Boulder, Colorado - It’s been difficult to explain patterns of toxic mercury in some parts of the world, such as why there’s so much of the toxin deposited into ecosystems from the air in the southeastern United States, even upwind of usual sources.
A new analysis led by researchers at the University of Colorado Boulder shows that one key to understanding mercury’s strange behavior may be the unexpected reactivity of naturally occurring halogen compounds from the ocean.
“Atmospheric chemistry involving bromine and iodine is turning out to be much more vigorous than we expected,” said CU-Boulder atmospheric chemist Rainer Volkamer, the corresponding author of the new paper published in the Proceedings of the National Academy of Sciences. “These halogen reactions can turn mercury into a form that can rain out of the air onto the ground or into oceans” up to 3.5 times faster than previously estimated, he said.
The new chemistry that Volkamer and his colleagues have uncovered, with the help of an innovative instrument developed at CU-Boulder, may also help scientists better understand a longstanding limitation of global climate models. Those models have difficulty explaining why levels of ozone, a greenhouse gas, were so low before the Industrial Revolution.
“The models have been largely untested for halogen chemistry because we didn’t have measurements in the tropical free troposphere before,” Volkamer said. “The naturally occurring halogen chemistry can help explain that low ozone because more abundant halogens destroy ozone faster than had previously been realized.”
Volkamer is a Fellow of CIRES, the Cooperative Institute for Research in Environmental Sciences, at CU-Boulder and is an associate professor in the Department of Chemistry and Biochemistry. For the new paper, he worked with scientists from the U.S., China, Denmark and England.
The international team relied on a differential optical absorption spectroscopy instruments (DOAS) that Volkamer’s research group built to measure tiny amounts of atmospheric chemicals including highly reactive bromine oxide and iodine oxide radicals. Those radicals are very short-lived in the air, and collecting air samples doesn’t work well. DOAS uses solar light to measure the scattering and absorption of sunlight by gases and particles to identify the chemicals’ distinct spectroscopic fingerprints and quantify extremely small amounts directly in the atmosphere.
Reactions involving those bromine and iodine radicals can turn airborne mercury—emitted by power plants and other sources—into a water-soluble form that can stay high in the atmosphere for a long time. High in the air, the mercury can sweep around the world. Towering thunderstorms can then pull some of that mercury back out of the atmosphere to the ground, lakes or oceans. There, the toxin can accumulate in fish, creating a public health concern.
Volkamer’s team’s measurements show that the first step in that process, the oxidation of mercury in the atmosphere by bromine, happens up to 3.5 times faster than previously estimated because of halogen sources in oceans. Their work may help explain a mystery: For many pollutants, thunderstorms can rain out the chemicals quickly, so by the end of the storm there’s little left in the air. Not so for mercury. Volkamer said its concentration in rainwater remains constant throughout a storm.
“To some extent, because of these halogens, we have a larger pool of oxidized mercury up there,” Volkamer said.
Naturally occurring bromine in air aloft illustrates the global interconnectedness between energy choices affecting mercury emissions in developing nations, and mercury deposition in the U.S.
Finally, the measurements will be helpful for climate modelers seeking to improve their understanding of halogen impacts on ozone and other greenhouse gases.
The 24 authors of “Active and widespread halogen chemistry in the tropical and subtropical free troposphere” published in the current issue of the Proceedings of the National Academy of Sciences (PNAS) are from CU-Boulder and CIRES, NOAA, Harvard University, the University of Copenhagen, the National Center for Atmospheric Research, and more. The work was funded primarily by the National Science Foundation.