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The Effects and Mechanisms of pH and Dissolved Oxygen Conditions on the Release of Arsenic at the Sediment–Water Interface in Taihu Lake

The pH and dissolved oxygen (DO) conditions are important environmental factors that control the migration of arsenic (As) at the sediment–water interface. This study investigates the distribution differences of reactive iron, manganese, and arsenic at the sediment–water interface under anaerobic an...

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Autores principales: Zeng, Liqing, Yan, Changzhou, Yang, Fan, Zhen, Zhuo, Yang, Jiaming, Chen, Jielun, Huang, Yujie, Xiao, Yuhui, Zhang, Wen
Formato: Online Artículo Texto
Lenguaje:English
Publicado: MDPI 2023
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10675530/
https://www.ncbi.nlm.nih.gov/pubmed/37999542
http://dx.doi.org/10.3390/toxics11110890
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author Zeng, Liqing
Yan, Changzhou
Yang, Fan
Zhen, Zhuo
Yang, Jiaming
Chen, Jielun
Huang, Yujie
Xiao, Yuhui
Zhang, Wen
author_facet Zeng, Liqing
Yan, Changzhou
Yang, Fan
Zhen, Zhuo
Yang, Jiaming
Chen, Jielun
Huang, Yujie
Xiao, Yuhui
Zhang, Wen
author_sort Zeng, Liqing
collection PubMed
description The pH and dissolved oxygen (DO) conditions are important environmental factors that control the migration of arsenic (As) at the sediment–water interface. This study investigates the distribution differences of reactive iron, manganese, and arsenic at the sediment–water interface under anaerobic and aerobic conditions at different pH levels. The strong buffering capacity of sediment to water pH results in a shift towards neutral pH values in the overlying water under different initial pH conditions. The level of DO becomes a key factor in the release of As from sediment, with lower DO environments exhibiting higher release quantities and rates of As compared to high DO environments. Under low DO conditions, the combined effects of ion exchange and anaerobic reduction lead to the most significant release of As, particularly under pH 9.5 conditions. The formation of amorphous ferrous sulfide compounds under low DO conditions is a significant factor contributing to increased arsenic concentration in the interstitial water. Therefore, the re-migration of endogenous arsenic in shallow lake sediments should consider the combined effects of multiple driving forces.
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spelling pubmed-106755302023-10-30 The Effects and Mechanisms of pH and Dissolved Oxygen Conditions on the Release of Arsenic at the Sediment–Water Interface in Taihu Lake Zeng, Liqing Yan, Changzhou Yang, Fan Zhen, Zhuo Yang, Jiaming Chen, Jielun Huang, Yujie Xiao, Yuhui Zhang, Wen Toxics Article The pH and dissolved oxygen (DO) conditions are important environmental factors that control the migration of arsenic (As) at the sediment–water interface. This study investigates the distribution differences of reactive iron, manganese, and arsenic at the sediment–water interface under anaerobic and aerobic conditions at different pH levels. The strong buffering capacity of sediment to water pH results in a shift towards neutral pH values in the overlying water under different initial pH conditions. The level of DO becomes a key factor in the release of As from sediment, with lower DO environments exhibiting higher release quantities and rates of As compared to high DO environments. Under low DO conditions, the combined effects of ion exchange and anaerobic reduction lead to the most significant release of As, particularly under pH 9.5 conditions. The formation of amorphous ferrous sulfide compounds under low DO conditions is a significant factor contributing to increased arsenic concentration in the interstitial water. Therefore, the re-migration of endogenous arsenic in shallow lake sediments should consider the combined effects of multiple driving forces. MDPI 2023-10-30 /pmc/articles/PMC10675530/ /pubmed/37999542 http://dx.doi.org/10.3390/toxics11110890 Text en © 2023 by the authors. https://creativecommons.org/licenses/by/4.0/Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/).
spellingShingle Article
Zeng, Liqing
Yan, Changzhou
Yang, Fan
Zhen, Zhuo
Yang, Jiaming
Chen, Jielun
Huang, Yujie
Xiao, Yuhui
Zhang, Wen
The Effects and Mechanisms of pH and Dissolved Oxygen Conditions on the Release of Arsenic at the Sediment–Water Interface in Taihu Lake
title The Effects and Mechanisms of pH and Dissolved Oxygen Conditions on the Release of Arsenic at the Sediment–Water Interface in Taihu Lake
title_full The Effects and Mechanisms of pH and Dissolved Oxygen Conditions on the Release of Arsenic at the Sediment–Water Interface in Taihu Lake
title_fullStr The Effects and Mechanisms of pH and Dissolved Oxygen Conditions on the Release of Arsenic at the Sediment–Water Interface in Taihu Lake
title_full_unstemmed The Effects and Mechanisms of pH and Dissolved Oxygen Conditions on the Release of Arsenic at the Sediment–Water Interface in Taihu Lake
title_short The Effects and Mechanisms of pH and Dissolved Oxygen Conditions on the Release of Arsenic at the Sediment–Water Interface in Taihu Lake
title_sort effects and mechanisms of ph and dissolved oxygen conditions on the release of arsenic at the sediment–water interface in taihu lake
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10675530/
https://www.ncbi.nlm.nih.gov/pubmed/37999542
http://dx.doi.org/10.3390/toxics11110890
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