Management of Saltwater Intrusion in Sloping Coastal Aquifers Using the Meshless Local Petrov–Galerkin (MLPG) Numerical Method

Document Type : Research Paper

Authors

1 1. . PhD Student, Water Science and Engineering, Faculty of Agriculture, University of Birjand, Birjand, Iran.

2 Professor, Department of Civil Engineering, Faculty of Engineering, University of Birjand, Birjand, Iran

3 3. Associate Professor, Department of Water Science and Engineering, Faculty of Agriculture, University of Birjand, Birjand, Iran

4 Seyed Saeid Eslamian, Department of Water Science and Engineering, College of Agriculture, Isfahan Univetsity of Technology, Isfahan, Iran

5 5. Associate Professor, Department of Water Science and Engineering, Faculty of Agriculture, University of Birjand, Birjand, Iran

10.22059/ijswr.2025.402060.670004

Abstract

Coastal fresh groundwater management is a challenging research topic due to the importance of this resource and the significant risks arising from global changes and population growth. Rising sea levels and declining groundwater tables alter the hydraulic gradient and cause the expansion of the saltwater front in coastal aquifers. Moreover, the geometric configuration and morphology of coastal aquifers play a controlling role in saltwater intrusion. In this study, the management of saltwater intrusion in a sloping coastal aquifer using an impermeable cutoff wall was investigated numerically through the Meshless Local Petrov–Galerkin (MLPG) method. Three aquifer bed slope models—including seaward slope (coastal slope, SS), horizontal bed (H), and landward slope (landside slope, LS)—were simulated for different scenarios (no cutoff wall, and cutoff walls with depths of 0.15, 0.30, 0.45, and 0.60 m). The results were compared with previous studies. The findings showed that the geometric shape of the aquifer can affect the extent of saltwater intrusion. Specifically, the advancement of the saltwater front in the seaward and landward sloping aquifers, compared to the horizontal case without a cutoff wall, decreased by 5% and increased by 10%, respectively. In all models, the saltwater intrusion for the 0.60 m wall scenario was 0.50 m, representing the least penetration. Therefore, this scenario can be considered the optimal and most effective wall depth for all cases. To evaluate the accuracy of the MLPG numerical model, the simulation results were compared with the Henry problem and the study by Abd-Elaty & Polemio (2023), and assessed using the RMSE, R², and NSE indices. The results showed that RMSE values in all scenarios were less than 0.06, and R² values exceeded 0.95, indicating excellent agreement between the model and reference data. Model performance, based on the Nash–Sutcliffe Efficiency (NSE) index, was above 0.9 in all cases, confirming the high accuracy and stability of the model in predicting the distribution of the saltwater front.

Keywords

Main Subjects


Introduction

Coastal aquifers are vital sources of freshwater for densely populated coastal regions. Under natural conditions, groundwater flows from inland areas toward the sea. However, excessive groundwater extraction can reverse the hydraulic gradient, allowing seawater to intrude into aquifers and degrade water quality. Climate change, sea-level rise, and reduced aquifer recharge further intensify this process, increasing the risk of groundwater salinization. Given that nearly 70% of the world’s population lives in coastal zones, managing seawater intrusion has become a major environmental and economic challenge. Among various management solutions, subsurface cutoff walls have been recognized as one of the most effective techniques to control the advancement of the saline front. The present study investigates the influence of aquifer bed slope geometry and cutoff wall depth on the extent of saltwater intrusion using the Meshless Local Petrov–Galerkin (MLPG) numerical method.

Method

In this research, the MLPG numerical model was developed to simulate seawater intrusion in a coastal aquifer. This mesh-free approach eliminates the need for complex grid generation and provides higher accuracy in solving partial differential equations compared to finite element and finite difference methods. Modeling was performed in MATLAB using a computational grid of 231 nodes with a uniform spacing of 0.1 m in both directions. Three aquifer slope geometries were considered: seaward slope (SS), horizontal bed (H), and landward slope (LS). Each geometry was simulated under four cutoff wall depths (0.15, 0.30, 0.45, and 0.60 m) and one scenario without a wall. Model parameters were based on the Henry problem, and the model’s accuracy was validated against the study by Abd-Elaty & Polemio (2023). The statistical indicators RMSE, R², and NSE were used to evaluate the model’s precision and performance.

Results

The findings revealed that increasing the cutoff wall depth significantly reduces seawater intrusion. In the horizontal (H) model, increasing wall depth from 0.15 m to 0.60 m reduced intrusion from 0.93 m to 0.50 m—a 50% reduction. In the landward slope (LS) model, the intrusion decreased from 1.05 m to 0.50 m (52.4%), and in the seaward slope (SS) model, it decreased from 0.90 m to 0.50 m (45%).The LS condition showed the highest saltwater advancement, while the SS condition showed the least. In all models, the 0.60 m cutoff wall depth consistently produced the minimum intrusion (0.50 m) and can therefore be identified as the optimal depth. Statistical validation confirmed the high accuracy of the MLPG model: RMSE < 0.06, R² > 0.95, and NSE > 0.9 in all scenarios, indicating excellent agreement with benchmark data. Sensitivity analysis showed that a ±20% change in hydraulic conductivity (K) caused a 6–9% variation in the position of the saline front, highlighting the importance of accurately defining hydraulic properties in simulation models.

Conclusions

This study demonstrates that aquifer bed geometry and cutoff wall depth have a significant impact on seawater intrusion in coastal aquifers. A landward slope increases intrusion by about 10%, while a seaward slope reduces it by about 5%, compared to the horizontal case. The 0.60 m cutoff wall depth was found to be the most effective and optimal configuration across all scenarios. The high accuracy and numerical stability of the MLPG method confirm its potential as a reliable and efficient tool for modeling and managing coastal groundwater systems.

Author Contributions

Conceptualization A. Akbarpour and Z. Baazm; methodology, , A. Akbarpour; software, Z. Baazm and A. Akbarpour; validation S. S. Islamian and H. Khozaimenejad; formal analysis, A. Akbarpour and Z. Baazm; investigation, M. Yaqubzadeh and H. Khozaimenejad. ; resources, Z. Baazm; data curation Z. Baazm, A. Akbarpour and M. Yaqubzadeh,; writing-original draft preparation, Z. Baazm; writing-review and editing, Z. Baazm, A. Akbarpour, M. Yaqubzadeh and H. Khozaimenejad.; visualization, Z. Baazm and M. Yaqubzadeh; supervision, Z. Baazm and A. Akbarpour,; project management A. Akbarpour and M. Yaqubzadeh; funding acquisition, Z. Baazm and A. Akbarpour. All authors have read and agreed to the published version of the manuscript.

Data Availability Statement

Data available on request from the authors.

Ethical considerations

The authors avoided data fabrication, falsification, plagiarism, and misconduct.

Conflict of interest

The author declares no conflict of interest.

Ataie- Ashtiani, B., Hosseinabadi, H. R., & Fatemi, E. (2006). Numerical model of Transport and Contaminant Discharge from Coastal Aquifers into Seaward. Iran- water resources research, 2(1), 1-17. (In Persian).
Abd-Elaty, I., Hany, FA., & Nezhad, M. (2019). Numerical analysis of physical barriers systems efficiency in controlling saltwater intrusion in coastal aquifers. Environ Sci Pollut Res, 26(35):35882–35899. https://doi. org/10.1007/s11356-019-06725-3.
Abd-Elaty, I., Saleh, OK., Ghanayem, H.M., Grischek, T., & Zelenakova, M. (2021). Assessment of hydrological, geohydraulic and operational conditions at a riverbank filtration site at Embaba, Cairo using flow and transport modeling. Journal of Hydrology: Regional Studies, 37(8), 100900. https://doi.org/10.1016/ j. ejrh.2021.100900
Abd-Elaty, I., & Zelenakova, M. (2022). Saltwater intrusion management in shallow and deep coastal aquifers for high aridity regions. Journal of Hydrology: Regional Studies, 40:101026, DOI:https://doi. org/10.1016/ j.ejrh.2022.101026
Abd-Elaty, Il., & Polemio, M. (2023). Saltwater intrusion management at different coastal aquifers bed slopes considering sea level rise and reduction in fresh groundwater storage, Stochastic Environmental Research and Risk Assessment, 37:2083–2098
Abdoulhalik, A., Ahmed, A. & Hamill, G. (2017) A new physical barrier system for seawater intrusion control. Journal of Hydrology, 549, 416–427. [https://doi.org/10.1061/(ASCE)EE.1943-7870.0001194]
Armanuos, A., El-Morshedy, A., & Hassan, H. (2020). Optimization of subsurface wall depth for landfill leachate management. Waste Management, 102, 123–135. [https://doi.org/10.1016/j.wasman.2019.10.041] .
Armanuos, A.M., Al-Ansari, N., & Yaseen, Z.M. (2020). Underground barrier wall evaluation for controlling saltwater intrusion in sloping unconfined coastal aquifers. Water. 12, 2403.
Allow, KA. (2012). The use of injection wells and a subsurface barrier in the prevention of seawater intrusion: a modelling approach. Arab Journal Geosci. 5(5), 1151–1161.
Atluri, S. N. (2004). The meshless method (MLPG) for domain & BIE discretizations. Tech Science Press. [https://engineering.uci.edu/](https://engineering.uci.edu)
Bear, J., Cheng, A.H., Sorek, S., Quazar, D., & Herrera, I. (1999). Seawater intrusion in coastal aquifers, concepts, methods and practices. Kluwer Academic publisher, Dordrecht.
Diersch, H.J. (1988). Finite element modelling of recirculating density-driven saltwater
intrusion processes in groundwater. Advances in Water Resources, 11(1), 25-43.
El Shinawi, A., Kuriqi, A., Zelenakova, M., Vranayova, Z., & Abd-Elaty, I. (2022). Land subsidence and environmental threats in coasta aquifers under sea level rise and over-pumping stress. Journal of Hydrology, 608, 127607. DOI:https://doi.org/10.1016/j.jhydrol.2022.12760
Hans, J., & Diersch, G. (2014). Finite element modeling of flow mass and heat transport in porous and fractured media, springer.
Hughes, JD., & Sanford, WE. (2004). SUTRA-MS: a version of sutra modified to simulate heat and multiple-solute transport, 1207. Open-File Report 1207.
Singh, A. (2012). An overview of the optimization modelling applications. Journal of Hydrology, 5, 466–467. https://doi.org/10.1016/j.jhydrol
Harbaugh, AW., Banta, ER., Hill, MC., & McDonald, MG. (2000). MODFLOW-2000, the U.S. Geological survey modular ground-water model—user guide to modularization concepts and the groundwater flow process: U.S. Geological Survey Open-File Report 00–92, p 121.
IPCC. (2021). The IPCC has finalized the first part of the sixth assessment report, climate change 2021: the physical science basis, the working group i contribution to the sixth assessment report. It was finalized on 6 August 2021 during the 14th Session of Working Group I and 54th Session of the IPCC.
IPCC. (2014). Climate change 2014: synthesis report. In: Core WritingTeam, R.K. Pachauri and L.A. Meyer (eds.) Contribution of working groups I, II and III to the fifth assessment report of the intergovernmental panel on climate change. IPCC, Geneva, Switzerland, pp 151.
IPCC. (2007). An Assessment of the Intergovernmental Panel on Climate Change. Adopted section by section at IPCC Plenary XXVII (Valencia, Spain, 12–17 November 2007), represents the formally agreed statement of the IPCC concerning key findings and uncertainties contained in the Working Group contributions to the Fourth Assessment Report.
Javadi, A., Hussain, M., Sherif, Mohsen., & Farmani, Raziyeh., (2015). Multi-objective Optimization of Different Management Scenarios to Control Seawater Intrusion in Coastal Aquifers. Water Resour Manage, 29, 1843–1857, DOI 10.1007/s11269-015-0914-1.
 Karim zadeh, E. Akbarpour. A. Mohtashami, A. (2024). Simulation of sea water infiltration in coastal aquifer using MLPG numerical method. Journal of Aquifer and Qanat, 5(8), 44-19. https://doi.org/10.22077/jaaq.2024.8115.1076.(In Persian).
Liu, G. R., & Gu, Y. T. (2005). An introduction to meshfree methods and their programming. Springer. [https://link.springer.com/](https://link.springer.com)
Li, L., Barry, D. A., Stagnitty, F. and Parlange, J. Y. (1999). Submarine Ground Water Discharge and Associated Chemical Input to a Coastal Sea. Water Resources Research., 35 (11). 3253-3259.
Liu, W.K., Jun, S., & Zhang, Y.F. (1995). Mesh free methods, CRC PRESS, Boca Raton, London, NewYork, Washington, D.C.
Moore, W. S. (1996). Large Ground Water Inputs to Coastal Waters Revealed by Ra226 Enrichment, Nature, 380, pp. 612-614.
Mazzia, A., and Putti, M. (2002). Mixed-finite element and finite volume discretization for heavy brine simulations in groundwater, Journal of Computational and Applied Mathematics, 147, 1, 191-213.
Mohamed, A., Abu-Bakr, H.A.-A., Farag, M.M., Taher, M.H., Mohamed, H.G., & Ahmed, G. (2023). Hydrogeophysical and Hydrochemical Assessment of the Northeastern Coastal Aquifer of Egypt for Desalination Suitability. Water,15, 423.
McDonald, RI., Green, P., Balk, D., Fekete, BM., Revenga, C., Todd, M., & Montgomery, M. (2011). Urban growth, climate change, and freshwater availability. Proceedings of the National Academy of Sciences. 108, 6312–6317. https://doi.org/10.1073/pnas.1011615108.
Omajene, A, Egbai J. C., & Okolie E. C., (2024)..Investigation of Saltwater Intrusion into Freshwater Aquifers in Some Estuary Environment in Niger Delta, Journal of Water Resources and Ocean Science, 13(4), 94-104, DOI:10.11648/j.wros.20241304.11.
Polemio, M., & Zuffiano, L.E. (2020). Review of utilization management of Groundwater at risk of salinization. Journal of Water Resources Planning and Management, 146(9), 20. https://doi.org/10.1061/ (ASCE)WR.1943-5452. 0001278.
Rastogi, A. K., Choi, G. W., & Ukarande, S. K. (2004). Diffused interface model to prevent ingress of seawater in multi-layer coastal aquifers, Journal of Special Hydrology,.1-31.
Roger, L.J., Kazuro, M., Kei, N. (2010). Effects of artificial recharge and flow barrier on seawater intrusion. Journal of Ground Water. https://doi.org/10.1007 /s00477-023-02381-9.
Shokri, N., & Homayoun, S. R. (2013). Evaluation of methods for solving the advection diffusion equation using the finite volume method, 12th Iranian Hydraulic Conference, Karaj, https://civilica. com/doc/379534.(In Persian).
Sun, Q., Zheng, T., Zheng, X., & Walther, M. (2021). Effectiveness and comparison of physical barriers on seawater intrusion and nitrate accumulation in upstream aquifers. Journal of Contaminant Hydrology, 243, 103913 https://doi.org/10.1016/j. jconhyd.2021.103913.
Voss, C.I, & Provost, A.M. (2010). SUTRA-A model for saturated-unsaturated variable-density ground-water flow with solute or energy transport. Report 02–4231.
Wada, Y., Flo¨rke, M., Hanasaki, N., Eisner, S., Fischer, G., Tramberend, S., Satoh, Y., Van Vliet M.T.H., Yillia, P., Ringler, C. & et al. (2016). Modeling global water use for the 21st century: the water futures and solutions (WFaS) initiative and its approaches. Geoscientific Model Development, 9:175–222. https://doi.org/10.5194/gmd-9-175-2016.
Yang, J., Graf, T., Luo, J. & Lu, C., (2021). Effect of cutoff wall on freshwater storage in small islands considering ocean surge inundation. Journal of Hydrology. 603, 127143. https://doi.org/10.1016/ j.jhydrol.2021.127143.
Yu. Ye., Chiogna, G., Cirpka, O., Grathwohl, P., & Rolle, M. (2015). Experimental Investigation of CompoundSpecific Dilution of Solute Plumes in Saturated Porous Media: 2-D vs. 3-D Flow-Through Systems. Journal of Contaminant Hydrology, 172, 33-47.
Zheng, C., & Wang, P.P. (1999) MT3DMS, a modular three-dimensional multi species transport model for simulation of advection, dispersion and chemical reactions of contaminants in groundwater systems: documentation and user’s guide. U.S. Army Engineer Research and Development Center Contract Report SERDP-99-1, Vicksburg, MS, pp 202.