Soil absorption refers to the process by which water and nutrients are taken up by the soil. This occurs when rainwater or irrigation water seeps into the ground, filling the spaces between soil particles. The ability of soil to absorb water depends on its texture, structure, and organic matter content. Sandy soils, for example, drain quickly, while clay soils retain water longer. Effective soil absorption is crucial for plant growth, as it allows roots to access moisture and essential nutrients. Additionally, proper absorption helps prevent surface runoff, reducing erosion and promoting groundwater recharge. Healthy soil management practices can enhance absorption capabilities, benefiting both agriculture and the environment.