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Infiltration rate can be slowed by several factors, including soil compaction, which reduces pore spaces and limits water movement. High clay content in soil can also impede infiltration due to its dense structure and low permeability. Additionally, the presence of vegetation or organic matter can create surface crusts that hinder water absorption. Lastly, land management practices, such as excessive tilling or urbanization, can alter soil structure and affect infiltration rates.

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