Soil moisture is the amount of water in the soil.
Soil moisture refers to the water that is held in the soil and is influenced by factors such as precipitation, temperature, and soil properties. The type of biome present, as well as the suitability of land for growing crops, are determined by the same criteria.
Soil moisture will typically range from 10% to 45 percent, but it may be greater during and after irrigation. The water in your soil is held in the pores, which are holes or gaps between individual soil particles, as well as on the surface of the soil particles.
What is the source of soil moisture?
Gravity, osmosis, and capillarity all influence how water travels in soil. By buoyancy, water displaces air from linked macropores and fractures aggregates into which air is trapped, a process known as slaking.
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