Groundwater Flow Modeling in Mining Hydrogeology

Summary

Groundwater flow modelling in mining hydrogeology employs numerical representations of subsurface water movement to inform safe and sustainable mine operations. By integrating geological frameworks, aquifer properties, boundary conditions and pumping regimes, models capture the transient interaction between excavations and regional groundwater systems. Saturated‐zone flow is often simulated with finite‐difference or finite‐element solvers, while coupling to the unsaturated or vadose zone enables prediction of infiltration, capillary rise and evapotranspiration effects. Calibration using site measurements—such as water‐level monitoring, slug and pump tests—and subsequent sensitivity analyses quantify uncertainty and guide further data collection. These models support the design of dewatering schemes for open‐pit and underground mines, evaluation of contaminant transport pathways, prediction of post‐closure rebound and assessment of ecological impacts in arid or water‐stressed regions. Recent methodological advances include three‐dimensional transient formulations, incorporation of fault and fracture networks, automated parameter estimation and integration of remote sensing and machine‐learning techniques to improve forecasting reliability and reduce environmental risks.

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Groundwater Flow Modeling in Mining Hydrogeology publication trend

The graph below shows the total number of articles in groundwater flow modeling in mining hydrogeology across all publications each year (not limited to Nature Index journals).

Technical terms

Aquifer: A geological formation capable of storing and transmitting significant quantities of groundwater.

Dewatering: The active pumping of groundwater to lower the water table around a mine excavation for safe working conditions.

Finite‐element model: A numerical method that divides the subsurface into discrete elements to solve groundwater flow equations in complex geometries.

Saturated zone: The subsurface region in which all pore spaces are filled with water, governing bulk groundwater flow.

Vadose zone: The unsaturated layer above the water table where pores contain both air and water, controlling infiltration and capillary processes.

References

  1. Estimating dewatering in an underground mine by using a 3D finite element model. PLOS ONE (2020).
  2. Open-Pit Mine Dewatering Based on Water Recirculation—Case Study with Numerical Modelling. Energies (2021).
  3. The Significance of Groundwater Flow Modeling Study for Simulation of Opencast Mine Dewatering, Flooding, and the Environmental Impact. Water (2019).

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