Calculation of Azarshahr plain storage coefficient by usingThe simplified equation of hydrogeology in order to Certainty of mathematical model
| Category | Hydrogeology |
|---|---|
| Group | GSI.IR |
| Location | 21th symposium on geosciences |
| Holding Date | 24 May 2008 |
Abstract:
In the step by step balance method, by having one of the hydrodynamic coefficients of the aquifer, the other coefficient is calculable.
The study area is first divided into equal square nets, then by plotting the equipotential lines of months Azar and Esfand the value of hydraulic head for the center of squares obtained.
By using the simplified equation of hydrogeology, transmissivity and infiltration flux from surface flows, the storage coefficient for the square nets was calculated. Negative values of some data are due to neglecting the ratio of outflow.
General:
In the step by step balance method, by having one of the hydrodynamic coefficients of the aquifer, the other coefficient is calculable.
The study area is first divided into equal square nets, then by plotting the equipotential lines of months Azar and Esfand the value of hydraulic head for the center of squares obtained.
By using the simplified equation of hydrogeology, transmissvity and infiltration flux from surtace flows, the storage coefficient for the square nets was calculated. Negative values of some data are due to neglecting the ratio of outflow