Spatial-temporal interaction in the system of «seismicity-terminal waters-solar heterogeneity»on the territory of Kyrgyzstan

Based on the analysis of numerous materials, it is shown that geochemical and hydrodynamic inhomogeneities associated with the unstable state of the earths crust are determined by multi-channel ways of entering components into them. The absence of identity of hydroeffects from one earthquake to another in the system atmospheric and space processes-groundwater-earthquakes is influenced by indices of 11-year cycles of solar activity and technical regulation of wells flow rate.