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Title: ROLE OF SOIL IN THE STRUCTURE AND FORMATION OF A STEEP PART OF THE SHORES OF THE RIVERS OF NORTHERN KAZAKHSTAN
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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
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1314-2704
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English
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17
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32
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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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conference
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17th International Multidisciplinary Scientific GeoConference SGEM 2017
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17th International Multidisciplinary Scientific GeoConference SGEM 2017, 29 June - 5 July, 2017
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Proceedings Paper
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STEF92 Technology
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International Multidisciplinary Scientific GeoConference-SGEM
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Bulgarian Acad Sci; Acad Sci Czech Republ; Latvian Acad Sci; Polish Acad Sci; Russian Acad Sci; Serbian Acad Sci & Arts; Slovak Acad Sci; Natl Acad Sci Ukraine; Natl Acad Sci Armenia; Sci Council Japan; World Acad Sci; European Acad Sci, Arts & Letters; Ac
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477-482
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29 June - 5 July, 2017
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website
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cdrom
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3454
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soil; humus cracks; inter-cracked space; moisture drain; inside a fissure drain
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