THE COMPOSITION AND CHANGES OF WATER-SOLUBLE SALTS IN THE TERMIZ DISTRICT

Authors

  • Kadirova D. A. Head of the Department of Agrochemistry and Soil Science Doctor of Biological Sciences, Prof. Tashkent State Agrarian University
  • Allayarov Kh. N. "Agrochemistry and Soil Science"" Basic Doctoral student in Soil Science.
  • Turdaliev J. M. Junior Research Fellow of “TAITI” Doctor of Philosophy (PhD) in Biological Sciences
  • Kh. N. Rasulov Department of Agrochemistry and Soil Science, Ph.D., Associate Professor, Tashkent State Agrarian University

Keywords:

The soils are irrigated desert-sandy, slightly saline, irrigated desert-meadow, moderately saline, irrigated meadow-alluvial soils are highly saline.

Abstract

We know that in recent years, despite the improvement of land reform in a number of regions of our republics, the salinization of saline soils has been increasing. We see that the supply of easily soluble salts in water and their composition in all cases represent a certain value of salinity. The reserve of salts in direct deposits is the same as that of soil-forming rocks and anthropogenic fastors, and is present in certain quantities in the same soil-forming rocks. On the alluvial slopes, irrigated service-sandy, meadow-meadow and irrigated meadow soils are formed. It can be observed in new and old irrigated areas of I-II surface terraces of Surkhandarya; it differentiates soils even in differentiated areas and in differentiated layers, provided that organic products are differentiated

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Published

2025-01-12

Issue

Vol. 6 No. 1 (2025): wos

Section

Articles

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