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Soil Compaction
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Soil compaction refers to the process by which soil particles are compressed, reducing the pore spaces between them. This leads to increased soil density and reduced porosity.
Causes of Compaction: Soil compaction can result from various factors, including heavy machinery or equipment traffic, repeated tillage, and natural settling processes.
Effects of Compaction: Compacted soils have reduced aeration, limited root penetration, and impaired water infiltration and drainage. These effects can hinder plant growth and crop yields.
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