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• W2187843318 abstract "— 70 — Oxidation-reduction reactions play a key role in ecologically important biogeochemical processes in soil and influence on soil chemical, biochemical, physical and biological properties. The redox potential is a critical environmental factor because it governs the chemical and biochemical form of many compounds and their availability for plants and soil microorganisms, and it also influences on the products of microbial metabolism in soil. Furthermore, oxidation and reduction of organic matter are intimately linked with energy transformations which may form the basis of an energy-yielding metabolism [1–3]. Peat has traditionally been characterized in the Russian literature as possessing a hydrologically active, low-density upper layer, and a higher-density, hydrologically inactive lower layer. This classification was formalized by Ingram [4] who identified the upper layer as the acrotelm and the lower layer as the catotelm. The acrotelm contains roots and decomposing plant material, typically possesses a relatively a high hydraulic conductivity (~1 cm s -1 ), and crucially is defined as the zone through which the water table fluctuates. The catotelm is the water saturated anaerobic zone that comprises layers of defense peat with small pore spaces and hydraulic conductivity 3–5 orders of magnitude lower [5–7]." @default.
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• W2187843318 date "2011-01-01" @default.
• W2187843318 modified "2023-09-26" @default.
• W2187843318 title "ACTIVITIES OF ENZYMES PARTICIPATING IN REDOx POTENTIAL IN ThE TwO DEPThS OF TAGAN PEATLAND" @default.
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