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.
Reference: Bear, J. (1972). Dynamics of Fluids in Porous Media. Dover Publications.