Definitions & Terms used in Irrigation
That water is adsorbed from an atmosphere of water vapour because of attractive forces in the surface of particles.
It is the log of in one of the two associated process or phenomena during reversion.
It is the plant, which reflects specific growing condition by its presence or character of growth.
It is the maximum rate at which a soil under given condition and at given time can absorb water when there is no divergent flow at borders
Intake Rate or Infiltration Velocity:
It is the rate of water entry into the soil expressed as a depth of water per unit area applicable or divergence of flow in the soil.
It refers to the quantity of water, exclusive of precipitation, required for crop production. This amounts to net irrigation requirement plus other economically avoidable losses. It is usually expressed in depth for given time.
It is removal of soluble material by the passage of water through the soil.
It is the fraction of water entering the soil that must pass through the root zone in order to prevent soil salinity from exceeding a specific value.
It is the exchange of heat whereby air over crop is cooled to supply heat for evaporation.
It is the down word movement of water through the soil.
Permanent Wilting Point (PWP):
Permanent wilting point is the moisture content in percentage of soil at which nearly all plants wilt and do not recover in a humid dark chamber unless water is added from an outside source. This is lower limit of available moisture range for plant growth ceases completely. The force with which moisture is held by dry soil this point corresponds to 15 atmospheres.
Permeability is the property of a porous medium to transmit fluids It is a broad term and can be further specified as hydraulic conductivity and intrinsic permeability.
It is the logarithm of height in cm of column of water which represents the total stress with which water is held by soil.
It is the negative logarithm of hydrogen ion concentration.
It represents evaporation from a large body of free water surface. It is assumed that, there is no effect of addictive energy .It is primarily a function of evaporative demand of climate.
It is the amount of water evaporated in a unit time from short uniform green crop growing actively and covering an extended surface and never short of water. Penman prefers the term potential transpiration.
It is the water escaped through the soil under gravitational forces.
It is removal of excess water known as free or ravitational water from the surface or below the surface of farm land to create favorable condition for proper growth and development of the plot.
when the excess water saturates the pores spaces removal of water of water by downward flow through the soil is called subsurface drainage.
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