Applied Geosciences - Geohydromodelling

Application studies

Aim of the model application studies are the characterization, quantitative description and prognosis of non-isothermal flow and reactive transport process occurring in the subsurface. Applications are both on the laboratory as well as the field and reservoir scale. Application areas are:

  • The detailed simulation of laboratory and field experiments for process characterization, optimization and parameter identification
  • Simulation of energy- (e.g. methane or hydrogen) or CO₂-storage in the subsurface and the induced reactive flow and transport processes and geomechanic effects
  • High resolution simulation of borehole heat extractors
  • Prognosis of ground water contamination and biodegradation processes and of contaminated site remediation
  • Simulation and assessment of monitoring- and site investigation strategies
  • Application of high performance computing methods for reservoir scale simulations



Fig.1: Bench-scale experimantal and numeric simulation of solutes in heterogeneous porous media on the laboratory scale (Figure: E. Ballarini, in Ballarini, E., Bauer, S., Eberhardt, C. & Beyer, C., 2014. Evaluation of the Role of Heterogeneities on Transverse Mixing in Bench-Scale Tank Experiments by Numerical Modeling. Groundwater, 52(3), 368–377, doi:10.1111/gwat.12066)



Fig. 2: Analysis and validation of pressure monitoring in a virtual CO2 storage formation (Figure: K. Benisch, in Benisch, K. and Bauer, S., 2013. Short- and long-term regional pressure buildup during CO2 injection and its applicability for site monitoring. International Journal of Greenhouse Gas Control 19, 220-233, doi: 10.1016/j.egypro.2013.06.260.)


Brine vs CO2

Fig. 3: Numerical model of the convection flow in the subsurface induced by the chemical reaction of injected CO2 with brine and parent rock. After 1000 years of  equilibrium reaction, the brine density increases by 23 gl-1 due to salinity  alterations. The model space measures 87.5 m by 35.0 m. The top 10.0 m of the model space are discretized with 0.05 m by 0.05 m, the lower 25.0 m with 0.05 m by 0.10 m (Figure: A.B. Mitiku and S. Bauer).