Interactions of ferrous iron with clay mineral surfaces during sorption and subsequent oxidation-Reference-Cited by-同舟云学术

Interactions of ferrous iron with clay mineral surfaces during sorption and subsequent oxidation

Published:2020 Issue:6 Volume:22 Page:1355-1367
ISSN:2050-7887
Container-title:Environmental Science: Processes & Impacts
language:en
Short-container-title:Environ. Sci.: Processes Impacts

Author:

Van Groeningen Natacha¹²³⁴⁵^ORCID,ThomasArrigo Laurel K.¹²³⁴⁵^ORCID,Byrne James M.⁶⁷⁸⁹¹⁰^ORCID,Kappler Andreas⁶⁷⁸⁹¹⁰^ORCID,Christl Iso¹²³⁴⁵^ORCID,Kretzschmar Ruben¹²³⁴⁵^ORCID

Affiliation:

1. Institute of Biogeochemistry and Pollutant Dynamics

2. Department of Environmental Systems Science

3. CHN

4. ETH Zürich

5. 8092 Zürich

6. Geomicrobiology Group

7. Centre for Applied Geosciences (ZAG)

8. University of Tübingen

9. Tübingen

10. Germany

Abstract

Under anoxic conditions, clay minerals sorb dissolved Fe(ii) predominantly by forming surface precipitates, which transform into Fe(iii)-phases upon aeration.

Funder

Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung

Publisher

Royal Society of Chemistry (RSC)

Subject

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

Link

http://pubs.rsc.org/en/content/articlepdf/2020/EM/D0EM00063A

Reference77 articles.

1. Reduction of SeO42- Anions and Anoxic Formation of Iron(II)−Iron(III) Hydroxy-Selenate Green Rust

2. In Situ Time-Resolved X-ray Near-Edge Absorption Spectroscopy of Selenite Reduction by Siderite

3. Sorption of As(III) and As(V) to siderite, green rust (fougerite) and magnetite: Implications for arsenic release in anoxic groundwaters

4. Nature and origin of arsenic carriers in shallow aquifer sediments of Bengal Delta, India

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