Isotopic evidence (δ13C, δ37Cl, δ2H) for distinct transformation mechanisms of chloroform: Catalyzed H2-water system vs. zero-valent iron (ZVI)

Author:

Asfaw Berhane AbrhaORCID,Sakaguchi-Söder KaoriORCID,Schiedek ThomasORCID,Michelsen Nils,Bernstein Anat,Siebner HagarORCID,Schüth ChristophORCID

Publisher

Elsevier BV

Subject

Process Chemistry and Technology,Pollution,Waste Management and Disposal,Chemical Engineering (miscellaneous)

Reference133 articles.

1. Terrestrial natural sources of trichloromethane (chloroform, CHCl3) - an overview;Laturnus;Biogeochemistry,2002

2. Chloroform in the environment: Occurrence, sources, sinks and effects;McCulloch;Chemosphere,2003

3. T. Ivannenko, J.S. Zogorski, Sources and occurrence of chloroform and other trihalomethanes in drinking-water supply wells in the United States, 1986 – 2001, U.S. Geol. Surv. Sci. Investig. Rep. 2006–5015. (2006) 13. https://pubs.usgs.gov/sir/2006/5015/sir2006–5015.pdf.

4. Agency for toxic substances and disease registry(ATSDR). 2019 Substance Priority list, (n.d.). https://www.atsdr.cdc.gov/spl/index.html#2019spl.

5. USEPA IRIS, Chloroform (CASRN 67–66-3), Integr. Risk Inf. Syst. (1999) 1–39. https://iris.epa.gov/static/pdfs/0025_summary.pdf.

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