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Water store in Soil
Soil
Defined as the top layer of the earth's crust. It is formed by
mineral particles, organic matter, water, air and living
organisms.
Water store in different forms
Evaporation
Transpiration
Surface runoff
Infiltration
Subsurface
Ground water
Evaporation
A type of vaporization of a liquid that
occurs from the surface of a liquid into a
gaseous phase
Transpiration
The process by which
moisture is carried
through plants from
roots to small pores on
the underside of
leaves, where it
changes to vapor and
is released to the
atmosphere
Surface runoff
The water, from rain, snowmelt, or other sources, that
flows over the land surface, and is a major
component of the water cycle.
Infiltration
The process by
which water on the
ground surface
enters the soil. It is
measured in
inches per hour or
millimeters per
hour.
Subsurface
The flow of water beneath
earth's surface as part of
the water cycle.
Groundwater
The water located beneath
Earth's surface in soil pore
spaces. A unit of rock or an
unconsolidated deposit is
called an aquifer
Different Factor is involved in water stored
Soil Texture
soil will makeup of the
mineral portion.
The soil is composed
of small particles.
These small particles
are the result of massive
rocks of different
mineralogy sand , silt
and clay etc……
Sandy soils will
have faster water
transmission an
low water
retention
Clay soils will
have slow water
transmission and
high water
retention
Soil structure
The arrangement of soil
particles into groupings.
These groupings are
called peds or
aggregates
which often form
distinctive shapes
typically found with in
certain soil horizons.
For example, granular
soil
Gravitational
 Gravitational water occupies
the larger soil pores (macro
pores) and moves down
under the force of gravity.
 Gravitational water is not
use to plants because it
occupies the larger pores.
 It reduces aeration in the
soil.
Capillary water:
Capillary water is held in the
capillary pores (micro pores).
Capillary water is retained on the soil
particles by surface forces.
It is held so strongly that gravity
cannot remove it from the soil
particles.
The molecules of capillary water
are free and mobile and are present
in a liquid state.
plant roots are able to absorb it.
Hygroscopic water
The water that held tightly on the surface
of soil colloidal particle is known as
hygroscopic water.
It is essentially non-liquid and moves
primarily in the vapor form.
Some microorganism may utilize
hygroscopic water.
Hygroscopic water cannot be separated
from the soil unless it is heated.
Water vapour
Present in soil
atmosphere and
move along vapour
pressure gradients
Important for plant
growth
Free water
This is water
saturated soils

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Water store in soil an its factor

  • 1. Water store in Soil Soil Defined as the top layer of the earth's crust. It is formed by mineral particles, organic matter, water, air and living organisms. Water store in different forms Evaporation Transpiration Surface runoff Infiltration Subsurface Ground water
  • 2. Evaporation A type of vaporization of a liquid that occurs from the surface of a liquid into a gaseous phase
  • 3. Transpiration The process by which moisture is carried through plants from roots to small pores on the underside of leaves, where it changes to vapor and is released to the atmosphere
  • 4. Surface runoff The water, from rain, snowmelt, or other sources, that flows over the land surface, and is a major component of the water cycle.
  • 5. Infiltration The process by which water on the ground surface enters the soil. It is measured in inches per hour or millimeters per hour.
  • 6. Subsurface The flow of water beneath earth's surface as part of the water cycle. Groundwater The water located beneath Earth's surface in soil pore spaces. A unit of rock or an unconsolidated deposit is called an aquifer
  • 7. Different Factor is involved in water stored Soil Texture soil will makeup of the mineral portion. The soil is composed of small particles. These small particles are the result of massive rocks of different mineralogy sand , silt and clay etc……
  • 8. Sandy soils will have faster water transmission an low water retention Clay soils will have slow water transmission and high water retention
  • 9. Soil structure The arrangement of soil particles into groupings. These groupings are called peds or aggregates which often form distinctive shapes typically found with in certain soil horizons. For example, granular soil
  • 10. Gravitational  Gravitational water occupies the larger soil pores (macro pores) and moves down under the force of gravity.  Gravitational water is not use to plants because it occupies the larger pores.  It reduces aeration in the soil.
  • 11. Capillary water: Capillary water is held in the capillary pores (micro pores). Capillary water is retained on the soil particles by surface forces. It is held so strongly that gravity cannot remove it from the soil particles. The molecules of capillary water are free and mobile and are present in a liquid state. plant roots are able to absorb it.
  • 12. Hygroscopic water The water that held tightly on the surface of soil colloidal particle is known as hygroscopic water. It is essentially non-liquid and moves primarily in the vapor form. Some microorganism may utilize hygroscopic water. Hygroscopic water cannot be separated from the soil unless it is heated.
  • 13. Water vapour Present in soil atmosphere and move along vapour pressure gradients Important for plant growth Free water This is water saturated soils