the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
| 11 Dec 2025
Assessment of seismicity and risk from gas injection in the Groningen gas field
Abstract. Production of natural gas from the Groningen gas field in the Netherlands has led to earthquakes, the societal impact of which has ultimately led to the decision to cease all gas production from the field starting October 2023. Seismicity is expected to continue for some time, even after production has stopped, at least in part because of the existing pressure gradients in the field and the time that it will take for gas to re-distribute and pressure to equilibrate. We investigate the possibility to reduce the seismicity by means of gas injection. We employ a dedicated model chain previously developed to model gas production, induced seismicity, and associated hazard and risk. The model chain was adapted to support modelling of pressure increases associated with gas injection, and to account for the effects of reservoir cooling when relatively cold gas is injected. Several injection scenarios are considered that are based on realistically feasible total injection gas volumes. Additional scenarios are designed to provide useful insight into fundamental mechanisms. The scenarios are compared to a no-injection reference case to be able to identify and quantify beneficial effects. The results indicate that reductions in seismicity can be achieved in all scenarios and that these reductions could be substantial also for relatively modest volumes of injection gas. The results also show that benefits may be lost if injection is stopped before reservoir-wide equilibration has been achieved. We discuss also some limitations of the model chain and highlight possibilities to deploy more targeted injection schemes.
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Status: final response (author comments only)
- RC1: 'Comment on egusphere-2025-6007', Anonymous Referee #1, 14 Mar 2026
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RC2: 'Comment on egusphere-2025-6007', Anonymous Referee #2, 17 Mar 2026
The study explores whether injecting gas back into the Groningen gas field in the Netherlands could reduce earthquake activity. Using an adapted modeling framework, TNO Model Chain for Groningen, that accounts for pressure increases and cooling effects from injected gas, the study tested several hypothetical injection scenarios and compared them to a no-injection case. The results suggest that gas injection can significantly reduce seismicity, though benefits may diminish if injection stops before pressure equilibrium is fully restored across the reservoir. Overall, this study is well-designed and comprehensive, and the findings are meaningful for earthquake risk management for gas production areas. However, I still have several comments and suggestions as follows.
1) Figure 1: It is suggested to discuss how the model and data uncertainties/errors propagate through the workflow.
2) In the Methodology section, how was the grid size of the models determined, and how would the different spatial resolution of the model grid affect the simulated results?
3) Equations 2.a and 2.b: What is the difference between the subscripts “H” and “h”?
4) Equation (5) may not be correct because the Young’s modulus was not included.
5) Figure 2 and other maps: It is suggested to add a north arrow and a scale bar to the maps, and it is also better to add units to the color bars of the simulated results.
6) Line 322: Could you justify if the calibrated parameters based on historical data are still applicable to the future scenarios?
7) Line 497: It is suggested to clearly define the “personal risk” or “seismic risk” in the Methodology section. Is the probability of property loss also considered? Remove the repeated explanations in Lines 521-522.
8) Line 25: A typo, change “The are two main reasons for this” to “There are…”
9) Lines 130 and 492: Correct the punctuation marks such as “,”.
10) Line 149 and Table 1: Please keep the notation of the variables (e.g., P_p) or scenarios (e.g., LO-10ZB or LO_10ZB) consistent throughout the manuscript.
11) Lines 203, 209, and 257: “Table 2” should be “Table A2”.
12) Lines 238-239: Correct the format of the units, cubic meters.
13) Section 4.1: Use either “MPa” or “bar” throughout the discussion.
14) Line 333: “Fig. 7 to 13” or “Fig. 6 to 13”?Citation: https://doi.org/10.5194/egusphere-2025-6007-RC2
Data sets
Inputdata for Nitrogen Injection study Groningen gas field Sander Osinga and Olwijn Leeuwenburgh https://doi.org/10.5281/zenodo.17232637
Model code and software
Seismic source model Sander Osinga et al. https://github.com/TNO/SHRA-Groningen-seismic-source-model
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This manuscript investigates the potential mitigation of induced seismicity in the Groningen gas field through nitrogen injection into the depleted reservoir following the cessation of gas production. The study employs the existing TNO modelling framework, integrating reservoir flow simulations, a seismic source model (SSM), ground motion modelling, and seismic hazard and risk assessment to evaluate the potential impact of several injection scenarios on seismicity and associated societal risk.
The topic is relevant to NHESS and timely. Although gas production in the Groningen field ceased in October 2023, seismicity is expected to persist due to delayed reservoir compaction and ongoing stress redistribution. Exploring potential mitigation strategies for post-production seismicity is therefore scientifically and societally important. The integrated modelling chain used in this study provides a structured framework to link reservoir pressure evolution to seismicity forecasts and seismic risk metrics.
The manuscript is generally well written and logically structured. The scenario-based analysis provides useful insight into how reservoir repressurization through nitrogen injection may influence the temporal evolution of seismicity and associated seismic risk. The results indicate that nitrogen injection may reduce the predicted seismicity rate and corresponding risk metrics compared to a reference case without injection.
Several modelling assumptions and simplifications are already acknowledged and discussed by the authors in the discussion section. Since these limitations are transparently presented in the manuscript, it is not necessary to reiterate them in this review. My main comment concerns the validation of the modelling framework against historical observations, which would help strengthen confidence in the predictive capability of the model.
The seismic source model (SSM) described in Section 2.2 is a central component of the modelling framework, as it converts reservoir pressure changes into forecasts of seismic activity. The manuscript states that the SSM has been calibrated against historical seismicity, and the comparison between observed and simulated number of events per year appears to show a good agreement (e.g., the green shaded part in Figures 6–13). However, it is less clear how well the calibrated SSM reproduces other important characteristics of the historical seismicity. In particular, the manuscript does not appear to show comparisons of the spatial distribution of events between observed and simulated seismicity. Since fault geometry and spatial stress redistribution play an important role in induced seismicity, demonstrating that the model reproduces the spatial pattern of seismicity would strengthen confidence in the calibration.
In addition, it would be useful to clarify how the model represents larger events, particularly the Huizinge earthquake (M3.6 in 2012), which represents the largest recorded event in the Groningen field. It is not clear from the manuscript whether events of this magnitude can be reproduced by the calibrated SSM, or whether the calibration mainly focuses on reproducing the overall seismicity rate. Demonstrating whether events with magnitude larger than 3 can be reproduced within the calibrated SSM would be helpful for assessing the model’s capability to represent the historical seismicity.
Furthermore, since the seismicity in Groningen is closely related to reservoir compaction and resulting surface subsidence, it would also be useful to show how well the reservoir model reproduces the historical subsidence evolution observed in the Groningen field. Subsidence measurements provide an important constraint on reservoir compaction behaviour and therefore indirectly on the stress changes driving seismicity. A brief comparison between observed and simulated subsidence evolution would therefore further strengthen the validation of the modelling framework.
Overall, a figure or additional comparison showing (i) spatial seismicity patterns, (ii) magnitude distribution including larger events such as the Huizinge earthquake, and (iii) subsidence history matching would provide a more comprehensive validation of the modelling framework against historical observations.