype:
Journal Article
Larger Work Title:
Geology
First page:
319
Last page:
322
Number of Pages:
4