Javascript must be enabled to continue!
Tropospheric degradation of Fourth-Generation halocarbons by O3: Formation of long-lived greenhouse gases and ozone-depleting substances
View through CrossRef
Hydrofluoroolefins (HFOs) and hydrochlorofluoroolefins (HCFOs) are widely adopted as next-generation substitutes for ozone-depleting substances (ODSs) and long-lived greenhouse gases (GHGs) in refrigeration, foam-blowing, and propellant applications. In the troposphere, these compounds are primarily removed by reaction with hydroxyl radicals, resulting in short atmospheric lifetimes and low global warming potentials (GWPs) compared with their predecessors, hydrofluorocarbons (HFCs), hydrochlorofluorocarbons (HCFCs), and chlorofluorocarbons (CFCs).¹˒² However, their secondary chemistry, particularly the formation of the potent GHG trifluoromethane (HFC-23) during the ozonolysis of HFOs and HCFOs,³˒⁴ has raised increasing concern and remains incompletely understood.In this work, we examine the ozonolysis of selected HFOs and HCFOs in the 123 L EXTreme RAnge (EXTRA) chamber, a Teflon®-coated stainless-steel reactor,⁵ under atmospheric conditions (25 °C, 1 atm). Studies of four HFOs demonstrate that ozonolysis can produce either the GHG HFC-23 or carbon tetrafluoride (PFC-14). HFC-23 is formed from HFO-1234ze(E) in a yield of Figure 1. Experimentally determined ozonolysis product yields at 298 K and 1 atm pressure of: Left panel: HFC-23 from HFO-1234ze(E); Middle panel: PFC-14 from HFO-1225ye(E), HFO-1225ye(Z), and HFO-1234yf; Right panel: CFC-13 from HFCO-1233xf. Different symbols distinguish separate experiments. The panels show the ratio of products to initial HFO or HCFO concentrations plotted against the fractional change in the HFO or HCFO concentration. 1 B. Burkholder, R. A. Cox, A. R. Ravishankara, Chem. Rev., 2015, 115, 3704.2 J. Wallington, M. P. Sulbæk Andersen, O. J. Nielsen, Chemosphere, 2015, 129, 135.3 R. McGillen, Z. T. P. Fried, M. A. H. Khan, K. T. Kuwata, C. M. Martin, S. O’Doherty, F. Pecere, D. E. Shallcross, K. M. Stanley, K. Zhang, Proc. Natl. Acad. Sci. USA, 2023, 120, e23127141204.4 J. Nielsen, M. P. Sulbaek Andersen, T. J. Wallington, Atmos. Environ., 2025, 343, 120953.5 E. Leather, M. R. McGillen, C. J. Percival, Phys. Chem. Chem. Phys.,2010, 12, 2935.6 M.d.l.A. Garavagno, A. Wenger, R. E. T. Holland, B. R. Fena, S. D. Goldstein, D. E. Hicks, F. Liu, J. B. Madell, S. J. Solomon, K. T. Kuwata, M. R. McGillen, M. A. H. Khan, D. E. Shallcross, K. M. Stanley, A. J. Orr-Ewing, Environ. Sci. Technol., 2025, 59, 26031.
Title: Tropospheric degradation of Fourth-Generation halocarbons by O3: Formation of long-lived greenhouse gases and ozone-depleting substances
Description:
Hydrofluoroolefins (HFOs) and hydrochlorofluoroolefins (HCFOs) are widely adopted as next-generation substitutes for ozone-depleting substances (ODSs) and long-lived greenhouse gases (GHGs) in refrigeration, foam-blowing, and propellant applications.
In the troposphere, these compounds are primarily removed by reaction with hydroxyl radicals, resulting in short atmospheric lifetimes and low global warming potentials (GWPs) compared with their predecessors, hydrofluorocarbons (HFCs), hydrochlorofluorocarbons (HCFCs), and chlorofluorocarbons (CFCs).
¹˒² However, their secondary chemistry, particularly the formation of the potent GHG trifluoromethane (HFC-23) during the ozonolysis of HFOs and HCFOs,³˒⁴ has raised increasing concern and remains incompletely understood.
In this work, we examine the ozonolysis of selected HFOs and HCFOs in the 123 L EXTreme RAnge (EXTRA) chamber, a Teflon®-coated stainless-steel reactor,⁵ under atmospheric conditions (25 °C, 1 atm).
Studies of four HFOs demonstrate that ozonolysis can produce either the GHG HFC-23 or carbon tetrafluoride (PFC-14).
HFC-23 is formed from HFO-1234ze(E) in a yield of Figure 1.
Experimentally determined ozonolysis product yields at 298 K and 1 atm pressure of: Left panel: HFC-23 from HFO-1234ze(E); Middle panel: PFC-14 from HFO-1225ye(E), HFO-1225ye(Z), and HFO-1234yf; Right panel: CFC-13 from HFCO-1233xf.
Different symbols distinguish separate experiments.
The panels show the ratio of products to initial HFO or HCFO concentrations plotted against the fractional change in the HFO or HCFO concentration.
1 B.
Burkholder, R.
A.
Cox, A.
R.
Ravishankara, Chem.
Rev.
, 2015, 115, 3704.
2 J.
Wallington, M.
P.
Sulbæk Andersen, O.
J.
Nielsen, Chemosphere, 2015, 129, 135.
3 R.
McGillen, Z.
T.
P.
Fried, M.
A.
H.
Khan, K.
T.
Kuwata, C.
M.
Martin, S.
O’Doherty, F.
Pecere, D.
E.
Shallcross, K.
M.
Stanley, K.
Zhang, Proc.
Natl.
Acad.
Sci.
USA, 2023, 120, e23127141204.
4 J.
Nielsen, M.
P.
Sulbaek Andersen, T.
J.
Wallington, Atmos.
Environ.
, 2025, 343, 120953.
5 E.
Leather, M.
R.
McGillen, C.
J.
Percival, Phys.
Chem.
Chem.
Phys.
,2010, 12, 2935.
6 M.
d.
l.
A.
Garavagno, A.
Wenger, R.
E.
T.
Holland, B.
R.
Fena, S.
D.
Goldstein, D.
E.
Hicks, F.
Liu, J.
B.
Madell, S.
J.
Solomon, K.
T.
Kuwata, M.
R.
McGillen, M.
A.
H.
Khan, D.
E.
Shallcross, K.
M.
Stanley, A.
J.
Orr-Ewing, Environ.
Sci.
Technol.
, 2025, 59, 26031.
.
Related Results
Physiological response of Garlic (Allium sativum) to elevated tropospheric ozone in high altitude region of Western Ghats, Tamil Nadu, India
Physiological response of Garlic (Allium sativum) to elevated tropospheric ozone in high altitude region of Western Ghats, Tamil Nadu, India
Abstract
A pot culture study was conducted at Horticultural Research Station, Ooty, to assess the effect of ground-level ozone on physiology in garlic plants and find out s...
Classification of tropospheric ozone profiles over Johannesburg based on MOZAIC aircraft data
Classification of tropospheric ozone profiles over Johannesburg based on MOZAIC aircraft data
Abstract. Each ozone profile is a unique response to the photochemical and dynamic processes operating in the troposphere and hence is critical to our understanding of processes an...
Variations in tropospheric ozone driven by Rossby Wave Breaking events over the Indian subcontinent through Remote Sensing Retrievals
Variations in tropospheric ozone driven by Rossby Wave Breaking events over the Indian subcontinent through Remote Sensing Retrievals
Rossby wave breaking (RWB) is a significant pathway for intrusion of stratospheric ozone into the troposphere. These events increase tropospheric ozone, which influences the greenh...
Development of a cost efficient observation operator for GNSS tropospheric gradients
Development of a cost efficient observation operator for GNSS tropospheric gradients
<p>GNSS data collected at a single station allow the estimation of the Zenith Total Delay (ZTD) and tropospheric gradients. In order to make use of such data in numer...
Impact of Elevated Ozone on Cabbage
Impact of Elevated Ozone on Cabbage
Tropospheric ozone (O3) is a pervasive greenhouse gas and air pollutant known for its detrimental effects on human health and vegetation. In the recent years, tropospheric ozone ha...
Remote Sensing of Tropospheric Ozone from Space: Progress and Challenges
Remote Sensing of Tropospheric Ozone from Space: Progress and Challenges
Ozone stands out as a crucial trace gas within the Earth’s atmosphere, exerting a substantial influence on climate change and air pollution. Tropospheric ozone plays an important r...
Update and evaluation of the ozone dry deposition in Oslo CTM3 v1.0
Update and evaluation of the ozone dry deposition in Oslo CTM3 v1.0
Abstract. High concentrations of ozone in ambient air are hazardous not only to humans but to the ecosystem in general. The impact of ozone damage on vegetation and agricultural pl...
Novel intrathoracic irrigation using ultrafine ozone bubbles in a rat empyema model
Novel intrathoracic irrigation using ultrafine ozone bubbles in a rat empyema model
Abstract
Dissolved ozone is generally used for sanitization, but it has not been used for thoracic cavity sanitization because of its short half-life (< 20 min) and poss...

