Pump Testing In-Situ Leach Hydrostratigraphic Units

The hydrostratigraphy of uranium in situ leach sites consists typically of interbedded layers of sand, silt, clay and gravel deposited by fluvial processes. 'These layers usually form leaky multiple aquifer systems where sand and gravel aquifers are separated by silt or clay confining layers (aquitards). It is very important to evaluate the hydraulic properties of the ore zone aquifer and the confining layers by aquifer pump testing to ascertain the effects that in situ leach mining will have on the multiple aquifer system. The degree to which current methods of aquifer pump testing will provide the information necessary to adequately characterize the hydraulic properties of the ore zone aquifer and its confining layers is dependent upon the hydrostratigraphic conditions at the site and the limitations of the testing methods. The primary objectives of the aquifer testing program should be to evaluate the vertical hydraulic conductivity of the confining layers and to quantify leakage into or out of the ore zone under mining conditions.