EGU25-110, updated on 14 Mar 2025
https://doi.org/10.5194/egusphere-egu25-110
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Thursday, 01 May, 17:35–17:45 (CEST)
 
Room -2.31
The bound growth of induced earthquakes could de-risk hydraulic fracturing
Ryan Schultz1, Federica Lanza1, Ben Dyer2, Dimitrios Karvounis2, Remi Fiori2, Peidong Shi1, Vanille Ritz1, Linus Villiger1, Peter Meier2, and Stefan Wiemer1
Ryan Schultz et al.
  • 1ETH Zürich, Swiss Seismological Service (SED), Switzerland
  • 2Geo-Energie Suisse, Zürich, Switzerland

The world's energy supply depends critically on hydraulic fracturing (HF): HF operations utilize microseismicity to enhance subsurface permeability, so that hydrocarbons or geothermal heat can be extracted economically.  Unfortunately, HF also has the potential to induce larger earthquakes – with some projects being prematurely terminated because of perceived earthquake risks.  To de-risk HF, we use a suite of novel statistical tests called CAP-tests to discern if some physical process has restricted the growth of earthquake magnitudes.  We show that all stage stimulations at UK PNR-1z indicate bound fracture growth, implying a more controllable operation.  Contrastingly, stimulations at Utah FORGE and UK PNR-2 sequentially transitioned into unbound fault reactivation.  The problematic stages (that ultimately led to the termination of PNR-2) are clearly distinguishable using CAP-tests.  We postulate that our research can discriminate fracture stimulation from fault reactivation, contributing to the de-risking of HF operations worldwide.

How to cite: Schultz, R., Lanza, F., Dyer, B., Karvounis, D., Fiori, R., Shi, P., Ritz, V., Villiger, L., Meier, P., and Wiemer, S.: The bound growth of induced earthquakes could de-risk hydraulic fracturing, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-110, https://doi.org/10.5194/egusphere-egu25-110, 2025.