Prayon and Pulead to create JV for manufacture and sale of lithium iron phosphate material for Li-ion batteries
VW uncovers irregularities in type-approval CO2 levels affecting about 800K vehicles as part of diesel investigation

Study finds some refrigerants less damaging to ozone layer can degrade to long-lived GHG CF4

Some of the substitutes for ozone-damaging chemicals that being phased out worldwide under international agreements are themselves potent greenhouse gases and contribute to warming. A new study published in Geophysical Research Letters, a publication of the American Geophysical Union, shows for the first time how some of those replacement chemicals can break down in the atmosphere to form a greenhouse gas that can persist for millennia—much longer than the substitute chemicals themselves.

Specifically, when some chemicals widely used as refrigerants break down in the stratosphere under some conditions, they can form carbon tetraflouride (CF4)—a potent greenhouse gas that lasts for up to 50,000 years, according to scientists from the Cooperative Institute for Research in Environmental Sciences (CIRES) at the University of Colorado Boulder and the NOAA Earth System Research Laboratory (ESRL) in Boulder.

CF4 essentially lasts forever because there aren’t any known removal mechanisms in the atmosphere, said James Burkholder, a research chemist at NOAA ESRL and lead author of the study.

Burkholder’s colleague Aaron Jubb, a CIRES scientist working at NOAA ESRL and now at Oak Ridge National Laboratory, did the laboratory work showing how CF4 can be made from some halocarbons, chemicals that include hydrofluorocarbons (HFCs) and hydrochlorofluorocarbons (HCFCs) and are substitutes for the more ozone-damaging chemicals that have largely been phased out. Jubb started with trifluoroacetyl fluoride—a compound produced in the atmosphere when some halocarbons breaks down—exposed it to short-wavelength UV radiation, and looked at the reaction products that formed. CF4 was one of those breakdown products.

The amount of CF4 produced by this photochemical process was shown to be a small fraction of atmospheric CF4; industrial sources are much larger emitters of CF4. Still, identifying this particular source of such a potent and lasting greenhouse gas is important, particularly since its production could continue to grow depending on which “parent” products are used by industry.

We really need to understand the chemistry of the compounds we use. Even as we move towards shorter-lived halocarbons for industrial use, during atmospheric degradation they can produce a long-lived atmospheric effect.

—Aaron Jubb

This work was supported in part by NOAA’s Atmospheric Chemistry, Carbon Cycle, and Climate (AC4) Program and NASA’s Atmospheric Composition Program. CIRES is a partnership of NOAA and CU-Boulder.


  • Aaron M. Jubb, Max R. McGillen, Robert W. Portmann, John S. Daniel and James B. Burkholder (2015) “An atmospheric photochemical source of the persistent greenhouse gas CF4” Geophysical Research Letters doi: 10.1002/2015GL066193


The comments to this entry are closed.