It is not possible for me to accurately estimate the hydraulic conductivity of an unconfined aquifer without additional information.
The hydraulic conductivity of an aquifer is a measure of its ability to transmit water, and it depends on various factors such as the porosity and permeability of the aquifer materials, the depth and thickness of the aquifer, the extent of the aquifer's saturation with water, and the hydraulic gradient within the aquifer.
The radius of influence around a pumping well is not necessarily related to the hydraulic conductivity of an aquifer.
In order to estimate the hydraulic conductivity of an unconfined aquifer, a hydrologist would need to conduct detailed field measurements and possibly use modeling techniques to take into account the various factors that affect the aquifer's ability to transmit water.
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