The movement of water in soil is influenced by various soil characteristics such as texture, structure, organic matter content, and compaction. Finer-textured soils like clay have smaller pore spaces, leading to slower water movement compared to coarser-textured soils like sand. Soil structure affects water movement by influencing the arrangement of aggregates and pore spaces. Organic matter improves soil structure and water-holding capacity. Compaction reduces pore spaces, limiting water infiltration and drainage.
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