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This article reviews the literature on soil erosion from an environmental perspective.
Based on the analysis of scientific sources, the main causes of erosion processes and their consequences
were determined. The lithological and geomorphological conditions of soil erosion in the northern part
of Namangan region were thoroughly studied.
It was found that erosion processes disrupt the normal course of soil formation processes,
change the morphological properties of soils, deteriorate physical, water, biological, agrochemical and
other properties. features.
The cause of erosion in the examined area is the presence of surface water flow; The greater the
flow, the greater the washing and erosion. The flow regime depends on the nature of the relief, the
amount of precipitation, soil properties, vegetation cover and human economic activity. The greatest
influence on the formation of surface water is the surface relief: the steepness of the slopes, the
exposure, the shape and length of the slopes, the depth of local erosion bases.
Based on the structure of the surface of the region, geographical location, geological age, relief
and the nature of the rocks included in the composition, six geomorphological regions were identified,
which differ from each other not only in lithological and geomorphological diversity, but also in
heterogeneity. soil cover and their susceptibility to erosion processes.
 

  • Web Address
  • DOI
  • Date of creation in the UzSCI system26-12-2023
  • Read count19
  • Date of publication25-12-2023
  • Main LanguageIngliz
  • Pages44-48
English

This article reviews the literature on soil erosion from an environmental perspective.
Based on the analysis of scientific sources, the main causes of erosion processes and their consequences
were determined. The lithological and geomorphological conditions of soil erosion in the northern part
of Namangan region were thoroughly studied.
It was found that erosion processes disrupt the normal course of soil formation processes,
change the morphological properties of soils, deteriorate physical, water, biological, agrochemical and
other properties. features.
The cause of erosion in the examined area is the presence of surface water flow; The greater the
flow, the greater the washing and erosion. The flow regime depends on the nature of the relief, the
amount of precipitation, soil properties, vegetation cover and human economic activity. The greatest
influence on the formation of surface water is the surface relief: the steepness of the slopes, the
exposure, the shape and length of the slopes, the depth of local erosion bases.
Based on the structure of the surface of the region, geographical location, geological age, relief
and the nature of the rocks included in the composition, six geomorphological regions were identified,
which differ from each other not only in lithological and geomorphological diversity, but also in
heterogeneity. soil cover and their susceptibility to erosion processes.
 

№ Author name position Name of organisation
1 AKHMEDOV B.R. teacher , Namangan Engineering and Technology Institute
№ Name of reference
1 1. V.N.Federko. Economic and geographical foundations of improving the territorial structure of nature management in Uzbekistan. Abstract of the dissertation.PhD, 2018.
2 2. M.N.Zaslavsky. Ways to increase the productivity of slope lands and protect them from erosion. "International people.agricultural journal", No. 5,1982.
3 3. G. I. Shvebs. Sovremennaya paradigma erosiovedeniya i ee prikladnoe znachenie [Modern paradigm of erosion studies and its applied significance]. Moscow State University, 1981.
4 4. Kh.M.Mustafayev, B.K.Shakuri - Study of the effectiveness of the use of trace elements on eroded soils of Azerbaijan. Tbilisi. 1980.
5 5. Kh.Kh.Khamdamov. Irrigation erosion and measures to control it in the Zarafshan valley. Author's abstract. doct. dissert., T., 1975.
6 6. M.S.Kuznetsov Methodology for predicting soil washout and assessing the potential danger of irrigation erosion. Biol. nauki, No. 8, 1977.
7 7. Kh.M.Makh'sudov. Eroded serozems and ways to increase their productivity. "Fan" T., 1981.
8 8. G.A.Cheremisinov. Eroded soils and their productive use. "Kolos" Moscow, 1968.
9 9. B.K.Shakuri. The content of gross and mobile forms of trace elements in the soils of Transcaucasia. g. Soil science. №4. 1981.
10 10. Gafurova L.А., Ergasheva O.Х., Djalilova G.T., Distinctive features of the distribution of medium high mountain soils and their degree of erodibility // European Science Review. – Austria, 2018. - P. 10-13. (03.00.00. № 6)
11 11. Jalilova G. T. - Geoinformation analysis of erosion processes in the middle and low mountains of Uzbekistan. Abstract of the dissertation, Doctor of Biological Sciences, 2018.
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