Oklahoma’s coordinated response to more than a decade of elevated seismicity

Author:

Murray* Kyle E.1,Brooks Colin2,Walter Jacob I.3,Ogwari Paul O.3

Affiliation:

1. Murray GeoConsulting, LLC, Norman, Oklahoma 73072, USA

2. Induced Seismicity Department, Oklahoma Corporation Commission, 2101 N. Lincoln Boulevard, Oklahoma City, Oklahoma 73105, USA

3. Oklahoma Geological Survey, University of Oklahoma, 100 East Boyd Street, N-131 Sarkeys Energy Center, Norman, Oklahoma 73019, USA

Abstract

ABSTRACT In the period between 1961 and 2008, Oklahoma, USA, averaged about two M ≥3.0 earthquakes per year, with no damage to any built infrastructure. A substantial increase in seismic activity was first observed in 2009, when there were 20 M ≥3.0 earthquakes, and activity peaked in 2015, when over 900 M ≥3.0 earthquakes occurred. Because of the unprecedented increase in seismic activity, the governor’s office of Oklahoma formed a Coordinating Council of researchers, regulators, industry, and other stakeholders in 2015. The Coordinating Council was led by the Secretary of Energy and Environment and charged with understanding and attempting to mitigate (that is, reduce, if not eliminate) induced seismicity and potential impacts. Major outcomes of the coordinated efforts included delineation of an area of interest (AOI) for seismicity in Oklahoma, modifications to underground injection control (UIC) well completion depths and injection rates into UIC wells in the AOI, development of the Oklahoma Well and Seismic Monitoring (OWSM) application used for regulatory oversight and action, modified well completion protocols, a more robust seismic network, and numerous scientific investigations and publications. Because of concerted efforts between regulators and industry, disposal into the Arbuckle Group, the primary zone for wastewater disposal, in the AOI was reduced by more than 50% though oil production continued to increase. Seismic activity decreased over a 6 yr period with 619, 302, 195, 65, 39, and 29 M ≥3.0 earthquakes occurring in 2016, 2017, 2018, 2019, 2020, and 2021, respectively. At the time of latest updates to this chapter (16 October 2022), there have been 12 M ≥3.0 earthquakes and one M ≥4.0 earthquake, so the projected total of M ≥3.0 earthquakes in 2022 is 17. Using these metrics, the coordinated efforts of Oklahoma stakeholders appear to have successfully reduced seismicity with respect to frequency and number in the range of minor but often felt (M 3.0–3.9), light (M 4.0–4.9), and moderate (M 5.0–5.9) earthquakes. So, the Oklahoma case provides examples of how stakeholder action diminished seismic hazards and how similar actions could be used to reduce induced seismicity in other areas where injections occur.

Publisher

Geological Society of America

Reference43 articles.

1. Teleseismic waves reveal anisotropic poroelastic response of wastewater disposal reservoir;Barbour,;Earth and Planetary Physics,2021

2. The effects of varying injection rates in Osage County, Oklahoma, on the 2016 Mw 5.8 Pawnee earthquake;Barbour,;Seismological Research Letters,2017

3. Leakage and increasing fluid pressure detected in Oklahoma’s wastewater disposal reservoir;Barbour,;Journal of Geophysical Research–Solid Earth,2019

4. Generalized Contours: Top of the Arbuckle Group;Campbell,;Oklahoma Geological Survey Open-File Report (OF1-2020),2020

5. Carrell,J.R., 2014, Field-Scale Hydrogeologic Modeling of Water Injection into the Arbuckle Zone of the Midcontinent [M.S. thesis]: Norman, Oklahoma, University of Oklahoma, 90 p.

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