Application of high-resolution techniques in the assessment of the mobility of Cr, Mo, and W at the sediment-water interface of Nansi Lake, China

被引:0
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作者
Jin Wang
Dan Shi
Xin Ma
Liyuan Yang
Shiming Ding
Enfeng Liu
机构
[1] University of Jinan,School of Water Conservancy and Environment
[2] Hohai University,College of Hydrology and Water Resources
[3] Nanjing Institute of Geography and Limnology,State Key Laboratory of Lake Science and Environment
[4] Chinese Academy of Sciences,College of Geography and Environment
[5] Shandong Normal University,undefined
来源
Environmental Monitoring and Assessment | 2023年 / 195卷
关键词
High-resolution sampling; Nansi Lake; Sediment-water interface; Heavy metal; Mobility;
D O I
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中图分类号
学科分类号
摘要
There are few studies on the simultaneous behavior of chromium (Cr), molybdenum (Mo), and tungsten (W) belonging to group VIB of the periodic table. Herein, based on high-resolution dialysis (HR-Peeper) and diffusive gradients in thin films (DGT) technology, the vertical distribution characteristics of DGT-labile and soluble Cr, Mo, and W in two lakes of Nansi Lake (Weishan Lake and Dushan Lake) were analyzed. In addition, the net diffusion fluxes and R-value (CDGT/Csol) were used to evaluate the mobility and release risk of metals at the sediment-water interface. The results showed that the DGT-labile concentrations of the three metal elements (Cr, Mo, and W) in Weishan Lake were higher than those in Dushan Lake, both in overlying water and sediment. This is mainly due to the dredging of the Dushan Lake area, which can permanently remove the polluted sediment in the lake. Meanwhile, the exogenous input is relatively high near the tourist area of Weishan Island. The net diffusion fluxes indicate that the W has a potential release risk of diffusion to the overlying water in Dushan Lake. The release of Cr, Mo, and W is thought to be related to the reductive dissolution of Fe/Mn (hydr)oxides based on Pearson correlation coefficients. The R-values of Cr and W indicate that Cr and W belong to the partial continuity case. The R-value of Mo was lower than the minimum value, meaning that Mo belongs to the single diffusion type and it is difficult for Mo sediments to supply pore water.
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