Arsenic distribution characteristics and release mechanisms in aquaculture lake sediments.

IF 11.3 Journal of hazardous materials Pub Date : 2024-09-05 Epub Date: 2024-07-07 DOI:10.1016/j.jhazmat.2024.135141
Xiangyu He, Wenming Yan, Xiang Chen, Yan Wang, Minjuan Li, Qi Li, Zhongbo Yu, Tingfeng Wu, Chengmei Luan, Yichun Shao, Jingwei Wu
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Abstract

It is well known that aquaculture can alter the microenvironments of lakes at sediment-water interface (SWI). However, the main mechanisms underlying the effects of aquaculture activities on arsenic (As) transformations are still unclear. In this context, the present study aims to investigate the variations in the sediment As contents in Yangcheng Lake, as well as to assess its chemical transformations, release fluxes, and release mechanisms. The results showed substantial spatial differences in the dissolved As concentrations in the sediment pore water. The As release fluxes at the SWI ranged from 1.32 to 112.09 μg/L, with an average value of 33.68 μg/L. In addition, the highest As fluxes were observed in the aquaculture areas. The transformation of crystalline hydrous Fe oxide-bound As to adsorbed-As in the aquaculture lake sediments increased the ability of As release. The Partial least squares path modeling results demonstrated the great contributions of organic matter (OM) to the As transformations by influencing the sediment microbial communities and Fe/Mn minerals. The changes in the As fractionation and competing adsorption increased the dissolved As concentrations in the 0-10 mm surface sediment. Non-specifically and specifically adsorbed As were the major sources of dissolved As in the sediments. Specifically, microbial reduction of As[V] and dissolution of Fe oxides increased the dissolved As concentrations at the SWI (20 to -20 mm). The results of the current study highlight the positive enhancement effects of aquaculture on As release from sediments.

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水产养殖湖泊沉积物中砷的分布特征和释放机制。
众所周知,水产养殖会改变湖泊沉积物-水界面(SWI)的微环境。然而,水产养殖活动对砷(As)转化影响的主要机制仍不清楚。在此背景下,本研究旨在调查阳澄湖沉积物砷含量的变化,并评估其化学转化、释放通量和释放机制。研究结果表明,沉积物孔隙水中的溶解态砷浓度存在很大的空间差异。SWI 处的砷释放通量在 1.32 至 112.09 μg/L 之间,平均值为 33.68 μg/L。此外,水产养殖区的砷通量最高。水产养殖湖泊沉积物中结晶的水合氧化铁结合砷转化为吸附砷增加了砷的释放能力。偏最小二乘法路径建模结果表明,有机质(OM)通过影响沉积物微生物群落和铁/锰矿物对砷的转化做出了巨大贡献。砷分馏和竞争吸附的变化增加了 0-10 毫米表层沉积物中的溶解砷浓度。非特异性和特异性吸附砷是沉积物中溶解砷的主要来源。具体而言,微生物还原 As[V] 和铁氧化物的溶解增加了 SWI(20 至 -20 毫米)处的溶解砷浓度。本研究的结果突显了水产养殖对沉积物中 As 释放的积极促进作用。
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