Aquifer permeability

Aquifer permeability refers to how easily water can flow through the porous materials, like gravel, sand, or fractured rock, that store underground water. It depends on the size and connectivity of the pores or cracks within these materials. High permeability means water moves quickly, making it a good source for wells, while low permeability indicates slow flow, which can restrict water movement. Understanding permeability helps determine how accessible and sustainable an aquifer is for water supply, guiding effective groundwater management and well placement.