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What is Predicting Water Table Fluctuations in Aquifers about?
This paper presents a mathematical model to predict water table fluctuations in an anisotropic aquifer due to time-varying recharge from multiple rectangular infiltration basins. The model uses the Boussinesq approximation and incorporates horizontal anisotropy in hydraulic conductivity, demonstrating significant effects on water table variation. Numerical results validate the analytical solutions against MODFLOW, highlighting the importance of considering time-varying recharge in groundwater management.
- Author
- Rajeev Bansal
- Language
- EN