“We have been scratching our heads to find helium that is free from fossil fuels,” lead author Ernest Mulaya
A major breakthrough came in 2016, when geologists discovered giant reserves of such helium near Lake Rukwa in Tanzania’s Great Rift Valley region. One year later, researchers established the key geologic conditions for “carbon-free” helium production, Mulaya said.
Related: Giant reserves of ‘gold’ hydrogen may be lurking beneath at least 30 US states, 1st-of-its-kind map reveals
The new study examined three locations — Yellowstone in the U.S., Bakreswar-Tantloi in eastern India, and the Rukwa Rift in southwestern Tanzania — that satisfy most of these conditions. Notably, the locations are geothermally active, meaning they are in places where heat from Earth’s interior rises to the surface, leading to formations such as geysers and hot springs.
Geothermal heat is required for the production of carbon-free helium, because it releases helium atoms from rocks at depth. Helium results from the decay of uranium and thorium, which takes billions of years, study co-author Jon Gluyas
“If the temperature is raised above what is called the closure temperature of the particular mineral, then the helium will be released,” Gluyas said.
The helium then enters fluids — water or brine — that flow in the space between the rocks, eventually forming a gas that can migrate underground and rise to Earth’s surface, he said. In some places — such as near Babbitt, Minnesota — Earth’s crust forms a seal that traps helium in faults between the rocks, thus forming large accumulations of the gas.
These accumulations are extremely valuable, as they could help alleviate helium shortages around the world. Helium is a critical cooling component in rockets, nuclear reactors, superconductors and medical diagnostic equipment, but suppliers may soon struggle to meet
The helium discovery in Tanzania sparked hope that similar geological settings elsewhere might also hold carbon-free helium stores, Mulaya said. In addition to being geothermally active, the Rukwa Rift sits on rocks that are billions of years old and rich in uranium and thorium, meaning helium has had ample time to form.
It turns out that Yellowstone and the Bakreswar-Tantloi province also sit on ancient, helium-producing rocks. Yellowstone is rooted in the Wyoming Craton, which contains 3.5 billion-year-old rocks, and faults on the edges of the caldera likely form conduits for huge amounts of helium, according to the new study.
A scientists studies helium gas released from the hot springs in Yellowstone National Park. Photo taken in October 1983. (Image credit: James L. Amos/Getty Images) But it’s unlikely that there is a sealed reservoir beneath Yellowstone, Gluyas said. Rather, the national park forms a system of pipes through which helium escapes into the atmosphere: Annually, about 66 tons (60 metric tons) of helium leak out via hot springs and steam vents, scientists revealed in 2014
However, “it is not as if you could put an enormous bag over the whole area and catch it,” Gluyas said.
But helium from the Wyoming Craton could be stored in reservoirs elsewhere. “There might be areas peripheral to Yellowstone where it is getting trapped once released,” Gluyas said.
The main takeaway from the new study is that “there are hugely promising conditions in all three sites,” Mulaya said, “so now, this encourages us to explore further.”
Results from a helium drill site near Babbitt suggest that carbon-free helium production is possible and that the helium concentration in the extracted gas can be extremely high .
“There’s a promising future for helium to cover the shortage we are currently facing,” Mulaya said.
