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Soil Moisture, typically expressed as Volumetric Water Content, refers to the volume of water contained per unit volume of soil, measured in cubic meters per cubic meter (m³/m³) or percentage (%). It is a core parameter describing soil water status and directly participates in surface energy balance, water cycle processes, and vegetation growth activities. Volumetric water content reflects the degree to which soil pores are filled with water, influenced by multiple factors including precipitation, irrigation, evaporation, transpiration, and soil permeability. It serves as a key indicator in agriculture, hydrology, meteorology, and environmental science.
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