The process of infiltration is affected by many different
factors. Important factors are the following:
(i) Soil Texture and Structure:
It is already made clear that the water cannot continue to enter
soil more rapidly than it is transmitted downward. The conditions at the
surface, therefore, cannot increase infiltration unless the transmission
capacity of the soil profile is adequate.
The continuity of non-capillary or large pores provides easy
paths for percolating water. If the subsoil formation has coarse texture the
water may infiltrate into the soil so quickly that no water will be left for
runoff even if rainfall is quite heavy. On the contrary clayey soils after
soaking some water in the initial stages of the rainfall may swell
considerably. It makes the soil almost watertight and infiltration may get
reduced to practically negligible extent.
(ii) Conditions at Soil Surface:
Even if the subsoil has excellent under drainage but at the
surface soil pores are sealed due to turbid water or by in wash of fine soil
particles it may prevent entry of water into the soil and infiltration rate
will be low.
(iii) Soil-Moisture Content:
When the soil is fairly dry the rate of infiltration into the
soil is quite high. The infiltration rate diminishes as the soil-moisture
storage capacity is exhausted. After this infiltration rate equals transmission
rate. The rate of infiltration in early phases of a rainfall will be less if
the soil pores are still filled from previous rain storm.
(iv) Type of Vegetative Cover:
Vegetative cover affects surface entry of water significantly.
The vegetation or mulches protect the soil surface from impact of rain drops.
The lengthy and extensive root system penetrate the soil and increases its porosity.
Organic matter from crops promotes a crumbly by structure and improves soil
permeability. Forest canopy protects soil surface whereas row crops provide
less protection to soil.
(v) Soil Temperature:
If saturated soil mass gets frozen due to severe low temperature
it becomes nearly impermeable. It affects the infiltration.
(vi) Human Activities on Soil Surface:
If the soil surface gets compacted due to
construction of roads, operation of tractors and other farm implements and
machinery the porosity of the soil is decreased. As a result bigger pores are
almost eliminated making soil impermeable. It reduces the infiltration rates
appreciably.
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