Proper management and evaluation of environmental effects for coastal groundwater aquifers require accurate estimation of salt and fresh water movement. For this we compare two numerical methods to study saltwater intrusion. The two numerical methods are the CIP (constrained interpolation profile) and the MOC (method of characteristics). The two numerical methods are used to solve the salt transport equation. The two methods are applied and compared to saltwater intrusion experiments for confined and unconfined aquifer case studies. It is found that for both cases, the CIP-method is superior in terms of calculation time while keeping an acceptable numerical accuracy
Sea Water Intrusion (SWI) is one of the major hydrological problem in coastal aquifers. This global ...
Sea Water Intrusion (SWI) is one of the major hydrological problem in coastal aquifers. This global ...
Coastal aquifers are very vulnerable to seawater intrusion through, for example, the overdraft of gr...
Saltwater intrusion into coastal aquifers is a global issue, exacerbated by increasing demands for f...
Saltwater intrusion into coastal aquifers is a global issue, exacerbated by increasing demands for f...
In this study, saltwater intrusion in coastal aquifers and prevention techniques were investigated u...
The saltwater intrusion in a coastal aquifer is a highly complex and nonlinear process. The manageme...
The saltwater intrusion in a coastal aquifer is a highly complex and nonlinear process. The manageme...
This study demonstrates the influence of climate change-induced sea level rise on multiobjective sal...
The objective of this study is to simulate the seawater intrusion into unconfined aquifer near shore...
Saltwater intrusion occurs in coastal areas worldwide and a theoretical investigation of its sources...
Abstract. Seawater intrusion in coastal aquifers is generally three dimensional (3-D) in nature. In ...
Saltwater intrusion in coastal aquifers due to human intervention has become a major challenge in di...
A two-dimensional numerical model of variable-density groundwater flow and dispersive solute transpo...
A series of three-dimensional numerical simulations using a multidimensional hydrodynamic dispersion...
Sea Water Intrusion (SWI) is one of the major hydrological problem in coastal aquifers. This global ...
Sea Water Intrusion (SWI) is one of the major hydrological problem in coastal aquifers. This global ...
Coastal aquifers are very vulnerable to seawater intrusion through, for example, the overdraft of gr...
Saltwater intrusion into coastal aquifers is a global issue, exacerbated by increasing demands for f...
Saltwater intrusion into coastal aquifers is a global issue, exacerbated by increasing demands for f...
In this study, saltwater intrusion in coastal aquifers and prevention techniques were investigated u...
The saltwater intrusion in a coastal aquifer is a highly complex and nonlinear process. The manageme...
The saltwater intrusion in a coastal aquifer is a highly complex and nonlinear process. The manageme...
This study demonstrates the influence of climate change-induced sea level rise on multiobjective sal...
The objective of this study is to simulate the seawater intrusion into unconfined aquifer near shore...
Saltwater intrusion occurs in coastal areas worldwide and a theoretical investigation of its sources...
Abstract. Seawater intrusion in coastal aquifers is generally three dimensional (3-D) in nature. In ...
Saltwater intrusion in coastal aquifers due to human intervention has become a major challenge in di...
A two-dimensional numerical model of variable-density groundwater flow and dispersive solute transpo...
A series of three-dimensional numerical simulations using a multidimensional hydrodynamic dispersion...
Sea Water Intrusion (SWI) is one of the major hydrological problem in coastal aquifers. This global ...
Sea Water Intrusion (SWI) is one of the major hydrological problem in coastal aquifers. This global ...
Coastal aquifers are very vulnerable to seawater intrusion through, for example, the overdraft of gr...