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Soil Moisture and Soil Environmental Science

What is Soil Moisture?

Soil moisture is the amount of water retained in the soil. It is expressed as a percentage of the total soil volume. Soil moisture plays a critical role in plant growth, soil stability, and nutrient availability.

Best Measure of Soil Moisture

The best measure of soil moisture is the soil water potential. Soil water potential is a measure of the energy required to remove water from the soil. It is expressed in units of joules per cubic meter (J/m³).

Factors Affecting Soil Moisture

Several factors affect soil moisture, including:

  • Precipitation
  • Evaporation
  • Transpiration
  • Infiltration
  • Percolation
  • Soil texture
  • Soil structure
  • Organic matter content

Importance of Soil Moisture

Soil moisture is essential for plant growth. Plants use water for photosynthesis, respiration, and nutrient uptake. Soil moisture also affects soil stability and nutrient availability. Dry soils are more susceptible to erosion, while wet soils can restrict root growth and nutrient uptake.

Managing Soil Moisture

Managing soil moisture is a key element of soil management. There are several ways to manage soil moisture, including:

  • Irrigation
  • Mulching
  • Tillage
  • Cover cropping