Non-Darcian flow in a single confined vertical fracture toward a well
Non-Darcian flow towards a well which fully penetrates a confined single vertical fracture is
presented in this paper on the basis of the Izbash equation. We have obtained semi …
presented in this paper on the basis of the Izbash equation. We have obtained semi …
Fuzzy solution of nonlinear Boussinesq equation
C Tzimopoulos, K Papadopoulos… - Journal of …, 2022 - iwaponline.com
In this paper, the solution of the one-dimensional second-order unsteady nonlinear fuzzy
partial differential Boussinesq equation is examined. The physical problem concerns …
partial differential Boussinesq equation is examined. The physical problem concerns …
A class of exact solutions of the Boussinesq equation for horizontal and sloping aquifers
MS Bartlett, A Porporato - Water Resources Research, 2018 - Wiley Online Library
The nonlinear equation of Boussinesq (1877) is a foundational approach for studying
groundwater flow through an unconfined aquifer, but solving the full nonlinear version of the …
groundwater flow through an unconfined aquifer, but solving the full nonlinear version of the …
A simple and accurate closed-form analytical solution to the Boussinesq equation for horizontal flow
M Hayek - Advances in Water Resources, 2024 - Elsevier
The classical problem used to model the response of an unconfined aquifer to a sudden
change in boundary head is considered in this paper. This problem is usually modeled …
change in boundary head is considered in this paper. This problem is usually modeled …
Exact and approximate analytical solutions for unsteady fully developed turbulent flow in porous media and fractures for time dependent boundary conditions
KN Moutsopoulos - Journal of Hydrology, 2009 - Elsevier
The problem of recharge of water to an initially dry, semi-infinite aquifer is investigated,
where the occurrence of turbulent flow is considered. By applying a similarity transform an …
where the occurrence of turbulent flow is considered. By applying a similarity transform an …
Solutions of the Boussinesq equation subject to a nonlinear Robin boundary condition
KN Moutsopoulos - Water Resources Research, 2013 - Wiley Online Library
The case of inflow to an aquifer or porous medium inhibited by the presence of a
semipervious (clogging) layer is investigated. The flow process is characterized by transient …
semipervious (clogging) layer is investigated. The flow process is characterized by transient …
The hysteresis response of groundwater to reservoir water level changes in a plain reservoir area
Y Huang, K Miao, X Liu, Y Jiang - Water Resources Management, 2022 - Springer
Reservoir immersion will lead to some environmental geological problems, such as soil
swamping or salinization, reduction of building foundation strength, or even overall …
swamping or salinization, reduction of building foundation strength, or even overall …
Traveling wave solution of the Boussinesq equation for groundwater flow in horizontal aquifers
HA Basha - Water Resources Research, 2013 - Wiley Online Library
An approximate nonlinear solution of the one‐dimensional Boussinesq equation is
presented using the traveling wave approach. The solution pertains to a semi‐infinite …
presented using the traveling wave approach. The solution pertains to a semi‐infinite …
Accurate approximate semi-analytical solutions to the Boussinesq groundwater flow equation for recharging and discharging of horizontal unconfined aquifers
M Hayek - Journal of Hydrology, 2019 - Elsevier
The Boussinesq equation is usually used to describe one-dimensional unconfined
groundwater movement. Solutions of this equation are important as they provide useful …
groundwater movement. Solutions of this equation are important as they provide useful …
One-dimensional unsteady inertial flow in phreatic aquifers induced by a sudden change of the boundary head
KN Moutsopoulos - Transport in Porous Media, 2007 - Springer
We are examining the classical problem of unsteady flow in a phreatic semi-infinite aquifer,
induced by sudden rise or drawdown of the boundary head, by taking into account the …
induced by sudden rise or drawdown of the boundary head, by taking into account the …