Hydrogeological Impact Assessment of Tunnel Excavation Using the TOUGH3–FLAC3D Coupled Modeling Approach.
DOI:
https://doi.org/10.64862/Keywords:
hydrogeological model , TOUGH3–FLAC3D coupling, groundwater inflowAbstract
Tunnel excavation in complex geological settings often induces groundwater inflow, which poses substantial engineering and environmental challenges. Excessive inflow can cause flooding, collapse, and structural instability, leading to delays and increased construction costs. This study employs a coupled TOUGH3–FLAC3D model to investigate the hydro-mechanical interactions between groundwater flow and rock deformation during tunnel excavation. The three-dimensional hydrogeological conceptual model was established based on field geological data and digital terrain to simulate groundwater responses. Simulation results indicate that excavation in the Kangkou Formation may induce a groundwater head decline of 7–10 m near the tunnel and increase local inflow rates up to 7.7 L/min when intersecting the Waiao Fault. The results reveal that under bare rock conditions, tunnel inflow has a negligible effect on reservoir recharge. However, when the tunnel intersects high-permeability fault zones, mitigation measures such as grouting or water-blocking tunnel designs should be implemented to reduce potential impacts on the groundwater system.
References
Rutqvist, J., Wu, Y.S., Tsang, C.F., & Bodvarsson, G. (2002). A modeling approach for analysis of coupled multiphase fluid flow, heat transfer, and deformation in fractured porous rock. International Journal of Rock Mechanics and Mining Sciences, 39, 429–442.
Yang, F.R. (2009). A study on groundwater inflow and its influence on surrounding hydrogeological environment during mountain tunnel excavation. Ph.D. Dissertation, Department of Resources Engineering, National Cheng Kung University, Taiwan.
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Data Availability Statement
The numerical data and model setup (TOUGH3–FLAC3D coupling scripts) are available from the corresponding author upon reasonable request.
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