The type of water left in the soil after excess water has been drained off, after heavy rainfall and it is available to crop plant is called

Answer Details

After heavy rainfall, soil pore spaces fill with water. The excess water that responds freely to gravity drains downward - this is gravitational water, and it is the first to leave. Once gravitational water has drained away, the water that remains held in the smaller pore spaces by surface tension and capillary forces is called capillary water. This is the water that plant roots can actually absorb, and it is therefore the type that is "available to crop plants."

The other terms describe different categories of soil water:

• Field capacity describes the state of the soil (its moisture content) once gravitational water has drained, not a type of water. At field capacity the soil holds the maximum amount of capillary water.
• Hygroscopic water is a very thin film of water tightly adsorbed onto the surface of soil particles by molecular forces. It is held so tightly that plant roots cannot extract it, so it is not available to crops.
• Gravitational water is the excess water that drains freely under gravity. Far from being the water that stays, it is precisely the water that leaves.

Examination tip: Remember the availability sequence - gravitational water drains away, capillary water is available to plants, and hygroscopic water is unavailable.