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Recent advances in modeling of well hydraulics
HD Yeh, YC Chang - Advances in Water Resources, 2013 - Elsevier
Well hydraulics is a discipline to understand the process of flow to the well in an aquifer
which is regarded as a source of groundwater. A variety of analytical and numerical models …
which is regarded as a source of groundwater. A variety of analytical and numerical models …
A review of groundwater-surface water interaction studies in India
R Gupta, PK Sharma - Journal of Hydrology, 2023 - Elsevier
Worldwide, highly populated countries are experiencing an imbalance between the supply
and demand of water. India is one such example which has only 4% of the world's water …
and demand of water. India is one such example which has only 4% of the world's water …
Groundwater fluctuations in slo** aquifers induced by time-varying replenishment and seepage from a uniformly rising stream
RK Bansal - Transport in porous media, 2012 - Springer
This paper analyses the classical problem of transient surface–groundwater interaction in a
stream–aquifer system under rather realistic conditions. The downward slo** unconfined …
stream–aquifer system under rather realistic conditions. The downward slo** unconfined …
Groundwater flow in slo** aquifer under localized transient recharge: Analytical study
RK Bansal - Journal of Hydraulic Engineering, 2013 - ascelibrary.org
This paper analyzes the groundwater flow system in an unconfined downward-slo**
aquifer of semi-infinite extent in response to localized transient recharge. The aquifer is in …
aquifer of semi-infinite extent in response to localized transient recharge. The aquifer is in …
Unsteady seepage flow over slo** beds in response to multiple localized recharge
RK Bansal - Applied Water Science, 2017 - Springer
New generalized solutions of linearized Boussinesq equation are derived to approximate
the dynamic behavior of subsurface seepage flow induced by multiple localized time-varying …
the dynamic behavior of subsurface seepage flow induced by multiple localized time-varying …
A semi-analytical time integration for numerical solution of Boussinesq equation
G Tang, AN Alshawabkeh - Advances in water resources, 2006 - Elsevier
A semi-analytical time integration method is proposed for the numerical simulation of
transient groundwater flow in unconfined aquifers by the nonlinear Boussinesq equation …
transient groundwater flow in unconfined aquifers by the nonlinear Boussinesq equation …
Modeling of water table profile variations owing to stream–aquifer interaction
A Upadhyaya, MM Kankarej, P Jeet - Water Science & Technology, 2023 - iwaponline.com
Spatial and temporal variations of the water table could be explained by the one-
dimensional Boussinesq equation by incorporating the variables of evapotranspiration and …
dimensional Boussinesq equation by incorporating the variables of evapotranspiration and …
Simulation of two dimensional subsurface seepage flow in isolated anisotropic aquifer
Mathematical models have emerged as important tools for prediction of transient and steady
state behavior of water table in unconfined aquifer under seepage and recharge condition …
state behavior of water table in unconfined aquifer under seepage and recharge condition …
Numerical simulation of groundwater table falling in horizontal and slo** aquifers by differential quadrature method (DQM)
A Ghaheri, SH Meraji - Journal of Hydrologic Engineering, 2012 - ascelibrary.org
Since a nonlinear partial differential equation was developed by Boussinesq based on
Darcy's law and the Dupuit-Forchheimer assumption, it has played an essential role in the …
Darcy's law and the Dupuit-Forchheimer assumption, it has played an essential role in the …
[PDF][PDF] An approximate analytical solution for groundwater variation in unconfined aquifers subject to variable boundary water levels and groundwater recharge
AP Wang, MC Wu, PC Hsieh - AIMS Mathematics, 2024 - aimspress.com
An approximate analytical solution for groundwater variation in unconfined aquifers subject to
variable boundary water levels an Page 1 AIMS Mathematics, 9(10): 28722–28740. DOI …
variable boundary water levels an Page 1 AIMS Mathematics, 9(10): 28722–28740. DOI …