EGU24-18902, updated on 11 Mar 2024
https://doi.org/10.5194/egusphere-egu24-18902
EGU General Assembly 2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

Development of a new computer tool for coupling HYDRUS-1D and MODFLOW

Bartosz Balis1, Mateusz Pawlowicz1, Adam Szymkiewicz2, Jirka Simunek3, Anna Gumula-Kawecka2, and Beata Jaworska-Szulc2
Bartosz Balis et al.
  • 1AGH University, Krakow, Poland (balis@agh.edu.pl)
  • 2Gdansk University of Technology, Gdansk, Poland
  • 3University of California-Riverside, CA, USA

Groundwater management relies increasingly on numerical models to assess past, present, and future conditions, optimize strategies, and protect resources from climate and land use changes. Groundwater systems encompass the unsaturated (vadose) and saturated (groundwater) zones, with vadose zone modeling presenting computational challenges due to nonlinear equations and complex parameters. One possible solution to include the vadose zone processes in groundwater models in a flexible manner is to couple computer programs modeling 3D flow in the saturated zone with programs modeling 1D flow in the vadose zone. 

 

In this study, we introduce the HYDRUS-MODFLOW Synergy Engine (HMSE), a novel coupling approach for HYDRUS-1D and MODFLOW-2005, aimed at enhancing groundwater modeling. HMSE employs external coupling via a versatile interface, offering three deployment options: a desktop application, a Docker container, and a Kubernetes cluster. Users interact through a web interface, enabling project setup, model uploads, configuration adjustments, simulations, and result retrieval.

 

The MODFLOW's area is divided into recharge zones, each assigned a HYDRUS-1D model representing soil profiles, land cover, groundwater depth, and weather conditions. HMSE offers two coupling modes. In the simple mode, groundwater table positions are assumed constant, HYDRUS-1D simulations are performed for the entire period, and average recharge rates are calculated for MODFLOW. In the second coupling mode, MODFLOW and HYDRUS-1D interact iteratively to update the water table position in HYDRUS-1D profiles after each stress period in the MODFLOW simulation. This involves splitting the MODFLOW model into segments corresponding to different stress periods, performing HYDRUS-1D simulations, passing recharge data to the RCH file, running a MODFLOW simulation for each stress period, and using MODFLOW results to calculate the average water table depth for each recharge zone, thus updating the corresponding HYDRUS profiles while avoiding oscillations in recharge flux. 

 

HMSE combines the strengths of mature and validated HYDRUS-1D and MODFLOW-2005 programs, offering a more comprehensive understanding of groundwater systems. Our study presents a preliminary validation of HMSE for a shallow aquifer in northern Poland. We also evaluated HMSE performance in the three deployments (desktop, Docker and Kubernetes). 

How to cite: Balis, B., Pawlowicz, M., Szymkiewicz, A., Simunek, J., Gumula-Kawecka, A., and Jaworska-Szulc, B.: Development of a new computer tool for coupling HYDRUS-1D and MODFLOW, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-18902, https://doi.org/10.5194/egusphere-egu24-18902, 2024.