Answer
The amount of rainwater that soaks into the ground, rather than running off as surface runoff, is influenced by several factors. The type of soil, its permeability, and porosity play a significant role. Sandy and well-structured soils tend to have higher infiltration rates, allowing more water to soak in. On the other hand, compacted or clayey soils may have lower infiltration rates, resulting in increased surface runoff. The slope of the land also matters, as steeper slopes can lead to faster runoff and less time for infiltration.
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