Hydraulic Calculation of Artesian Basin Water Resources Artificial Recharge in Mountain Relief Conditions

River water flowing in mountainous areas are characterized by significant seasonal changes due to spring and autumn floods, making their efficient use difficult. Fountain wells increase total water consumption by providing water not only for irrigation but also for drinking and household needs. It is known that in many countries the use of water comes from groundwater basins, into which, in addition to atmospheric precipitation, river runoff is forcibly directed. In flat places, these activities require large financial costs both for water purification and for injection into underground reservoirs. Mountainous areas have high water quality indicators. In addition, natural relief differences make it possible to pump large volumes of fresh water into the underground basin without the use of pumping stations. The volume of water injected into underground aquifers is determined by the pipeline's water pressure, the filtration properties of the aquifers, the number of wells, the distance between them, and other factors. Based on comparisons of the calculated data on water consumption according to different empirical formulas, which showed close results, the mentioned researchers were given reason to believe that these formulas can be trusted. The authors of this paper consider the use of empirical formulae for calculating the replenishment flow rate of an artesian basin is inappropriate, because of the large risk of distorting the real picture. Based on the fundamentals of technical hydromechanics a method for hydraulic calculation of the distribution of flow rates in absorbing wells has been proposed