Antarctica ice still releasing radioactive chlorine from 1950 nuclear bomb tests, research finds

Antarctica ice still releasing radioactive chlorine from 1950 nuclear bomb tests, research finds

A recently published study found that Antartica's ice sheets are still emitting radioactive chlorine from marine nuclear weapon tests in the 1950s. This suggests that Antartica regions contain and release the radioactive element differently than what was previously suspected. The results can help scientists with ancient ice dating and their study of the Earth's past climate.

Radioactive isotopes chlorine-36 and beryllium-10 are typically used by scientists to identify the ages of ice in ice cores, barrels of ice acquired by drilling into ice sheets, Abigail Eisenstadt of American Geophysical Union noted. Chlorine-36 has a different atomic mass than regular chlorine since it's a naturally occurring isotope.

The nuclear weapon tests in the United States conducted in the Pacific Ocean in the 1950s to 1960s resulted in reactions that triggered high concentrations of chlorine-36. The isotope reached the stratosphere, making it spread around the Earth. Some of the gas reached Antartica, where it was contained on ice and has stayed there since then.

Image credit: @noaa/Unsplash

Some isotopes from nuclear testing have mostly come back to pre-bomb levels in the past years. Scientists expected chlorine-36 to do the same, but their study showed the Vostok region in Antartica is still emitting radioactive chlorine into the atmosphere.

"There is no more nuclear chlorine-36 in the global atmosphere. That is why we should observe natural chlorine-36 levels everywhere," said co-author Mélanie Baroni, a geoscientist at the European Centre for Research and Teaching in Geosciences and the Environment in Aix-en-Provence, France.

Examining the behavior of the isotope in the continent can develop ice dating technology and help scientists understand how the planet's climate transformed over time.

Baroni and the team studied chlorine emissions in different parts of Antartica. They gathered ice samples from a snow pit at Vostok, a Russian research station in East Antartica where there is low snowfall. The scientists compared this sample to the ones from Talos Dome, where there is a big snowfall accumulation.

The results of the research showed that chlorine-36 in Talos Dome has lessened over time, while the Vostok ice had high levels of the isotope, revealing that the Vostok snowpack is still releasing radioactive chlorine.

The researchers are currently developing a plan to drill for a 1.5 million-year-old ice core in the Antartic for further research.

Reference

"A comparison of 36Cl nuclear bomb inputs deposited in snow from Vostok and Talos Dome, Antarctica, using the 36Cl/Cl‐ ratio" - Pivot, S. et al - JGR Atmospheres - https://doi.org/10.1029/2018JD030200

Abstract

36Cl production in the atmosphere is modulated by the magnetic field intensity of both the Sun and the Earth. The record of 36Cl concentration along with that of 10Be in ice cores may, therefore, provide information as to their variability. To better understand the 36Cl signal in glaciological archives, we measured its concentration in Talos Dome snow samples (mean accumulation rate of 8 g.cm‐2.yr‐1 water equivalent) spanning the 1955 to 1980 C.E. period with a resolution of one sample every 3 years, and in Vostok snow samples (mean accumulation rate of 1.96 g.cm‐2.yr‐1 water equivalent) spanning the 1949 to 2007 C.E. period with a six‐month resolution that had never before been obtained. Marine nuclear bomb tests in the late 1950s produced anthropogenic 36Cl which was injected into the stratosphere and spread around the globe. In the late 1950s, this anthropogenic pulse led to an increase of 36Cl concentration at Talos Dome that was more than 100 times higher than the pre‐ and post‐ bomb values. It is noteworthy that the atmosphere of Vostok remains polluted by anthropogenic 36Cl today. This pollution results from gaseous H36Cl mobility at low accumulation sites and implies re‐emission of 36Cl from the snowpack that is not observed at Talos Dome. The 36Cl/Cl‐ ratio may be used to discriminate the stratospheric anthropogenic 36Cl source from the tropospheric natural 36Cl source, which allows us to discuss the immobile vs. mobile 36Cl in the Vostok snowpack.

Featured image credit: @mattpalmer/Unsplash

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