KATTAQO‘RG‘ON SUV OMBORI ATROFIDAGI HUDUDLARDA SIZOT SUVLARINING SATHI VA GIDROMORFIZM JARAYONINING SHAKLLANISHI
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Maqolada Kattaqo‘rg‘on suv omborining atrofidagi tuproqlarning gidromorfizmga uchrash jarayoni o‘rganilgan, natijalarga ko‘ra,
suv omborining janubiy, g‘arbiy, sharqiy tomonlarida lalmi tipik bo‘z tuproqlar tarqalgan bo‘lib, gidromorfizmga uchramagan,
shimoliy tomonida esa gidromorfizmning kam, o‘rta va kuchli darajada shakllangan, buning sababi shimoliy tomoni bilan qolgan
tomonlari orasida dengiz sathidan joylashish balandlik orasida 55-60 metr orasida farq bor bo‘lib, chiqish va kirish kanali aynan
shimoliy tomonida joylashgan.
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