[Oxidoreductase activity of peat soils as an indicator of the degree of biochemical transformation of drained and forested bogs in west Siberia].
Multivariate analysis unambiguously demonstrated the differentiation of oxidoreductase activity (catalase, peroxidase, and dehydrogenase) in peat soils after a 20-25-year period of bog drainage and afforestation. The enzyme activity depended on the drainage depth. A statistical model has been developed to predict the degree of humification of peat organic matter from peroxidase activity and moisture of drained soils. Soil peroxidase activity can be an important indicator of the degree of biochemical transformation of drained and forested bogs.
Efremova
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Ovchinnikova
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D001711:Biotransformation; D008954:Models, Biological; D010084:Oxidation-Reduction; D010088:Oxidoreductases; D012800:Siberia; D012988:Soil Microbiology; D013997:Time Factors; D014197:Trees; D053833:Wetlands
D010088:Oxidoreductases