Worth Knowing: Dartmouth research details how fracking creates radioactive waste

Submitted 3 months ago

Two Dartmouth research papers pinpoint how fracking creates radioactive waste. Radioactivity in fracking wastewater comes from the interaction between a chemical slurry and ancient shale during the hydraulic fracturing process, according to Dartmouth College research.

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The study, detailed in twin papers appearing in Chemical Geology, is the first research that characterizes the phenomenon of radium transfer in the widely-used method to extract oil and gas. The findings add to what is already generally known about the mechanisms of radium release and could help the search for solutions to challenges in the fracking industry.

Radium from within rock leaches Radium from within rock leaches from clay minerals that transfer highly radioactive radium-228 and an organic phase that serves as the source of radium-226. (Illustration by Joshua D. Landis.)

As a result of fracking, the U.S. is already a net exporter of gas and is poised to become a net exporter of oil in the next few years. But the wastewater that is produced contains toxins like barium and radioactive radium. Upon decay, radium releases a cascade of other elements, such as radon, that collectively generate high radioactivity.

“The stuff that comes out when you frack is extremely salty and full of nasties,” said Mukul Sharma, a professor of earth sciences at Dartmouth and head of the research project. “The question is how did the waste become radioactive? This study gives a detailed description of that process.”

During fracking, millions of gallons of water combined with sand and a mixture of chemicals are pumped deep underground at high pressure. The pressurized water breaks apart the shale and forces out natural gas and oil. While the sand prevents the fractures from resealing, a large proportion of the so-called “slick water” that is injected into the ground returns to the surface as highly toxic waste.

In seeking to discover how radium is released at fracking sites, the research team combined sequential and serial extraction experiments to leach radium isotopes from shale drill core samples. For the study, the research team focused on rocks taken from Pennsylvania and New York locations of the Marcellus Shale. The geological feature is one of the major rock formations in the U.S. where fracking is being carried out to extract natural gas.

The first research paper found that radium present in the Marcellus Shale is leached into saline water in just hours to days after contact between rock and water are made. The leachable radium within the rock comes from two distinct sources, clay minerals that transfer highly radioactive radium-228, and an organic phase that serves as the source of the more abundant isotope radium-226.

The second study describes the radium transfer mechanics by combining experimental results and isotope mixing models with direct observations of radium present in wastewaters that have resulted from fracking in the Marcellus Shale.

 Taken together, the two papers show that the increasing salinity in water produced during fracking draws radium from the fractured rock. Prior to the Dartmouth study, researchers were uncertain if the radioactive radium came directly from the shale or from naturally-occurring brines present at depth in parts of the Marcellus Shale in Pennsylvania.

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