Reply to Comment by Peterie Et Al. on "Accelerated Fill‐Up of the Arbuckle Group Aquifer and Links to U.S. Midcontinent Seismicity". Issue 12 (7th December 2020)
- Record Type:
- Journal Article
- Title:
- Reply to Comment by Peterie Et Al. on "Accelerated Fill‐Up of the Arbuckle Group Aquifer and Links to U.S. Midcontinent Seismicity". Issue 12 (7th December 2020)
- Main Title:
- Reply to Comment by Peterie Et Al. on "Accelerated Fill‐Up of the Arbuckle Group Aquifer and Links to U.S. Midcontinent Seismicity"
- Authors:
- Ansari, Esmail
Bidgoli, Tandis S. - Abstract:
- Abstract: Peterie et al. question one observation in our paper: associating pressure increases to injection volumes at distances of up to 25 km from an injection well. In this reply, we show that the comment misunderstands our analysis and the evidence that led to this conclusion. We also show that gauge‐depth‐corrected pressures, used by the authors to produce statewide pressure maps, are discrepant with the static fluid level data, provided in our original compilation and analysis. The discrepancies are a result of the pressure correction method employed, which naïvely substitutes formation pressure for bottomhole pressure to calculate wellbore fluid density. Their linearly interpolated pressure maps, based on sparse data, contain interpolation and extrapolation artifacts that contradict injection trends in the state, the Theis solution, and the superposition principle. We reiterate that pressure and static fluid level increases in Class I wells existed prior to 2013, most notably in central Kansas, where recent earthquakes are cited in the comment as evidence of a pressure plume emanating from the Kansas‐Oklahoma border, 90 km away. We show that the space‐time pattern of seismicity in this area is inconsistent with a northward propagating pressure plume and, instead, seismicity appears to be centered on and near a cluster of high‐rate injection wells, two of which are among the highest rate wells in the state. These observations, along with recent M4 + earthquakes duringAbstract: Peterie et al. question one observation in our paper: associating pressure increases to injection volumes at distances of up to 25 km from an injection well. In this reply, we show that the comment misunderstands our analysis and the evidence that led to this conclusion. We also show that gauge‐depth‐corrected pressures, used by the authors to produce statewide pressure maps, are discrepant with the static fluid level data, provided in our original compilation and analysis. The discrepancies are a result of the pressure correction method employed, which naïvely substitutes formation pressure for bottomhole pressure to calculate wellbore fluid density. Their linearly interpolated pressure maps, based on sparse data, contain interpolation and extrapolation artifacts that contradict injection trends in the state, the Theis solution, and the superposition principle. We reiterate that pressure and static fluid level increases in Class I wells existed prior to 2013, most notably in central Kansas, where recent earthquakes are cited in the comment as evidence of a pressure plume emanating from the Kansas‐Oklahoma border, 90 km away. We show that the space‐time pattern of seismicity in this area is inconsistent with a northward propagating pressure plume and, instead, seismicity appears to be centered on and near a cluster of high‐rate injection wells, two of which are among the highest rate wells in the state. These observations, along with recent M4 + earthquakes during continued decreases in wastewater injection in southern Kansas and northern Oklahoma, question the usefulness of the comment for understanding and managing societally significant earthquakes. Key Points: The comment misunderstands the methods and key points in Ansari et al. (2019, https://doi.org/10.1029/2018JB016926 ) Gauge‐depth‐corrected pressures supplied in the comment are incorrect and discrepant with static fluid level data Pressure and seismicity increases in central Kansas are readily explained by local injection and do not require far‐field pressure diffusion … (more)
- Is Part Of:
- Journal of geophysical research. Volume 125:Issue 12(2020)
- Journal:
- Journal of geophysical research
- Issue:
- Volume 125:Issue 12(2020)
- Issue Display:
- Volume 125, Issue 12 (2020)
- Year:
- 2020
- Volume:
- 125
- Issue:
- 12
- Issue Sort Value:
- 2020-0125-0012-0000
- Page Start:
- n/a
- Page End:
- n/a
- Publication Date:
- 2020-12-07
- Subjects:
- induced seismicity -- Kansas and Oklahoma earthquakes -- waste water injection -- pressure diffusion -- poroelasticity
Geomagnetism -- Periodicals
Geochemistry -- Periodicals
Geophysics -- Periodicals
Earth sciences -- Periodicals
551.1 - Journal URLs:
- http://onlinelibrary.wiley.com/journal/10.1002/(ISSN)2169-9356 ↗
http://onlinelibrary.wiley.com/ ↗ - DOI:
- 10.1029/2019JB019275 ↗
- Languages:
- English
- ISSNs:
- 2169-9313
- Deposit Type:
- Legaldeposit
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- Available online (eLD content is only available in our Reading Rooms) ↗
- Physical Locations:
- British Library DSC - 4995.009000
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British Library HMNTS - ELD Digital store - Ingest File:
- 24363.xml