Estimation of Groundwater Recharge in a Mediterranean Island Aquifer with CMB and HYDRUS-1D Methods: Case study: Bozcaada (Türkiye)

Groundwater recharge is critical because it restores the underground aquifers that supply billions of people. Over-abstraction of groundwater without recharge can lead to falling water tables, land subsidence and long-term ecological damage. As natural recharge is slow in many areas, particularly in arid and semi-arid climates, active management is required to ensure sustainability. Accurate estimation of groundwater recharge is crucial for sustainable water resource management, especially on islands where surface water resources are limited and vulnerable to climate variability. In this study, annual groundwater recharge in the island aquifer was estimated using two different approaches, the Chloride Mass Balance (CMB) method and the numerical modeling tool HYDRUS-1D, using Bozcaada in the northern Aegean Sea, Türkiye. The CMB method is based on chloride concentrations measured in precipitation and groundwater samples, while the HYDRUS-1D model simulates water movement within the unsaturated zone over time. The analysis showed that the average annual recharge on the island was calculated to be 39 mm using the CMB method. In contrast, the HYDRUS-1D model provided more variable results for the different observation wells, with annual recharge estimated at 270 mm in the RK6 region, 75 mm in the RK12 region and 165 mm in the RK13 region. The results indicate a higher recharge potential, especially in highly permeable formations such as the Kirazlı Formation which includes sandstone. However, the study shows that the limitations of the CMB method become apparent on small islands and in areas at risk of seawater intrusion, leading to conflicting results between the methods. Consequently, it is emphasized that the combined use of approaches such as CMB and HYDRUS can provide a more comprehensive and reliable assessment, even under limited data conditions. This study received funding from the PRIMA programme of the European Union under grant agreement No 2221.

Authors

Institutions

Publication Details

Journal
Zenodo (CERN European Organization for Nuclear Research)
Published
2026-05-28
DOI
https://doi.org/10.5281/zenodo.20428209
Primary Topic
Groundwater and Isotope Geochemistry
Type
article
Field-Weighted Citation Impact
0.00
Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Estimation of Groundwater Recharge in a Mediterranean Island Aquifer with CMB and HYDRUS-1D Methods: Case study: Bozcaada (Türkiye)

Özge Yaren Türkseven, Raquel Marijuan, ORHAN GUNDUZ, ALPER BABA
Zenodo (CERN European Organization for Nuclear Research)
Groundwater and Isotope Geochemistry
article

Estimation of Groundwater Recharge in a Mediterranean Island Aquifer with CMB and HYDRUS-1D Methods: Case study: Bozcaada (Türkiye)

Özge Yaren Türkseven, Raquel Marijuan, ORHAN GUNDUZ, ALPER BABA
article en

Abstract

Groundwater recharge is critical because it restores the underground aquifers that supply billions of people. Over-abstraction of groundwater without recharge can lead to falling water tables, land subsidence and long-term ecological damage. As natural recharge is slow in many areas, particularly in arid and semi-arid climates, active management is required to ensure sustainability. Accurate estimation of groundwater recharge is crucial for sustainable water resource management, especially on islands where surface water resources are limited and vulnerable to climate variability. In this study, annual groundwater recharge in the island aquifer was estimated using two different approaches, the Chloride Mass Balance (CMB) method and the numerical modeling tool HYDRUS-1D, using Bozcaada in the northern Aegean Sea, Türkiye. The CMB method is based on chloride concentrations measured in precipitation and groundwater samples, while the HYDRUS-1D model simulates water movement within the unsaturated zone over time. The analysis showed that the average annual recharge on the island was calculated to be 39 mm using the CMB method. In contrast, the HYDRUS-1D model provided more variable results for the different observation wells, with annual recharge estimated at 270 mm in the RK6 region, 75 mm in the RK12 region and 165 mm in the RK13 region. The results indicate a higher recharge potential, especially in highly permeable formations such as the Kirazlı Formation which includes sandstone. However, the study shows that the limitations of the CMB method become apparent on small islands and in areas at risk of seawater intrusion, leading to conflicting results between the methods. Consequently, it is emphasized that the combined use of approaches such as CMB and HYDRUS can provide a more comprehensive and reliable assessment, even under limited data conditions. This study received funding from the PRIMA programme of the European Union under grant agreement No 2221.

Zenodo (CERN European Organization for Nuclear Research)
Izmir Institute of Technology (TR), Central Arkansas Radiation Therapy Institute (US)
Openalex Percentile: Top 6%
Groundwater and Isotope Geochemistry
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.