EGU26-16969, updated on 14 Mar 2026
https://doi.org/10.5194/egusphere-egu26-16969
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Tuesday, 05 May, 14:25–14:35 (CEST)
 
Room -2.43
Low-Frequency Distributed Acoustic Sensing reveals transient flow and heat-transfer regimes during geothermal injection
Johannes Hart1,2, Christopher Wollin1, Aurelio Andy3, Toni Ledig4, Thomas Reinsch5,6, and Charlotte Krawczyk1,2
Johannes Hart et al.
  • 1GFZ Helmholtz Centre for Geosciences, 2.2, Potsdam, Germany (johannes.hart@gfz.de)
  • 2Technical Univerity of Berlin, Berlin, Germany
  • 3Technical University of Munich, Munich, Germany
  • 4Stadtwerke München GmbH, Munich, Germany
  • 5Fraunhofer IEG, Bochum, Germany
  • 6Ruhr-Univerity Bochum, Bochum, Germany

High-resolution diagnostics of flow and heat transfer in deep geothermal wells are commonly constrained by sparse downhole instrumentation and production-logging tools that require well intervention, interrupting steady-state operations. Here, we demonstrate continuous flow profiling and convection-regime identification (pump-driven forced convection vs. buoyancy-driven natural convection) using fiber-optic sensing methods. We used a combination of the Low-Frequency Distributed Acoustic Sensing (LF-DAS) approach, which measures axial strain-rate changes along a fiber, and Distributed Temperature Sensing (DTS) in a 4.1 km MD (Measured Depth) geothermal injection well within Munich, Germany.

During shut-in, LF-DAS reveals three persistent, depth-localized natural convection cells, characterized by distinct strain-rate patterns and coincident with rapid warming with depth, as observed in the DTS data. In quasi-steady-state injection, operationally occurring temperature changes as small as 10 mK/min in the injected fluid induce thermo-mechanical deformation along the fiber. These downward-propagating thermal fronts initially reflect pump-driven forced convection and enable flow profiling based on advective heat transport. From a depth of 3580 m MD, these fronts are blurred by the onset of buoyancy-driven natural convection. LF-DAS allows estimation of the plume-shedding frequency, plume height, travel distance, and velocity, all related to the temperature gradient measured with DTS. The accuracy of a threshold criterion for the onset of buoyancy-driven flow based on the temperature gradient is currently limited by the precision of the reference DTS measurement. Across all operational states, values range from 39 to 44 °C/km of true vertical depth.

These findings show that fiber-optic sensing can detect fluid-flow pathways, convection behavior, and regime changes without well intervention, thereby improving continuous monitoring and reservoir characterization for sustainable geothermal operation.

How to cite: Hart, J., Wollin, C., Andy, A., Ledig, T., Reinsch, T., and Krawczyk, C.: Low-Frequency Distributed Acoustic Sensing reveals transient flow and heat-transfer regimes during geothermal injection, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-16969, https://doi.org/10.5194/egusphere-egu26-16969, 2026.