2021
DOI: 10.1016/j.jhazmat.2020.124924
|View full text |Cite
|
Sign up to set email alerts
|

Vertical redox zones of Fe–S–As coupled mineralogy in the sediments of Hetao Basin – Constraints for groundwater As contamination

Abstract: The formation of iron-sulfur-arsenic (Fe-S-As) minerals during biogeochemical processes in As contaminated aquifers remains poorly understood despite their importance to understanding As release and transport in such systems. In this study, X-ray absorption and Mössbauer spectroscopies complemented by electron microscopy, and chemical extractions were used to examine vertical changes of As, Fe and S speciation for the example of sediments in the Hetao Basin.Reduction of Fe(III), As(V) and SO4 2species were sho… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
1
1

Citation Types

1
8
0

Year Published

2021
2021
2023
2023

Publication Types

Select...
8

Relationship

0
8

Authors

Journals

citations
Cited by 16 publications
(9 citation statements)
references
References 64 publications
(92 reference statements)
1
8
0
Order By: Relevance
“…SEM-EDS images showed the presence of Fe–S containing mineral particles (∼1 μm in diameter) (Figure S3), consistent with the fact that the monosulfide fraction was generally the highest reduced S fraction (most around 50%) in the study area . The occurrence of secondary pyrite or even greigite in the study area has also been recently confirmed by Fe–S–As K-edge XANES data. , Taken together, these suggest that the Fe–S containing mineral particles were mainly secondary pyrite, which was widely found in high As aquifer sediments. , The formation of pyrite particles could immobilize aqueous As, while the oxidation of As-containing secondary pyrite particles would release the bond As. , The high sulfate extract. (356 ± 76 mg/kg), Fe­(II) sed /TFe sed (57.4 ± 1.9%), and ammonium extract.…”
Section: Resultssupporting
confidence: 82%
See 1 more Smart Citation
“…SEM-EDS images showed the presence of Fe–S containing mineral particles (∼1 μm in diameter) (Figure S3), consistent with the fact that the monosulfide fraction was generally the highest reduced S fraction (most around 50%) in the study area . The occurrence of secondary pyrite or even greigite in the study area has also been recently confirmed by Fe–S–As K-edge XANES data. , Taken together, these suggest that the Fe–S containing mineral particles were mainly secondary pyrite, which was widely found in high As aquifer sediments. , The formation of pyrite particles could immobilize aqueous As, while the oxidation of As-containing secondary pyrite particles would release the bond As. , The high sulfate extract. (356 ± 76 mg/kg), Fe­(II) sed /TFe sed (57.4 ± 1.9%), and ammonium extract.…”
Section: Resultssupporting
confidence: 82%
“…7 The occurrence of secondary pyrite or even greigite in the study area has also been recently confirmed by Fe−S−As K-edge XANES data. 76,77 Taken together, these suggest that the Fe−S containing mineral particles were mainly secondary pyrite, which was widely found in high As aquifer sediments. 78,79 The formation of pyrite particles could immobilize aqueous As, 68 while the oxidation of As-containing secondary pyrite particles would release the bond As.…”
Section: ■ Results and Discussionmentioning
confidence: 83%
“…There is a tension in the literature about the affinity of AsO 4 3– and PO 4 3– for adsorption on iron oxyhydroxides (e.g., Gt). While some studies reported higher adsorption of AsO 4 , , some other studies showed that PO 4 ,,…”
Section: Results and Discussionmentioning
confidence: 95%
“…Antelo et al reported that PO 4 3– is more sensitive to changes in pH and ionic strength. They showed that PO 4 3– adsorption increases in acidic pH at different ionic strengths and decreases at basic pH and low ionic strengths, compared to AsO 4 . Therefore, the AsO 4 3– and PO 4 3– adsorption on iron oxy-hydroxides depends on the system chemistry and may not be identical under different chemical conditions . In addition, Langmuir proposed that smaller ions with higher charges, that is, with a higher ionic potential (IP = Z/r), show a higher affinity for forming a strong covalent bond on the surface of solids.…”
Section: Results and Discussionmentioning
confidence: 99%
“…The current recommended limit of arsenic in drinking-water is 10 μg/L [5]. As rich groundwater (As >10 ug/L) is widely observed in many parts of the world such as Australia [6], Bangladesh [4], China [7], India [8], USA [9], South Korea [10] and Vietnam [11]. Flanagan et al [4] estimated that about 20 million and 45 million people in Bangladesh were exposed to As concentration greater than 50 g/L and 10 g/L respectively and approximately 24,000 deaths annually in the country due to the consumption of As rich groundwater.…”
Section: Introductionmentioning
confidence: 99%