The University of NSW has released a research paper which raises questions about the long term safety of Hydrofluoroolefin (HFO) refrigerants.
While it’s known that HFOs decompose into chemicals like trifluoroacetaldehyde, there has been persistent discussion about whether this compound further breaks down into fluoroform – the most environmentally damaging HFC they were used to replace.
The paper led by Dr Christopher Hansen from UNSW Chemistry found that HFOs do break down into a small amount of fluoroform.
“We don’t fully understand the environmental impacts of HFOs at this point,” Hansen said. “But, unlike previous examples such as the CFCs and leaded petrol, we are trying to figure out the consequences of large-scale emission before we’ve potentially harmed the environment and human health in an irreversible way. We're trying to try to change the way that science introduces new products.”
The hole in the ozone layer is a result of human activities that have released ozone-depleting chemicals, including chlorofluorocarbons (CFCs) – some of the first synthetic chemicals used as refrigerants and in aerosol cans.
Thanks to the Montreal Protocol chlorofluorocarbons (CFCs) were phased out and replaced by HFCs from the mid-1990s.
Although HFCs don't cause any ozone layer depletion, they turned out to be potent greenhouse gases.
“In the end, scientists discovered that 1kg of fluoroform – a once commonly used HFC – emitted today will contribute to as much to surface heating of the planet over the next century as more than 14,000kg of carbon dioxide,” Hansen said.
After realising the extreme greenhouse warming potential of HFCs, their global phaseout began in 2016.
HFOs, which have a shorter atmospheric lifetime, are now the leading synthetic replacements and are being rapidly proliferated as refrigerants, foam-blowing agents – such as those used in insulating foam – and aerosol propellants.
While scientists know some information about the chemical pathways of HFO decomposition, there has been a longstanding debate about whether they actually break down into some of the most environmentally unfriendly HFCs.
HFOs are made up of chemical units that are more reactive than their previous counterparts, so they don’t rise to the upper atmosphere and become long-lived greenhouse gases.
“But as chemists, we look at the structures of these molecules and we start to try and imagine what they are turned into,” Hansen said “So rather than just go, oh, this thing only has a lifetime of two weeks, it can't be a greenhouse gas, we must see what it's turned into.
“And most chemists will look at these structures, and they can draw reactions that actually lead to HFCs.”
But confirming whether HFOs break down into HFCs in low yields requires difficult experiments and most existing techniques and instruments lack the sensitivity and specificity to do so.
Dr Hansen and his team used multiple techniques, including two invented just for this study, to measure and evaluate the chemical reaction across the full range of pressures expected in the atmosphere.
“We used a variety of spectroscopic techniques to observe the reaction. And we made up a gas mixture at various pressures to simulate an atmosphere polluted with a trace amount of the immediate HFO decomposition product. Then we used a laser to simulate the photons that would otherwise come from the sun, to drive the reaction,” Hansen explained.
“We know that HFOs decompose into fluorinated carbonyls such as trifluoroacetaldehyde at a yield up to, or greater than, 100%. This means all the molecules of HFO turn into the first product and, for some HFOs, you might get two molecules of that product for each molecule of HFO that breaks down,” he said.
This study reveals that the next step of the reaction, driven by light, produces a small amount of fluoroform from the decomposition of trifluoroacetaldehyde.
Fluoroform is the HFC with the greatest global warming potential.
“We have demonstrated comprehensively that some of the most important HFOs do break down into HFCs and have provided the first hard scientific data needed to model and predict the consequences of large-scale emission,” Hansen said.
“Although the reaction only produces a small amount of fluoroform, the chemical can exist in the atmosphere for up to 200 years, and with a global warming potential more than 14000 times greater than CO2, a small yield can still have a significant impact.”
Hansen said this study settles a longstanding controversy and provides the hard, scientific data needed to model and predict the impact of large-scale emission of HFOs, before policymakers may need to react to an emerging environmental crisis.
Climate modelling groups at UNSW, as well as scientists around the world, are now ready to input this data into models, to help work out the environmental impact of continuing to use HFOs.
“Although questions remain, this paper offers crucial evidence that should inform the next steps in addressing the environmental impact of the chemicals we release into the atmosphere,” Hansen said.
Dr Hansen and his team are planning further novel experimental work. “For this paper, we performed the experiments at a single wavelength, the wavelength used in studies that are presently guiding regulators, industry, governments,” he said.
“We plan to study this chemistry using other wavelengths of light, where the yield could be higher or lower.”