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Soil moisture refers to the water held within the soil, playing a crucial role in the water cycle and supporting plant life. When precipitation occurs, some water infiltrates the soil, while excess may become runoff. This stored soil moisture is then lost through evaporation back into the atmosphere or absorbed by plants for transpiration.

The amount of soil moisture is influenced by factors like precipitation rates, soil type, and plant cover. In regions with limited rainfall, such as those practicing dry farming, efficient storage and utilization of soil moisture are essential for crop cultivation. Soil moisture levels fluctuate, generally rising after rain and decreasing during dry periods with high evaporation and transpiration rates. The study of soil moisture is vital for understanding plant growth, erosion, and overall water balance in a catchment area.123

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