Stanford researchers find similar characteristics in human-induced and natural earthquakes

New research shows manmade and naturally occurring earthquakes in the central U.S. share the same characteristics, information that will help scientists predict and mitigate damage from future earthquakes.

Whether an earthquake occurs naturally or as a result of unconventional oil and gas recovery, the destructive power is the same, according to a new study appearing in Science Advances Aug. 2. The research concludes that human-induced and naturally occurring earthquakes in the central U.S. share the same shaking potential and can thus cause similar damage.

A fallen brick chimney of a house in Oklahoma after a magnitude 5.6 earthquake likely induced by injection into deep disposal wells in the Wilzetta North field; Nov. 6, 2011.

A magnitude 5.6 earthquake likely induced by injection into deep disposal wells in the Wilzetta North field caused house damage in central Oklahoma on Nov. 6, 2011. Research conducted by Stanford scientists shows human-induced and naturally occurring earthquakes in the central U.S. share the same shaking potential and can thus cause similar damage. (Image credit: Brian Sherrod, USGS)

The finding contradicts previous observations suggesting that induced earthquakes exhibit weaker shaking than natural ones. The work could help scientists make predictions about future earthquakes and mitigate their potential damage.

“People have been debating the strength of induced earthquakes for decades – our study resolves this question,” said co-author William Ellsworth, a professor in the Geophysics Department at Stanford’s School of Earth, Energy & Environmental Sciences and co-director of the Stanford Center for Induced and Triggered Seismicity (SCITS). “Now we can begin to reduce our uncertainty about how hard induced earthquakes shake the ground, and that should lead to more accurate estimates of the risks these earthquakes pose to society going forward.”

Induced quakes

Earthquakes in the central U.S. have increased over the past 10 years due to the expansion of unconventional oil and gas operations that discard wastewater by injecting it into the ground. About 3 million people in Oklahoma and southern Kansas live with an increased risk of experiencing induced earthquakes.

“The stress that is released by the earthquakes is there already – by injecting water, you’re just speeding up the process,” said co-author Gregory Beroza, the Wayne Loel Professor in geophysics at Stanford Earth and co-director of SCITS. “This research sort of simplifies things, and shows that we can use our understanding of all earthquakes for more effective mitigation.”

Oklahoma experienced its largest seismic event in 2016 when three large earthquakes measuring greater than magnitude 5.0 caused significant damage to the area. Since the beginning of 2017, the number of earthquakes magnitude 3.0 and greater has fallen, according to the Oklahoma Geological Survey. That drop is partly due to new regulations to limit wastewater injection that came out of research into induced earthquakes.

Stress drop

To test the destructive power of an earthquake, researchers measured the force driving tectonic plates to slip, known as stress drop – measured by the difference between a fault’s stress before and after an earthquake. The team analyzed seismic data from 39 manmade and natural earthquakes ranging from magnitude 3.3 to 5.8 in the central U.S. and eastern North America. After accounting for factors such as the type of fault slip and earthquake depth, results show the stress drops of induced and natural earthquakes in the central U.S. share the same characteristics.

A second finding of the research shows that most earthquakes in the eastern U.S. and Canada exhibit stronger shaking potential because they occur on what’s known as reverse faults. These types of earthquakes are typically associated with mountain building and tend to exhibit more shaking than those that occur in the central U.S. and California. Although the risk for naturally occurring earthquakes is low, the large populations and fragile infrastructure in this region make it vulnerable when earthquakes do occur.

The team also analyzed how deep the earthquakes occur underground and concluded that as quakes occur deeper, the rocks become stronger and the stress drop, or force behind the earthquakes, becomes more powerful.

“Both of these conclusions give us new predictive tools to be able to forecast what the ground motions might be in future earthquakes,” Ellsworth said. “The depth of the quake is also going to be important, and that needs to be considered as people begin to revise these ground-motion models that describe how strong the shaking will be.”

The scientists said that the types of rocks being exploited by unconventional oil and gas recovery in the U.S. and Canada can be found all over the world, making the results of this study widely applicable.

“As we can learn better practices, we can help ensure that the hazards induced earthquakes pose can be reduced in other parts of the world as well,” Ellsworth said.

Additional authors include lead author Yihe Huang, a former postdoctoral researcher at Stanford and now an assistant professor at the University of Michigan. The study was supported by the Stanford Center for Induced and Triggered Seismicity.

Media Contacts

Gregory Beroza, School of Earth, Energy & Environmental Sciences: (650) 723-4958 (office), (650) 319-5636 (cell), beroza@stanford.edu

Danielle T. Tucker, School of Earth, Energy & Environmental Sciences: (650) 497-9541, dttucker@stanford.edu