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The capacity of porous materials like sand and gravel to transmit water is referred to as hydraulic conductivity or permeability. These materials typically have high porosity and larger pore spaces, allowing water to flow through them more easily compared to finer materials like clay. The efficiency of water transmission in sand and gravel is crucial for various applications, including groundwater recharge, drainage systems, and construction. Overall, their ability to transmit water is significantly influenced by factors such as grain size, shape, and arrangement.

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