A non-steady state diagenetic model for
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John W. Morse; Peter M. Eldridge
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Article
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2007
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Elsevier Science
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English
β 558 KB
Biogeochemical processes occurring near the sediment-water interface can play an important role in the establishment and persistence of hypoxic-to-anoxic conditions in areas of moderate-to-shallow water depth. Results are given in this paper for diagenetic modeling of two sites from the area on the