Preprints
https://doi.org/10.5194/egusphere-2022-1185
https://doi.org/10.5194/egusphere-2022-1185
 
24 Nov 2022
24 Nov 2022
Status: this preprint is open for discussion.

Transport mechanisms of hydrothermal convection in faulted tight sandstones

Guoqiang Yan, Benjamin Busch, Robert Egert, Morteza Esmaeilpour, Kai Stricker, and Thomas Kohl Guoqiang Yan et al.
  • Institute of Applied Geosciences, Karlsruhe Institute of Technology (KIT), Karlsruhe, 76131, Germany

Abstract. Motivated by the unknown reasons for a kilometer-scale high-temperature overprint of 270 ~ 300 °C in a reservoir outcrop analog (Piesberg Quarry, northwest Germany), numerical simulations are conducted to identify the transport mechanisms of the fault-related hydrothermal convection system. The system mainly consists of a main fault and a sandstone reservoir in which transfer faults are embedded. The results show that the buoyancy-driven convection in the main fault is the basic requirement for elevated temperatures in the reservoir. We studied the effects of permeability variations and lateral regional flow on the preferential fluid flow pathways, dominant heat transfer types, and mutual interactions among different convective and advective flow modes. The sensitivity analysis of permeability variations indicates that lateral convection in the sandstone and advection in the transfer faults can efficiently transport fluid and heat, thus causing elevated temperatures (≥ 269 °C) in the reservoir compared to purely conduction-dominated heat transfer (≤ 250 °C). Higher-level lateral regional flow interacts with convection and advection and changes the dominant heat transfer from conduction to advection in the transfer faults for the low permeability cases of sandstone and main fault. Simulations with anisotropic permeabilities detailed the dependence of the onset of convection and advection in the reservoir on the directional permeability distribution. The depth-dependent permeabilities of the main fault reduce the amount of energy transferred by buoyancy-driven convection. The increased heat and fluid flows resulting from the anisotropic main fault permeability provide the most realistic explanation for the thermal anomalies in the reservoir. Our numerical models can facilitate exploration and exploitation workflows to develop positive thermal anomalies zones as geothermal reservoirs. These preliminary results will stimulate further petroleum and geothermal studies of fully coupled thermo-hydro-mechanical-chemical processes in faulted tight sandstones.

Guoqiang Yan et al.

Status: open (until 05 Jan 2023)

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Guoqiang Yan et al.

Guoqiang Yan et al.

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Short summary
The physical processes leading to the kilometer-scale thermal anomaly in faulted tight sandstones are numerically investigated. The fluid flow pathways, heat transfer types, and interactions among different convective and advective flow modes are systematically identified. The methodologies and results can be applied to interpret hydrothermal convection-related geological phenomena and to draw implications for future petroleum and geothermal exploration and exploitation in analogous settings.