USP Electronic Research Repository

Atmospheric abundance and global emissions of perfluorocarbons CF4, C2F6 and C3F8 since 1800 inferred from ice core, firn, air archive and in situ measurements

Trudinger, C.M. and Fraser, P.J. and Etheridge, D.M. and Sturges, W.T. and Vollmer, M.K. and Rigby, M. and Martinerie, P. and Mühle, J. and Worton, D.R. and Krummel, P.B. and Steele, L.P. and Miller, B.R. and Laube, J.C. and Mani, Francis S. and Rayner, P.J. and Harth, C.M. and Witrant, E. and Blunier, T. and Schwander, J. and O'Dorothy, S. and Battle, M. (2016) Atmospheric abundance and global emissions of perfluorocarbons CF4, C2F6 and C3F8 since 1800 inferred from ice core, firn, air archive and in situ measurements. Atmospheric Chemistry and Physics, 16 . pp. 11733-11754. ISSN 1680-7316

[img]
Preview
PDF - Published Version
Available under License Creative Commons Attribution.

Download (656Kb) | Preview

    Abstract

    Perfluorocarbons (PFCs) are very potent and longlived greenhouse gases in the atmosphere, released predominantly during aluminium production and semiconductor manufacture. They have been targeted for emission controls under the United Nations Framework Convention on Climate Change. Here we present the first continuous records of the atmospheric abundance of CF4 (PFC-14), C2F6 (PFC-116) and C3F8 (PFC-218) from 1800 to 2014. The records are derived from high-precision measurements of PFCs in air extracted from polar firn or ice at six sites (DE08, DE08-2, DSSW20K, EDML, NEEM and South Pole) and air archive tanks and atmospheric air sampled from both hemispheres. We take account of the age characteristics of the firn and ice core air samples and demonstrate excellent consistency between the ice core, firn and atmospheric measurements. We present an inversion for global emissions from 1900 to 2014. We also formulate the inversion to directly infer emission factors for PFC emissions due to aluminium production prior to the 1980s. We show that 19th century atmospheric levels, before significant anthropogenic influence, were stable at 34:1�0:3 ppt for CF4 and below detection limits of 0.002 and 0.01 ppt for C2F6 and C3F8, respectively. We find a significant peak in CF4 and C2F6 emissions around 1940, most likely due to the high demand for aluminium during World War II, for example for construction of aircraft, but these emissions were nevertheless much lower than in recent years. The PFC emission factors for aluminium production in the early 20th century were significantly higher than today but have decreased since then due to improvements and better control of the smelting process. Mitigation efforts have led to decreases in emissions from peaks in 1980 (CF4) or early-to-mid-2000s (C2F6 and C3F8) despite the continued increase in global aluminium production; however, these decreases in emissions appear to have recently halted. We see a temporary reduction of around 15% in CF4 emissions in 2009, presumably associated with the impact of the global financial crisis on aluminium and semiconductor production.

    Item Type: Journal Article
    Subjects: Q Science > Q Science (General)
    Q Science > QD Chemistry
    Divisions: Faculty of Science, Technology and Environment (FSTE) > School of Biological and Chemical Sciences
    Depositing User: Francis Mani
    Date Deposited: 14 Feb 2017 14:18
    Last Modified: 14 Feb 2017 14:20
    URI: http://repository.usp.ac.fj/id/eprint/9596
    UNSPECIFIED

    Actions (login required)

    View Item

    Document Downloads

    More statistics for this item...