The assessment of the organic matter state in drained peat soils as related to the environmental conditions by the methods of multidimensional statistics
Т. Т. Ефремова, Т. М. Овчинникова
Abstract
Т. Т. Ефремова, Т. М. Овчинникова
Abstract
The specificity of the group and fraction composition of the organic matter in peat soils drained to a different extent that have developed for a 20-to 25-year period of hydro-and forest amelioration was characterized using the methods of multidimensional statistics. The differences in the organic matter of the soils studied are mainly determined by the contents of humic and fulvic acid of fractions 1 and 3, as well as of hemicelluloses and cellulose. The degree and depth of the humification are inversely related to the soil moisture and directly related to the peroxidase activity.
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The specificity of the group and fraction composition of the organic matter in peat soils drained to a different extent that have developed for a 20-to 25-year period of hydro-and forest amelioration was characterized using the methods of multidimensional statistics. The differences in the organic matter of the soils studied are mainly determined by the contents of humic and fulvic acid of fractions 1 and 3, as well as of hemicelluloses and cellulose. The degree and depth of the humification are inversely related to the soil moisture and directly related to the peroxidase activity.
Key concepts: Humus, Peat, Soil water, Organic matter, Environmental chemistry, Environmental science, Soil science, Soil organic matter