EGU26-21343, updated on 14 Mar 2026
https://doi.org/10.5194/egusphere-egu26-21343
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Thursday, 07 May, 08:30–10:15 (CEST), Display time Thursday, 07 May, 08:30–12:30
 
Hall A, A.109
Integrated Groundwater Modeling to Support Sustainable and Equitable Water Management in a Data-Scarce Volcanic Aquifer, Central Mexico
Febe Ortiz1,2, Yijiang Xie, Janice Cabeza, Michael McClain, Yangxiao Zhou, and Shreedhar Maskey
Febe Ortiz et al.
  • 1IHE, Delft, Netherlands
  • 2Delft University of Technology, Delft, Netherlands.

Groundwater resources in the Global South are increasingly stressed by rapid urbanization, agricultural expansion, and climate variability, yet effective management is often constrained by limited monitoring infrastructure and fragmented datasets. This study presents an integrated groundwater resource assessment of the Toluca Valley aquifer (central Mexico), a complex, multilayer volcanic system that supplies water to municipal, industrial, and agricultural users while also supporting inter-basin transfers to Mexico City.

A multilayer numerical groundwater flow model was developed using MODFLOW and implemented in the Groundwater Modeling System (GMS) to simulate aquifer dynamics from 1981 to 2017. The model integrates heterogeneous geological and hydrogeological information, long-term groundwater-level observations from multi-piezometer networks, climate-driven recharge estimates, and spatially distributed abstraction data. Monthly transient simulations were calibrated using a combination of manual and automated parameter estimation, explicitly addressing parameter uncertainty arising from sparse subsurface data. Model validation was strengthened through comparison of MODFLOW-simulated river leakage with independently derived SWAT baseflow estimates, providing cross-model consistency for surface–groundwater interactions.

Results indicate a progressive transition from near-balanced groundwater conditions in the 1980s to persistent storage deficits exceeding 70 million m³/year by 2017, driven primarily by increased abstraction that outpaces recharge. The strongest groundwater declines occur in high-elevation recharge zones, highlighting inequities in resource depletion between recharge areas and demand centers.

By combining accessible public datasets, integrated modeling, and uncertainty-aware calibration, this work demonstrates an inclusive and transferable approach to groundwater characterization in data-scarce regions. The results support evidence-based, locally grounded strategies for sustainable and climate-resilient groundwater governance.

How to cite: Ortiz, F., Xie, Y., Cabeza, J., McClain, M., Zhou, Y., and Maskey, S.: Integrated Groundwater Modeling to Support Sustainable and Equitable Water Management in a Data-Scarce Volcanic Aquifer, Central Mexico, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-21343, https://doi.org/10.5194/egusphere-egu26-21343, 2026.