Sources and sinks of chloromethane in a salt marsh ecosystem: constraints from concentration and stable isotope measurements of laboratory incubation experiments

Author:

Keppler Frank12345ORCID,Röhling Amelie Ninja1234,Jaeger Nicole1234,Schroll Moritz1234ORCID,Hartmann Simon Christoph12346ORCID,Greule Markus1234

Affiliation:

1. Institute of Earth Sciences

2. Heidelberg University

3. D-69120 Heidelberg

4. Germany

5. Heidelberg Center for the Environment HCE

6. Max Planck Institute for Chemistry

Abstract

Chloromethane (CH3Cl) is the most abundant long-lived chlorinated organic compound in the atmosphere and contributes significantly to natural stratospheric ozone depletion.

Publisher

Royal Society of Chemistry (RSC)

Subject

Management, Monitoring, Policy and Law,Public Health, Environmental and Occupational Health,Environmental Chemistry,General Medicine

Reference74 articles.

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2. L. J. Carpenter , S.Reimann , J. B.Burkholder , C.Clerbaux , B.Hall , R.Hossaini , J.Laube and S.Yvon-Lewis , Chapter 1: Update on Ozone-Depleting Substances (ODSs) and Other Gases of Interest to the Montreal Protocol , in Scientific Assessment of Ozone Depletion , World Meteorological Organization (WMO) , 2014 , pp. 21–125

3. S. A. Montzka and P.Fraser , Controlled substances and other source gases , in Scientific Assessment of Ozone Depletion: 2002 , World Meteorological Organization , Geneva , 2003 , ch. 1

4. Natural halocarbons in the air and in the sea

5. Ocean-atmosphere exchange of methyl chloride: Results from NW Atlantic and Pacific Ocean studies

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