Purpose. Podzolized Chernozems (Greyzemic Phaeozems) and typical low-humus Chernozems (Haplic Chernozems) form the basis of agricultural land in the Sokal ridge. They belong to the category of especially valuable soils, have long been used intensively mainly under arable land, and experience increased anthropogenic pressure, which leads to physical degradation. At the same time, there is little information on the agrophysical state of Chernozems in the scientific literature. Therefore, the study of Chernozems of the Sokal ridge is relevat in the context of the development of degradation processes and ways of optimizing the physical properties of soils.The purpose of the research is to characterize the current state of Chernozems of the Sokal ridge in the context of the development of degradation processes. In order to achieve this goal, the following tasks were carried out: field and laboratory studies of soils were conducted, their degradation rates were assessed. The object of the study is podzolized and typical Chernozems. The subject of research comprises structural and aggregate composition, general physical properties, water permeability of the soil.Data & Methods. When writing the article, we used our own materials from field and laboratory studies. The generally accepted methods of soil research were used (comparative-geographical, comparative profile, field and analytical methods). Physical degradation of soils was evaluated according to the methods adopted in Ukraine.Results. The following types of physical degradation of soils were investigated: structural destruction, lump formation, overconsolidation, crust formation, and water permeability deterioration. According to the research results, the content of air-dry agronomically valuable aggregates of 0.25–10.0 mm in the arable horizon of podzolized Chernozems is 17.37–30.48%, typical low-humus Chernozems – 27.83–41.00%. According to accepted estimates, the structurally-aggregate state of soils is characterized as unsatisfactory. The degree of degradation of the structurally aggregate composition of arable Chernozems is characterized as high and very high (crisis). Among the structural aggregates, the lump fraction prevails, the content of which is 55.42–82.17%.In terms of the density of the structure of the arable layer from 1.22 to 1.56 g/cm3 and the total porosity – 53.3–42.3%, the soils underwent physical degradation of mainly medium and high levels. Soil compaction leads to a decrease in their water permeability and increased erosion on the slopes.The physical degradation of Chernozems of the Sokal ridge has a purely anthropogenic origin. Optimization of the agrophysical conditions of the studied soils consists in reducing the specific pressure on the soil, minimizing the use of heavy machinery, applying organic fertilizers, sowing green manure crops, preserving eroded soils.
Read full abstract