Assessment and Diagnostic Indicators of Organic Matter Qualitative Composition of Yaroslavl Volga Region Post-Agrogenic Soils Against the Background of Modern Climate Changes

Abstract

The purpose of this work was to characterize the postagrogenic transformation of soil organic matter (SOM). For decision of this purpose the results of chemodestructive fractionation (CDF), the content of chlorophylls a and b , pheophetins and carotenoids, and Margalef's pigment index (PI) were used newly. Subjects of inquiry-humus horizons of soils of arable lands and fallow areas of Poshekhonsky district of the Yaroslavl region of the Russian Federation-were stitch together into two groups with differ in the type of land use. In one of them, the soils remained arable for 30-40 years (arable-arable group), in the other - the soils of arable land for the same time period were transferred to the fallow (arable-fallow group). It was found that increasing the soil water content of fallow plots compared to arable soils can lead: to improved livelihoods of the soil algocenoses (the value of PI Margalef decreased) to increase the carbon content of organic compounds, to increase the number legkomyslenno fraction in the organic component of soil, increased hydrolytic processes that reduce the content of carotenoids and chlorins (in particular, pheophytinand chlorophylls a and b) in SOM composition. Thus, results of CDF and content of chlorophylls a and b , pheophetins and carotenoids can be used to assess the postagrogenic transformation of SOM, and Margalef's PI-to characterize soil algocenosis.