Review of the Effect of Climatic Conditions to
the Development of Erosion Process in Soils of
Azerbaijan
Volume 1 - Issue 2
RAE Aliyev ZH*
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- Institute of Soil Science and Agrochemistry of ANAS, Azerbaijan
*Corresponding author:
RAE Aliyev ZH, Institute of Soil Science and Agrochemistry of ANAS, Baku, Azerbaijan
Received: August 30, 2018; Published: September 04, 2018
DOI: 10.32474/OAJESS.2018.01.000109
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Abstract
The Researchers proved that the process of soil erosion is also closely linked to climatic conditions of the region. Therefore,
depending on the climatic conditions of the erosive processes are different in both forms of its manifestation, and the quantitative
indicators of development. For example, in the north-eastern part of the Greater Caucasus Highlands powerful deposition of
snow cover, high intensity of spring melting of snow and summer rain water rainfalls the calling intensive lavages and size of its
development areas. But here, against a backdrop of high air temperatures during the growing season, pronounced wind regime
and extremely low relative humidity of the air is wind erosion. Climate also affects the surface configuration. Humid areas where
vegetation cover protects the soil from severe manifestations of water and wind erosion, characterized by soft, rounded slopes.
Abbreviations: Climate; Soil; Erosion; Infiltration
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