Review on the interactions of arsenic, iron (oxy)(hydr)oxides, and dissolved organic matter in soils, sediments, and groundwater in a ternary system

Article


Aftabtalab, Adeleh, Rinklebe, Jörg, Shaheen, Sabry M., Niazi, Nabeel Khan, Moreno-Jiménez, Eduardo, Schaller, Jörg and Knorr, Klaus-Holger. 2022. "Review on the interactions of arsenic, iron (oxy)(hydr)oxides, and dissolved organic matter in soils, sediments, and groundwater in a ternary system." Chemosphere. 286 (Part 2). https://doi.org/10.1016/j.chemosphere.2021.131790
Article Title

Review on the interactions of arsenic, iron (oxy)(hydr)oxides, and dissolved organic matter in soils, sediments, and groundwater in a ternary system

ERA Journal ID35098
Article CategoryArticle
AuthorsAftabtalab, Adeleh, Rinklebe, Jörg, Shaheen, Sabry M., Niazi, Nabeel Khan, Moreno-Jiménez, Eduardo, Schaller, Jörg and Knorr, Klaus-Holger
Journal TitleChemosphere
Journal Citation286 (Part 2)
Article Number131790
Number of Pages12
Year2022
PublisherElsevier
Place of PublicationUnited Kingdom
ISSN0045-6535
1465-9972
1879-1298
Digital Object Identifier (DOI)https://doi.org/10.1016/j.chemosphere.2021.131790
Web Address (URL)https://www.sciencedirect.com/science/article/abs/pii/S0045653521022621
Abstract

High concentrations of arsenic (As) in groundwater threaten the environment and public health. Geogenically, groundwater As contamination predominantly occurs via its mobilization from underground As-rich sediments. In an aquatic ecosystem, As is typically driven by several underlying processes, such as redox transitions, microbially driven reduction of iron (Fe) oxide minerals, and release of associated As. Notably, dissolved As mobilized from soils and sediments exhibits high affinity for dissolved organic matter (DOM). Thus, high DOM concentrations can increase As mobility. Therefore, it is crucial to understand the complex interactions and biogeochemical cycling of As, DOM, and Fe oxides. This review collates knowledge regarding the fate of As in multicomponent As–DOM–Fe systems, including ternary complexes involving both Fe and DOM. Additionally, the release mechanisms of As from sediments into groundwater in the presence of both Fe and DOM have been discussed. The mechanisms of As mobilization/sorption at the solid–water interface can be affected by negatively charged DOM competing for sorption sites with As on Fe (oxy)(hydr)oxides and may be further modified by other anionic ubiquitous species such as phosphate, silicic acid, or sulfur. This review emphasizes the need for a comprehensive understanding of the impact of DOM, Fe oxides, and related biogeochemical processes on As mobilization to aquifers. The review identifies important knowledge gaps that may aid in developing applicable practices for preventing the spread of As contamination in aquatic resources and traditional soil management practices.

KeywordsArsenic contamination ; Groundwater; Iron minerals
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Byline AffiliationsUniversity of Münster, Germany
University of Wuppertal, Germany
Sejong University, Korea
King Abdulaziz University, Saudi Arabia
University of Kafrelsheikh, Egypt
University of Agriculture Faisalabad, Pakistan
University of Southern Queensland
Autonomous University of Madrid, Spain
Leibniz Centre for Agricultural Landscape Research, Germany
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