The quantification of groundwater recharge is an important but challenging task in groundwater flow modeling because recharge varies spatially and temporally. The goal of this study is to present an innovative methodology to estimate groundwater recharge rates and zone structures for regional groundwater flow models. Here, the unknown recharge field is partitioned into a number of zones using Voronoi Tessellation (VT). The identified zone structure with the recharge rates is associated through a simulation-optimization model that couples MODFLOW-2000 and the hybrid PSOLVER optimization algorithm. Applicability of this procedure is tested on a previously developed groundwater flow model of the Tahtali Watershed. Successive zone structure sol...
Groundwater recharge rates calculated with the GROWA model have been applied as the recharge boundar...
International audienceThe distribution of groundwater fluxes in aquifers is strongly influenced by t...
Abstract Recharge is a fundamental component of groundwater systems, and in groundwater-modeling exe...
The quantification of groundwater recharge is an important but challenging task in groundwater flow ...
The quantification of groundwater recharge is an important but challenging task in groundwater flow ...
The aim of this study is to present a linked simulation optimisation model to estimate the groundwat...
The aim of this study is to present a linked simulation optimisation model to estimate the groundwat...
The aim of this study is to present a linked simulation-optimisation model to estimate the groundwat...
The aim of this study is to present a linked simulation optimisation model to estimate the groundwat...
Groundwater recharge is the main forcing of regional groundwater flow. In traditional partial‐differ...
Groundwater recharge is the main forcing of regional groundwater flow. In traditional partial‐differ...
Groundwater recharge is the main forcing of regional groundwater flow. In traditional partial‐differ...
Groundwater recharge, transit and discharge areas for aquifers must be found. Their location depends...
The accurate estimation of groundwater recharge is the key and a necessity for sustainable use of gr...
An analysis of recharge, i.e. the quantity of water that infiltrates from the land surface to the a...
Groundwater recharge rates calculated with the GROWA model have been applied as the recharge boundar...
International audienceThe distribution of groundwater fluxes in aquifers is strongly influenced by t...
Abstract Recharge is a fundamental component of groundwater systems, and in groundwater-modeling exe...
The quantification of groundwater recharge is an important but challenging task in groundwater flow ...
The quantification of groundwater recharge is an important but challenging task in groundwater flow ...
The aim of this study is to present a linked simulation optimisation model to estimate the groundwat...
The aim of this study is to present a linked simulation optimisation model to estimate the groundwat...
The aim of this study is to present a linked simulation-optimisation model to estimate the groundwat...
The aim of this study is to present a linked simulation optimisation model to estimate the groundwat...
Groundwater recharge is the main forcing of regional groundwater flow. In traditional partial‐differ...
Groundwater recharge is the main forcing of regional groundwater flow. In traditional partial‐differ...
Groundwater recharge is the main forcing of regional groundwater flow. In traditional partial‐differ...
Groundwater recharge, transit and discharge areas for aquifers must be found. Their location depends...
The accurate estimation of groundwater recharge is the key and a necessity for sustainable use of gr...
An analysis of recharge, i.e. the quantity of water that infiltrates from the land surface to the a...
Groundwater recharge rates calculated with the GROWA model have been applied as the recharge boundar...
International audienceThe distribution of groundwater fluxes in aquifers is strongly influenced by t...
Abstract Recharge is a fundamental component of groundwater systems, and in groundwater-modeling exe...