Hydraulic conductivity is a measure of a material’s ability to transmit water through its pore spaces or fractures. It is a critical parameter in hydrogeology, influencing groundwater flow, the design of wells, and the assessment of aquifers. Hydraulic conductivity depends on factors such as porosity, permeability, and the fluid’s viscosity.
Source Bear, J. (1972). Dynamics of Fluids in Porous Media. Dover Publications.