Abstract:This paper presents a timely and detailed study of significant injection-induced seismicity recently observed in the Sichuan Basin, China, where shale-gas hydraulic fracturing has been initiated and the aggressive production of shale gas is planned for the coming years. Multiple lines of evidence, including an epidemic-type aftershock sequence model, relocated hypocenters, the mechanisms of 13 large events (M
W > 3.5), and numerically calculated Coulomb failure stress results, convincingly suggest that a serie… Show more
“…[26][27][28][29] Engineering monitoring in this study proved this point, the maximal moment magnitude Some scholars pointed out that West Canadian reservoirs and Sichuan Basin in China experienced anomalous activity during multistage fracturing, the microseismic moment magnitude was more than 4.…”
Casing shear deformation has become a prominent problem in the process of completion in shale gas wells. It was believed that the slide of strike‐slip fault induced by multistage fracturing was the main reason. This paper presented a new numerical investigation for evaluating the casing inner diameter after strike‐slip fault sliding based on the microseismic data. A 3D finite element model, considering the mechanical anisotropy of shale and heat‐fluid‐solid coupling effect during multistage fracturing, was developed to calculate the variation of casing inner diameter after fault sliding under different engineering and geological conditions. The calculation result was verified by comparison with the measurement result of the multi‐finger caliper survey. Sensitivity analysis was carried out and the results showed that decreasing the sliding distance, maintaining high pressure, increasing the casing thickness, and increasing the elasticity modulus and decreasing the Poisson ratio of cement sheath were beneficial to protect the casing integrity. Finally, the engineering verification demonstrated that the numerical method has an accuracy up to 85.9%. Numerical model in this study was expected to provide a better understanding of casing shear deformation and an evaluation method of casing inner diameter after fault sliding during multistage fracturing in shale gas wells.
“…[26][27][28][29] Engineering monitoring in this study proved this point, the maximal moment magnitude Some scholars pointed out that West Canadian reservoirs and Sichuan Basin in China experienced anomalous activity during multistage fracturing, the microseismic moment magnitude was more than 4.…”
Casing shear deformation has become a prominent problem in the process of completion in shale gas wells. It was believed that the slide of strike‐slip fault induced by multistage fracturing was the main reason. This paper presented a new numerical investigation for evaluating the casing inner diameter after strike‐slip fault sliding based on the microseismic data. A 3D finite element model, considering the mechanical anisotropy of shale and heat‐fluid‐solid coupling effect during multistage fracturing, was developed to calculate the variation of casing inner diameter after fault sliding under different engineering and geological conditions. The calculation result was verified by comparison with the measurement result of the multi‐finger caliper survey. Sensitivity analysis was carried out and the results showed that decreasing the sliding distance, maintaining high pressure, increasing the casing thickness, and increasing the elasticity modulus and decreasing the Poisson ratio of cement sheath were beneficial to protect the casing integrity. Finally, the engineering verification demonstrated that the numerical method has an accuracy up to 85.9%. Numerical model in this study was expected to provide a better understanding of casing shear deformation and an evaluation method of casing inner diameter after fault sliding during multistage fracturing in shale gas wells.
“…Previous studies have reported some shallow earthquakes in the southern Sichuan Basin in the vicinity of the oil and gas wells, mostly triggered by hydraulic fracturing (e.g., Lei et al, 2008Lei et al, , 2017. However, the closest oil and gas wells with associated induced seismicity are located at least 40 km away from the Dianjiang earthquake.…”
Section: Discussionmentioning
confidence: 99%
“…The basement faults are hidden in the crystal basement (>5 km) and show minor activity . Based on the Chongqing Seismic Network catalog (1990 to 2018), there was no other M > 3.5 event within 100 km of the Dianjiang earthquake, indicating a low background seismic rate, although many shallow earthquakes in the Sichuan Basin have been linked with wastewater injection (e.g., Lei et al, 2008) and hydraulic fracturing in shale gas fields (e.g., Lei et al, 2017;Figure 1a). Based on the Chongqing Seismic Network catalog (1990 to 2018), there was no other M > 3.5 event within 100 km of the Dianjiang earthquake, indicating a low background seismic rate, although many shallow earthquakes in the Sichuan Basin have been linked with wastewater injection (e.g., Lei et al, 2008) and hydraulic fracturing in shale gas fields (e.g., Lei et al, 2017;Figure 1a).…”
Triggered or induced earthquakes have been widely reported as resulting from various human activities, yet seismicity triggered by small-scale infrastructure construction is rare. Here, we report on an investigation of an extremely shallow M w 4.1 earthquake which occurred on 11 August 2016 in the Sichuan Basin (China), a region with historically low seismicity. Our seismic waveform analyses indicate an almost pure thrust focal mechanism at a centroid depth of~1 km. Furthermore, 18 Sentinel-1 synthetic aperture radar interferograms, stacked to obtain subcentimeter accuracy, reveal up to 3 cm line-of-sight deformation which overlaps with an automotive testing site constructed in 2014. Removal of 10 m of a surface rock layer during the construction may have produced an unloading effect and resulted in up to 0.11 MPa Coulomb stress changes on a blind fault, larger than the 0.01 MPa threshold typically invoked in studies of tectonic earthquakes. However, the delayed triggering still requires further investigation.
Plain Language SummaryWhile induced earthquakes in the shallow part of the crust have been observed globally, a remaining knowledge gap is whether small-scale infrastructure construction can trigger earthquakes or not. We investigate these questions on an extremely shallow M w 4.1 earthquake in the eastern Sichuan Basin (China). To determine earthquake source parameters, we combine seismological data with satellite imaging. We find this thrust event ruptured at the depth of~1 km, located just beneath an automotive testing site constructed in 2014. Crucially, we note the testing site construction involved removal of a large volume of surface rock. We further analyze the stress changes produced by the unloading of the surface rock. We find a possible triggering relationship between the infrastructure construction and the occurrence of this shallow earthquake. Our results thus shed new light on the causes of shallow earthquakes associated with small-scale infrastructure construction.
“…Individual case examples of HF‐induced seismicity have been now be identified in Alberta (e.g., Wang et al, ), Arkansas (Yoon et al, ), British Columbia (e.g., B.C. Oil and Gas Commission, ), California (Kanamori & Hauksson, ), China (e.g., Lei et al, ), England (Clarke et al, ), Ohio (e.g., Skoumal et al, ), Oklahoma (e.g., Holland, ), Pennsylvania (Skoumal et al, ), and West Virginia (Skoumal et al, ).…”
Section: Introductionmentioning
confidence: 99%
“…This interpretation was based on the few documented cases of HF‐induced seismicity, with the cases consistent of small‐magnitude events. Since these interpretations were made, larger‐magnitude earthquakes that have been attributed to hydraulic fracturing have occurred, including the 2015 M 4.6 earthquake in British Columbia, Canada (Atkinson et al, ; Mahani et al, ), and the 2016 M 4.7 earthquake in the Sichuan Basin, China (Lei et al, ). Additionally, while the number of cases identified prior to these studies was limited (Clarke et al, ; Darold et al, ; Friberg et al, ; Holland, ), more recent studies have found a higher prevalence of HF‐induced seismicity than would have been previously expected (Atkinson et al, ; Skoumal et al, ).…”
Wastewater disposal is generally accepted to be the primary cause of the increased seismicity rate in Oklahoma within the past decade, but no statewide analysis has investigated the contribution of hydraulic fracturing (HF) to the observed seismicity or the seismic hazard. Utilizing an enhanced seismicity catalog generated with multistation template matching from 2010 to 2016 and all available hydraulic fracturing information, we identified 274 HF wells that are spatiotemporally correlated with bursts of seismicity. The majority of HF‐induced seismicity cases occurred in the SCOOP/STACK plays, but we also identified prominent cases in the Arkoma Basin and some more complex potential cases along the edge of the Anadarko Platform. For HF treatments where we have access to injection parameters, modeling suggests that poroelastic stresses are likely responsible for seismicity, but we cannot rule out direct pore pressure effects as a contributing factor. In all of the 16 regions we identified, ≥75% of the seismicity correlated with reported HF wells. In some regions, >95% of seismicity correlated with HF wells and >50% of the HF wells correlated with seismicity. Overall, we found ~700 HF‐induced earthquakes with M ≥ 2.0, including 12 events with M 3.0–3.5. These findings suggest state regulations implemented in 2018 that require operators in the SCOOP/STACK plays to take action if a M > 2 earthquake could have a significant impact on future operations.
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