A new study finds pumping fracking wastewater deep into the ground is a leading cause of the flurry of man-made earthquakes that have rattled Oklahoma. Scientists say a major seismic trigger is how deep _ not just how much _ wastewater is injected. Oklahoma has been hit with thousands of quakes in recent years including the magnitude 5.8 Pawnee quake in 2016. The findings were published Thursday in the journal Science.
, FILE - In this Nov. 6, 2011 file photo, Chad Devereaux examines bricks that fell from three sides of his in-laws home in Sparks, Okla., after two earthquakes hit the area in less than 24 hours. According to a study released on Thursday, Feb. 1, 2018, pumping energy drilling wastewater deep and nearer fault lines is a leading cause in much of the thousands of man-made earthquakes that have hit Oklahoma in recent years. (AP Photo/Sue Ogrocki, File)
01 of February 2018 19:21:54
WASHINGTON (AP) — A new study finds that a major trigger of man-made earthquakes rattling Oklahoma is how deep — not just how much — fracking wastewater is injected into the ground.
Scientists analyzed more than 10,000 wastewater injection wells where 96 billion gallons of fluid — leftover from hydraulic fracturing — are pumped yearly. The amount of wastewater injected and the depth are key to understanding the quake outbreak since 2009, they reported in Thursday's journal Science . The quakes included a damaging magnitude 5.8 in 2016, the strongest in state history.
State regulators could cut about in half the number of man-made quakes by restricting deep injections in the ground, said lead author Thea Hincks, an earth scientist at the University of Bristol in the United Kingdom. Companies drilling for oil and gas should not inject waste within 600 to 1500 feet (200 to 500 meters) of the geologic basement. That's the stable harder rock deep underground usually made of metamorphic and igneous rocks.
That region is usually crisscrossed with earthquake faults. The closer you get to the faults, the more likely you are to trigger them, said Stanford University geophysicist Matthew Weingarten, who wasn't part of the study.
Lab experiments show basement rocks are more susceptible to earthquakes because "having fluids in a rock is going to weaken the rock," said co-author Thomas Gernon, a geologist at the University of Southampton.
Previous studies had pinpointed the amount of fluids injected into wells as an issue. Gernon said volume does trigger earthquakes, but when volume levels were reduced the number of quakes didn't drop as much as had been expected. That's because where the stuff is put matters slightly more, he said.
The findings only apply to quakes in Oklahoma, researchers said.
Follow Seth Borenstein on Twitter at @borenbears . His work can be found here .