Most earthquakes in the Barnett Shale region of North Texas occur within a few miles of one or more injection wells used to dispose of waste such as hydrofracking fluids, according to new research.

“You can’t prove that any one earthquake was caused by an injection well,” says Cliff Frohlich, senior research scientist at the Institute for Geophysics at the University of Texas at Austin. “But it’s obvious that wells are enhancing the probability that earthquakes will occur.”

For a study published in Proceedings of the National Academy of Sciences, Frohlich analyzed seismic data collected between November 2009 and September 2011 by the EarthScope US Array Program, a National Science Foundation-funded network of broadband seismometers from the Canadian border to the Gulf of Mexico. Because of the high density of instruments (25 in or near the Barnett Shale), Frohlich was able to detect earthquakes down to magnitude 1.5, far too weak for people to feel at the surface.



Map showing earthquake epicenters determined in this study (red circles), injection wells (squares and + symbols) in use since October 2006, seismograph stations (white triangles), and mapped faults (green lines). Circle sizes indicate quality of epicentral location, with large, medium and small sizes indicating qualities A, B and C. For injection wells, yellow squares are wells with maximum monthly injection rates exceeding 150,000 barrels of water per month (BWPM); white squares, exceeding 15,000 BWPM; + symbols, exceeding 1,500 BWPM. (Credit: Cliff Frohlich/U. of Texas at Austin)

None of the quakes identified in the two-year study were strong enough to pose a danger to the public.

The most reliably located earthquakes—those that are accurate to within about 0.9 miles (1.5 kilometers)—occurred in eight groups, all within 2 miles (3.2 kilometers) of one or more injection wells. Before this study, the National Earthquake Information Center had only identified two earthquake groups in the area strongly associated with specific injection wells, suggesting that injection-triggered earthquakes are far more common than is generally recognized.

The Barnett Shale is a geological formation in North Texas bearing a large amount of natural gas that was difficult to recover prior to recent technological advances such as hydraulic fracturing. The formation lies beneath Dallas and Fort Worth and extends over several counties, mostly to the west of those cities. Development of the Barnett Shale and other unconventional plays—such as the Bakken Shale in North Dakota and the Marcellus Shale in Pennsylvania, New York and West Virginia—have spurred dramatic growth in domestic natural gas production.

The new study comes as some policymakers and members of the public are expressing concern about possible environmental and health effects of hydraulic fracturing. Most earthquakes identified in the study ranged in magnitude from 1.5 to 2.5, meaning they posed no danger to the public.

“I didn’t find any higher risks from disposal of hydraulic fracturing fluids than was thought before,” says Frohlich. “My study found more small quakes, nearly all less than magnitude 3.0, but just more of the smaller ones than were previously known. The risk is all from big quakes, which don’t seem to occur here.”

All the wells nearest to the eight earthquake groups reported high injection rates (maximum monthly injection rates exceeding 150,000 barrels of water). Yet in many other areas where wells had similarly high injection rates, there were no earthquakes. Frohlich tried to address those differences.

“It might be that an injection can only trigger an earthquake if injected fluids reach and relieve friction on a nearby fault that is already ready to slip,” says Frohlich. “That just isn’t the situation in many places.”

Hydraulic fracturing is an industrial process in which water and various chemicals are pumped deep underground in order to fracture rock, allowing oil or gas to more easily flow to a well. As petroleum is produced at the surface, most hydraulic fracturing fluids return to the surface too.

Frohlich is careful to point out that he did not evaluate the possible correlation of earthquakes with the actual hydraulic fracturing process, but rather the effects of disposing of fracturing fluids and other wastes in these injection wells.

Support for this study came from the U.S. Geological Survey and the Jackson School of Geosciences at The University of Texas at Austin.

The author has no financial ties to the hydraulic fracturing industry. Frohlich has consulted for the construction industry on seismic risks for projects including dams, power plants, and pipelines. He plans to participate in a future study relating to hydraulic fracturing in the Barnett Shale by the university’s Energy Institute.

By. Tim Green