thewater holding capacity is the highest in
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The water holding capacity is the highest in slit and clay soil surface
Water holding capacity can be determined by measuring soil moisture at Filed capacity and at Permanent Welting Point. The difference between those two soil moisture values is the water holding capacity. Usually a soil water characteristic curve is developed for the soil to determine its water holding capacity.
Soils with smaller particles (silt and clay) have a larger surface area than those with larger sand particles, and a large surface area allows a soil to hold more water. In other words, a soil with a high percentage of silt and clay particles, which describes fine soil, has a higher water-holding capacity.
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