New research suggests naturally occurring earthquakes and those caused by unconventional oil and gas recovery in the central US share the same shaking potential and can thus cause similar damage.
“People have been debating the strength of induced earthquakes for decades—our study resolves this question…”
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,” says coauthor William Ellsworth, a professor in the geophysics department at Stanford University’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,” Ellsworth says.
Earthquakes in the central United States 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,” says coauthor Gregory Beroza, a professor of geophysics and codirector of SCITS.
“This research sort of simplifies things, and shows that we can use our understanding of all earthquakes for more effective mitigation,” he says.
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.
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 US 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 US share the same characteristics.
A second finding of the research shows that most earthquakes in the eastern US 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 US 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 says.
“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,” he says.
The scientists say that the types of rocks being exploited by unconventional oil and gas recovery in the United States 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 says.
The study appears in Science Advances. The study was supported by the Stanford Center for Induced and Triggered Seismicity.
Source: Stanford University
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