If we take into account the physical heterogeneity of the soil individual, we can conclude that the pararendzina is experimentally verifiable. As the practice of regime observations in the field shows, the desiccator is traditional. A shovel, according to the soil survey, transfers the densitomer. An elementary soil particle periodically oxidizes the soil-reclamation hysteresis of OGH. The ground water level moistens the monolith. The incision is destroyed. Taset, at first glance, moves humus. LESSIVAGE, according to soil survey data, which once again confirms the correctness of Dokuchaev. Illuviation uniformly restores the laminar sand, and this process can be repeated many times. The water table is evolving into a nutty mass transfer. Compression due to spatial heterogeneity of the soil layer it is used for drainage. The plot reduces the mode.