Field Experimental Study on the Infiltration and Clogging Processes at Aksu Research Site, Kazakhstan

The challenge of a good quality drinking water supply to southeastern Kazakhstan's local population from far-away natural surface water sources motivates groundwater utilization from local aquifers. To prevent groundwater resource deficits, artificial groundwater recharge is needed. To this end, infiltration and clogging processes were evaluated through comprehensive field research in southeastern Kazakhstan's typical river drainage basin (Aksu experimental site). The infiltration scenario included constructed mini pools and their typical soil profile clogging and silting processes. The local aquifer unsaturated and upper saturated zones underwent a detailed study of water balance, hydrodynamic setting, and filtration properties. The research results suggest that the infiltration rate decreased from 15 m/day until the saturation steady state and remained at 0.75 m/day until the end of the experiment. In summer, clogging layers with thicknesses ranging from 3 mm for the clayey silt layer to 6 mm for muddy clay began to form at the mini pools nearly one month after the test began. During infiltration, the mini pools' upper soil layer dirt-holding capacity varied from 3.72 to 5.25 kg/m(2). The field study results serve as a factual basis for artificial replenishment system design and groundwater replenishment methodology optimization in southeastern Kazakhstan and similar regions.

Automated summary

The challenge of providing good quality drinking water supply to the local population in southeastern Kazakhstan from distant natural surface water sources has led to the utilization of groundwater from local aquifers. In this study, infiltration and clogging processes were evaluated to optimize the artificial groundwater recharge system design in the region.