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Sulfidation of ferric (hydr)oxides and its implication on contaminants transformation: a review

Journal

SCIENCE OF THE TOTAL ENVIRONMENT
Volume 816, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.scitotenv.2021.151574

Keywords

Ferric (hydr)oxides; Sulfidation; Contaminant transformation; Reduction; Adsorption; incorporation; Recrystallization

Funding

  1. National Natural Science Foundation of China [41807349, 52000040]
  2. Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) [GML2019ZD0403]
  3. Program for Guang-dong Introducing Innovative and Entrepreneurial Teams [2019ZT08L213]

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This paper provides a comprehensive review on the sulfidation process of ferric (hydr)oxides and the transformation of relevant contaminants. It presents detailed reaction mechanisms and factors that control the formation of surface associated Fe(II), iron sulfide minerals, as well as the transformation of secondary minerals. The paper also summarizes the transformation mechanisms of a variety of typical environmentally relevant contaminants and identifies challenges and further research needs in in situ remediation.
Rapid industrialization and urbanization have resulted in elevated concentrations of contaminants in the groundwa-ters and subsurface soils, posing a growing hazard to humans and ecosystems. The transformation of most contami-nants is closely linked to the mineralogy of ferric (hydr)oxides. Sulfidation of ferric (hydr)oxides is one of the most significant biogeochemical reactions in the anoxic environments, causing reductive dissolution and recrystallization of ferric (hydr)oxides and further affecting the transformation of iron-associated contaminants. This paper provides a comprehensive review on the sulfidation process of ferric (hydr)oxides and the transformation of relevant contami-nants. This review presents detailed reaction mechanisms between ferric (hydr)oxides and dissolved sulfide, and elu-cidates the factors (e.g. crystallinity of ferric (hydr)oxides, the ratio of sulfide concentration to the surface area concentration of ferric (hydr)oxides) that control the formation of surface associated Fe(II), iron sulfide minerals, as well as transformation of secondary minerals. Then, we summarized the transformation mechanisms of a variety of typical environmentally relevant contaminants existing in groundwater and subsurface soils, including heavy metals, metal(loid) oxyanions (arsenic, antimony, chromium), radionuclides (uranium, technetium), organic contaminants and phosphate/nitrate species. The general mechanisms of contaminant transformation involve a combination of re-lease, reduction and re-adsorption/incorporation processes, the specific pathway of which is highly dependent on the properties of the contaminant itself and the extent of sulfidation. Moreover, the challenge of extending our knowl-edge towards in situ remediation, as well as further research needs are identified.

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