Саноатда рақамли технологиялар Volume 3 Issue 1 (2025) · pp. 43-48
SOME FACTORS ARE THE FORMATION OF GROUNDWATER IN THE TAKYR AND PODTAKYR ZONES
Акимова, Азима Пердебаевна, Очилов, Голибжон Ерназаругли, Рахимбаев, Отабек Давлатбаевич, Жетписбаева, Айзада КауисКизи, Akimova, Azima Perdebayevna, Ochilov, G‘olibjon Ernazaro‘g‘li, Raximbayev, Otabek Davlatbayevich, Jetpisbayeva, Ayzada QauisKizi, Akimova, Azima Perdebayevna, Ochilov, Golibjon Ernazarugli, Rakhimbaev, Otabek Davlatbaevich, Jetpisbaeva, Ayzada Qauiskizi
Abstract
The article is devoted to the study of natural factors that, to one degree or another, contribute to the formation of lenses of fresh groundwater in limestone and marl strata of Neogene deposits. According to the results of the research, changes in the salinity of soils in depth have been established and the possibility of artificial accumulation of drinking and saturated groundwater, by the method of construction of artificial structures, and underground reservoirs in fractured and karst rocks has been revealed.
takyrsaeration zonesatmospheric precipitationclay soils of desertserosive-accumulative type of reliefsalinity of soilsfracturingkarstтакырызоны аэрации
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