НЕКОТОРЫЕ ФАКТОРЫ ФОРМИРОВАНИЕ ПОДЗЕМНЫХ ВОД ТАКЫРНЫХ И ПОДТАКЫРНЫХ ЗОНАХ

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.