determination of groudwater recharge

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chapter 9

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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