Resumen
determination of groudwater recharge
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surface flow
flow of water that runs through the surface of the earth in its different forms
for the climatics methods different parameters are used
precipitation
groudwater recharge
evapotranspiration
surface flow
precipitation
Precipitation in meteorology is referred to as the fall of water in any of its forms
Equation to determine water balance
λ ¼ 1 = 0; 8 þ 0; 145TÞ
Avec : α ¼ 0; 49239 þ 1; 79:10 2I 7; 71:10 5I2þ 6; 75:10 7I3; I ¼
P12 1;514
j¼1ioù i¼ 5
estimation of potencial and actual evapotranpiration
P ¼ ETR þ R þ I
climatic or water balance methods
more date
it is easer
can by done different methods
direct
geochemical
physical
Evapotranspiration
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Potential evapotranspiration
Amount of water that is or humidity that is returned to the atmosphere in optimal conditions
actual evapotranspiration
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the loss of water or humidity in real conditions
