Soil texture plays a key role in determining the amount of air and water held in soil. Coarse-textured soils like sandy soils have larger pore spaces, allowing for good drainage but lower water retention. Fine-textured soils like clay have smaller pore spaces, leading to higher water retention but poorer drainage. Loam soils, a mix of sand, silt, and clay, offer a balance of drainage and water retention due to their varied pore sizes.
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