THERMODYNAMIC ASPECTS OF THE GEOSYSTEM FUNCTION OF THE PEDOSPHERE

Modern unceasing processes of dehumification and degradation arable soils require the search for new non-traditional approaches to solving this global environmental problem, which determines relevance research. After all, plowing significantly disrupts thermodynamic interaction soil with factors. The purpose publication is consider regularities evolution properties pedosphere from a geosystem perspective, define concept geomembrane properties, reveal mechanism regulating environment based on its homeostasis, will allow more reasonable explanation forecast modern evolutionary changes in cover higher perspective organizational level geosystem. main tasks are defined as: development methodology studies climatic factors, creation tools monitoring course thermodynamically unbalanced environment, their approbation Forest-Steppe zone Ukraine. It proposed as dissipative non-equilibrium system that constantly process self-stabilization self-organization due factors environment. Therefore, homeostasis means presence subordinate energy-consuming certain intensity, form structure soil, pore space. was determined general direction pedosphere, an element Earth's lithospheric shell, densification parent rock formation structural macroporosity heterogeneity. shown example Ukraine, have zonal nature aimed at limiting power active energy-mass exchange.
 dynamics manifestation hierarchical organization, be used solve purely applied issues, such assessing impact climate change, humus formation, fertility, increasing sustainability ecological safety use.