Critical Role of Mineral Fe(IV) Formation in Low Hydroxyl Radical Yields during Fe(II)-Bearing Clay Mineral Oxygenation-Reference-Cited by-同舟云学术

Critical Role of Mineral Fe(IV) Formation in Low Hydroxyl Radical Yields during Fe(II)-Bearing Clay Mineral Oxygenation

Published:2024-05-21 Issue:22 Volume:58 Page:9669-9678
ISSN:0013-936X
Container-title:Environmental Science & Technology
language:en
Short-container-title:Environ. Sci. Technol.

Author:

Yu Chenglong¹,Ji Wenwen¹,Li Xinyi¹,Yuan Songhu²^ORCID,Zhang Peng²^ORCID,Pu Shengyan¹³^ORCID

Affiliation:

1. State Key Laboratory of Geohazard Prevention and Geoenvironment Protection, Chengdu University of Technology, Chengdu 610059, P. R. China

2. State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430078, P. R. China

3. State Key Laboratory of Environmental Criteria and Risk Assessment, Chinese Research Academy of Environmental Sciences, Beijing 100012, P. R. China

Funder

National Key Research and Development Program of China

National Natural Science Foundation of China

Publisher

American Chemical Society (ACS)

Link

https://pubs.acs.org/doi/pdf/10.1021/acs.est.3c09986

Reference61 articles.

1. Production of Abundant Hydroxyl Radicals from Oxygenation of Subsurface Sediments

2. Dynamic Production of Hydroxyl Radicals during the Flooding–Drainage Process of Paddy Soil: An In Situ Column Study

3. Redox Oscillations Activate Thermodynamically Stable Iron Minerals for Enhanced Reactive Oxygen Species Production

4. Tide-Triggered Production of Reactive Oxygen Species in Coastal Soils

5. Diel Fluctuation of Extracellular Reactive Oxygen Species Production in the Rhizosphere of Rice

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