Induced seismicity

We need to reach zero emissions by 2050 in order to meet the Paris Agreement goal of limiting temperature increase below 2.0 °C, but ideally below 1.5 °C. This objective will only be reached if several actions are undertaken simultaneously. Among the necessary actions, the International Energy Agency suggests that the subsurface can contribute with some 20 % of the total CO2 emissions reduction. This contribution comes mainly from geologic carbon storage, but also from geothermal energy and subsurface energy storage. The latter is particularly important because renewable energies do not produce energy in the moment that we need it and thus, we need to store energy when there is an excess of production and utilize the stored energy when the demand exceeds the production. Since batteries do not have enough capacity, energy storage in terms of hydrogen, compressed air energy storage (CAES) or aquifer thermal energy storage (ATES), will play a major role to efficiently store energy.

Induced seismicityThe downside of these geo-energies is that when we inject or extract fluids from the subsurface, we alter the pore pressure, temperature, stress state and geochemical composition of the geological formations, which may induce seismicity if fractures and/or faults are destabilized. The main geo-energy applications that may induce seismicity and thus, may benefit from the breakthroughs of this project are described here, including the potential harm to the environment, animals or plants:

Geothermal energy

This is a renewable energy source that provides energy without daily and seasonal fluctuations and is available worldwide. Geothermal energy projects usually inject and produce water from the same geological formation, creating a closed loop in which the pumped water is reinjected. Thus, if the system does not leak, there should not be any harm to the environment, animals or plants. The circulating fluid is usually water, but with a high concentration of dissolved ions because the high temperature of the geological formation enhances mineral dissolution. This high concentration of dissolved ions may lead to mineral precipitation when pressure and temperature drop in the pumping wells close to the surface, causing scaling of wells (e.g., Wanner et al., 2017). This problem highlights the importance of the geochemical composition of the circulating water in terms of operation and suggests that it would be advisable to put in place measures that prevent the circulating fluid to reach the environment in case of leakage along the pipes. As an alternative to water, it has been suggested to use carbon dioxide (CO2) as the working fluid to produce geothermal energy (Brown, 2000; Randolph and Saar, 2011). In that case, the pumped CO2 is also reinjected into the subsurface, so there are no hazards unless there is leakage. If a CO2 leakage occurs, there is no affection to the environment because CO2 is already present in the atmosphere. However, if CO2 is accumulated in depressions or in the basement of buildings, it could be fatal for humans and animals, because they could die by asphyxia. Thus, CO2 detectors should be placed in the surface along the pipes to detect any CO2 leakage and act quickly to stop it.

Geologic carbon storage

The aim of this application is to permanently store large amounts of CO2 in deep geological formations to mitigate climate change. If the storage is successful, CO2 will permanently remain deep underground. However, there is the risk of leakage of a small portion of the injected CO2 along wells, faults or across the caprock. CO2 leakage along wells can be detected by regularly monitoring the CO2 concentration at the wellhead. Such an event occurred in a well at the In Salah CO2 storage pilot project, in Algeria, and the leakage was immediately remediated (Ringrose et al., 2009). On the other hand, CO2 leakage across the caprock or through faults may lead to a diffusive leakage that can be more difficult to detect and remediate. Furthermore, CO2 does not necessarily need to reach the ground to produce harm to the environment, because if CO2 reaches freshwater aquifers, it may pollute drinking water resources because of water acidification and heavy metals release (Wang and Jaffe, 2004). CO2 will not penetrate caprocks because of their high entry pressure. Thus, the likelihood of CO2 leakage across caprocks, especially if they are thick or in multilayer sedimentary basins, is very low (Birkholzer et al., 2009). A more active debate has taken place about the possibility that induced seismicity may enhance fault permeability, leading to CO2 leakage (Zoback and Gorelick, 2012a, 2012b, 2015; Juanes et al., 2012; Vilarrasa and Carrera, 2015a, 2015b). Since the crystalline basement is critically stressed, but the sedimentary rocks where CO2 is planned to be injected are usually not (Vilarrasa and Carrera, 2015), induced earthquakes mostly nucleate in the crystalline basement below the storage formations, so permeability enhancement of faults occurs below and not above the storage formation (Verdon, 2014). Furthermore, faults in sedimentary basins are highly heterogeneous because they cross multiple aquifer-caprock sequences. This heterogeneity hinders upwards CO2 flow in case of CO2 reaching a fault (Rinaldi et al., 2014). Yet, monitoring and interpretation of the measured data must be performed for the prompt detection of CO2 leakage and its remediation (Zeidouni and Pooladi-Darvish, 2012).

Compressed Air Energy Storage (CAES)

This geo-energy application consists in injecting air at high pressure in an aquifer when there is excess of energy production from renewable sources, and pumping and recovering energy when the demand is higher than the production from renewable sources. Since the injected fluid is air, this application poses no hazards to the environment, animals or plants. Nonetheless, the water of the aquifers where air is injected should not have any potential use because the oxygen of the injected air may alter the geochemistry of the aquifer.

Natural gas storage

Natural gas storage is routinely performed for strategic reasons to ensure the gas supply in periods of high demand. The injected gas is recovered afterwards. Care should be taken in avoiding any leakage because methane is flammable.

Since induced seismicity is usually associated with hydraulic fracturing, we devote some lines to explain this geo-engineering application:

Hydraulic fracture techniques

Hydraulic fracturing consists in injecting a fluid at such high pressure that the minimum effective stress equals the tensile strength of the rock, generating a tensile fracture perpendicular to the direction of the minimum effective stress. Thus, hydraulic fracturing is performed to enhance the permeability of low permeable rock. It can be used for well stimulation in geothermal energy, but its most widely known application is shale gas exploitation. The injected fluid is usually water, but it has also been proposed to use CO2 (Middleton et al., 2015). The shale gas industry usually adds additives, which may be hazardous for the environment, to water in order to improve the performance of the fracturing operations. In addition to these additives, the backflow that occurs after hydraulic fracture operations becomes radioactive after being in contact with the radionuclides present in the shale that is being hydraulically fractured. Thus, the backflow of hydraulic fracturing operations must be managed with extreme care. Regarding induced seismicity, hydraulic fracturing generates microseismic events of such low magnitude that they cannot be felt on the ground surface. In rare cases, a generated hydraulic fracture has intersected a fault, pressurizing it, which has led to its reactivation and the occurrence of a felt earthquake on surface. But the felt seismicity is not directly induced by hydraulic fracturing. Nonetheless, it should be highlighted that the environmental risks related to the chemical composition of the backwater and the risk of induced seismicity are completely different. Indeed, even though the risks associated with induced seismicity are low in hydraulic fracturing, the environmental risks related to such operations such be assessed site specifically to decide on the feasibility of such projects.

 

 

REFERENCES

Birkholzer, J. T., Zhou, Q., & Tsang, C. F. (2009). Large-scale impact of CO2 storage in deep saline aquifers: A sensitivity study on pressure response in stratified systems. International Journal of Greenhouse Gas Control, 3(2), 181-194.

Brown, D. W. (2000). A hot dry rock geothermal energy concept utilizing supercritical CO2 instead of water. In Proceedings of the twenty-fifth workshop on geothermal reservoir engineering, Stanford University (pp. 233-238).

Juanes, R., Hager, B. H., & Herzog, H. J. (2012). No geologic evidence that seismicity causes fault leakage that would render large-scale carbon capture and storage unsuccessful. Proceedings of the National Academy of Sciences, 109(52), E3623-E3623.

Middleton, R. S., Carey, J. W., Currier, R. P., Hyman, J. D., Kang, Q., Karra, S., Jimenez-Martinez, J., Porter, M. L., & Viswanathan, H. S. (2015). Shale gas and non-aqueous fracturing fluids: Opportunities and challenges for supercritical CO2. Applied Energy, 147, 500-509.

Randolph, J. B., & Saar, M. O. (2011). Combining geothermal energy capture with geologic carbon dioxide sequestration. Geophysical Research Letters, 38(10), L10401.

Rinaldi, A. P., Jeanne, P., Rutqvist, J., Cappa, F., & Guglielmi, Y. (2014). Effects of fault‐zone architecture on earthquake magnitude and gas leakage related to CO2 injection in a multi‐layered sedimentary system. Greenhouse Gases: Science and Technology, 4(1), 99-120.

Ringrose, P., Atbi, M., Mason, D., Espinassous, M., Myhrer, Ø., Iding, M., Mathieson, A., & Wright, I. (2009). Plume development around well KB-502 at the In Salah CO2 storage site. First Break, 27(1).

Verdon, J. P. (2014). Significance for secure CO2 storage of earthquakes induced by fluid injection. Environmental Research Letters, 9(6), 064022.

Vilarrasa, V., & Carrera, J. (2015a). Geologic carbon storage is unlikely to trigger large earthquakes and reactivate faults through which CO2 could leak. Proceedings of the National Academy of Sciences, 201413284.

Vilarrasa, V., & Carrera, J. (2015b). Reply to Zoback and Gorelick: Geologic carbon storage remains a safe strategy to significantly reduce CO2 emissions. Proceedings of the National Academy of Sciences, 112(33), E4511-E4511.

Wang, S., & Jaffe, P. R. (2004). Dissolution of a mineral phase in potable aquifers due to CO2 releases from deep formations; effect of dissolution kinetics. Energy Conversion and Management, 45(18-19), 2833-2848.

Wanner, C., Eichinger, F., Jahrfeld, T., & Diamond, L. W. (2017). Causes of abundant calcite scaling in geothermal wells in the Bavarian Molasse Basin, Southern Germany. Geothermics, 70, 324-338.

Zeidouni, M., & Pooladi-Darvish, M. (2012). Leakage characterization through above-zone pressure monitoring: 2—Design considerations with application to CO2 storage in saline aquifers. Journal of Petroleum Science and Engineering, 98, 69-82.

Zoback, M. D., & Gorelick, S. M. (2012a). Earthquake triggering and large-scale geologic storage of carbon dioxide. Proceedings of the National Academy of Sciences, 109(26), 10164-10168.

Zoback, M. D., & Gorelick, S. M. (2012b). Reply to Juanes et al.: Evidence that earthquake triggering could render long-term carbon storage unsuccessful in many regions. Proceedings of the National Academy of Sciences, 109(52), E3624-E3624.

Zoback, M. D., & Gorelick, S. M. (2015). To prevent earthquake triggering, pressure changes due to CO2 injection need to be limited. Proceedings of the National Academy of Sciences, 112(33), E4510-E4510.