Orol bo'yi hududlari gidromorf tuproqlarining meliorativ holati
Abstract
This article discusses changes in the Aral Sea region under the influence of natural and anthropogenic factors, desertification processes and features of soil formation in these areas. As desertification intensifies, arid-zonal factors play a key role in soil formation; hydromorphic soils are transformed into automorphic soil types. As a result of sharp changes in natural and climatic conditions and increased desertification, hydromorphic processes in the Aral Sea region are gradually replaced by automorphic soil formation.
Authors
Abduraxmonov Nodirjon Yulchiyevich
Academic degree and academic title: Doctor of Biological Sciences, Professor
Institutional affiliation: Institute of Soil Science and Agrochemical Research
Position: Deputy General Director
A.R.Jo'rayev
Institutional affiliation: Ministry of Agriculture
Egamberdiyev Jobir. A
Institutional affiliation: Research Institute of Soil Science and Agrochemistry
Position: Independent seeker
Б.Р. Рамазонов
Academic degree and academic title: Doctor of Philosophy Biological Sciences
Institutional affiliation: Chirchik state Pedagogical Institute
Position: Teacher