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中国黄海潮间带和潮下带砷氧化还原形态及释放的季节变化:原位证据

Seasonal variations of arsenic redox speciation and release in the intertidal and subtidal zones of the Yellow Sea, China: in situ evidence.

作者信息

Luo Ting, Zhong Zhengchun, Dai Shijing, Qin Wei, Kong Shen, Zou Yang, Qian Jiayi, Sun Yan

机构信息

School of Environmental Science and Engineering, Yancheng Institute of Technology, Yancheng 224051, China; Jiangsu Province Ecology and Environment Protection Key Laboratory of Ecology and Pollution Control of Coastal Wetlands, Yancheng 224051, China.

School of Environmental Science and Engineering, Yancheng Institute of Technology, Yancheng 224051, China; Jiangsu Province Ecology and Environment Protection Key Laboratory of Ecology and Pollution Control of Coastal Wetlands, Yancheng 224051, China.

出版信息

Mar Pollut Bull. 2025 Nov;220:118425. doi: 10.1016/j.marpolbul.2025.118425. Epub 2025 Jul 10.

Abstract

Owing to seasonal changes and tidal processes, the environmental behavior of Arsenic (As) in coastal tidal flat wetlands is unclear. This study investigated the speciation and mobility of As at the sediment-water interface in the intertidal zone (IZ) and subtidal zone (SZ) during summer and winter. The DGT-As(III) in pore water increased with sediment depth, reaching maximum values of 10.3 and 2.0 μg/L at IZ and SZ sites in winter, respectively. The DGT-total As exhibited the maximum peak of 27.5 μg/L at the shallow layer in the IZ site, and of 11.6 μg/L at the deep layer in the SZ site in summer. The DGT-As(III) and DGT-total As at the IZ site were higher than at the SZ site. Seasonal changes affected the transformation of As speciation. DGT-As(III) was higher in winter than in summer in the two sites, which was attributed to the reduction of As by As-reducing bacteria (mainly respiratory reduction) and sulfate-reducing bacteria. However, DGT-total As was higher in the surface layer during summer and in the deep layer during winter at the IZ site, which was attributed to reduction and dissolution of crystalline and amorphous Fe minerals mediated by Fe-reducing bacteria. There were significant differences in the microbial composition between the two sites, and the microbial activity and As redox process were stronger at the IZ site than at the SZ site. This study reveals the different behaviors of As release in the intertidal and subtidal zones, shedding a light for controlling As pollution in coastal wetlands.

摘要

由于季节变化和潮汐过程,沿海潮滩湿地中砷(As)的环境行为尚不清楚。本研究调查了夏季和冬季潮间带(IZ)和潮下带(SZ)沉积物 - 水界面处砷的形态和迁移性。孔隙水中的DGT - As(III)随沉积物深度增加,冬季在IZ和SZ站点分别达到最大值10.3和2.0μg/L。夏季,DGT - 总砷在IZ站点浅层出现最大值27.5μg/L,在SZ站点深层出现最大值11.6μg/L。IZ站点的DGT - As(III)和DGT - 总砷高于SZ站点。季节变化影响了砷形态的转化。两个站点冬季的DGT - As(III)均高于夏季,这归因于砷还原细菌(主要是呼吸还原)和硫酸盐还原细菌对砷的还原作用。然而,IZ站点夏季表层和冬季深层的DGT - 总砷较高,这归因于铁还原细菌介导的结晶态和非晶态铁矿物的还原和溶解。两个站点的微生物组成存在显著差异,IZ站点的微生物活性和砷氧化还原过程比SZ站点更强。本研究揭示了潮间带和潮下带砷释放的不同行为,为控制沿海湿地砷污染提供了思路。

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