Moisture Transfer in Gray-Brown Heavy Clay Soils of the Siyazan-Sumgait Massif

Water yield in gray-brown heavy clay soils of the Siyazan-Sumgait massif with different structural organization indicates the difference in water-holding forces within the structure of each monolith, which form the overall rate of moisture passage through the monolith. The methodology for performing research is based on the principles of comparative analysis of the process of water permeability of the soil environment of natural composition with different levels of structural organization of the soil, including mixed and mixed-fixed polymer. An increase in the moisture capacity of soil aggregates occurs due to the loss of dead-end pores and an increase in the proportion of through capillaries.