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ROLE OF SOIL IN THE STRUCTURE AND FORMATION OF A STEEP PART OF THE SHORES OF THE RIVERS OF NORTHERN KAZAKHSTAN
Abstract
The study of the structure and formation of shores is now modern issue, both in the assessment of their morphology and the ecological conditions of the steppe zone of Kazakhstan. The article reflects a structure of abrupt bank of Northern Kazakhstan rivers in conjunction with the soil adjacent to it. The authors believe that the intrasoil runoff has not been taken into account so far due to the presence of both soil genetic cracks and high permeability of humidified moisture to "puffy" fouling. Therefore, there should be researched water consumption on the shores with addition and accounting of individual moisture fractures that have percolated through the inter-cracked space, and the share of humidified "puffy" sweat. The consequence of this is the formation of "visors" on steep areas, as well as a noticeable deepening in the places where cracks exit to the face of the precipices. Correct perception of the structure and functioning of the soil, emerging to the river bed, will lead to definitions and accounting of quantitative indicators for the volume of moisture and salts associated with the section of the bed of landscape components.
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