“…An analysis of more than 500 experimental pourings and injections of water into boreholes at the Nurek hydro development site, whose foundation is composed of intercalating strata of sandstones and siltstones, and the Toktogul hydro development, where crystalline limestones are widespread, showed [2] that the magnitude of specific water absorption, calculated on the basis of discharge during the first 30 min of injection, is quite close to the results obtained upon stabilization of the discharge with an incremental duration of 3 h-The coefficient of correlation of the indicated quantities varies from 0.8 to 0.9, increasing for larger values of water absorption. Lykoshin [1] and L. P. Konyarova [3] arrived at the same conclusions. A.…”