Evaluation of Landscape Elements by Hydrothermal Potential of the Soil Environment

Dissected slope of mountains on the narrow elongated plot and rather narrow sloping land with a different slope than surrounding areas, but preserving the overall direction of the down grade of the landscape, creating go their conditions, structural conditions of growth factor to the HTP soil envi-ronment, is closely correlated with the structure of the soil. HTP allows to link together the potential of the soil environment and the function of substances of soil-plant system, structural self-organization of the first, which is expressed in non-equilibrium conditions of soil developing, which is stimulating environment with the presence of gradients of heat, moisture and density potentials. HTP structural coefficient of soil-to gives the opportunity to make more precise differentiation potential of the soil profile. Certain values of Kstfor the mountain-forest brown soil sunder different ecosystems (forest, meadow) become in the range 0,202-0,566, 0,118-0,408.