期刊
GEOMICROBIOLOGY JOURNAL
卷 24, 期 7-8, 页码 547-558出版社
TAYLOR & FRANCIS INC
DOI: 10.1080/01490450701670137
关键词
sediment; organic matter; oxidation; manganese; cycle; redox
Both natural and anthropogenic processes are responsible for excessive organic loading of submerged soils, with detrimental environmental consequences. The often insufficient natural attenuation can be enhanced by exploiting microbial manganese cycles. This review describes how an anoxic oxidation of organic matter with concomitant reduction of MnO2 can link up with a reoxidation of the resulting, soluble Mn(II) in oxic layers. The potentially attainable oxidation rates through these natural cycles are of the same order as the organic carbon accumulation rates. The microbiology and physiology of the responsible organisms are discussed, as well as examples of naturally occurring manganese cycles and the possibility to engineer this natural phenomenon.
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