Properties and metal binding behaviors of sediment dissolved organic matter (SDOM) in lakes with different trophic states along the Yangtze River Basin: A comparison and summary

被引:51
作者
Fan, Tuantuan [1 ,2 ]
Yao, Xin [1 ,2 ,3 ]
Sun, Zhaoli [1 ]
Sang, Dongling [1 ]
Liu, Li [1 ]
Deng, Huanguang [1 ]
Zhang, Yinghao [1 ]
机构
[1] Univ Liaocheng, Sch Geog & Environm, Liaocheng 252000, Peoples R China
[2] Univ Liaocheng, Inst Huanghe Studies, Liaocheng 252000, Peoples R China
[3] Univ Liaocheng, Sch Geog & Environm, Hunan Rd, Liaocheng 252000, Peoples R China
基金
中国国家自然科学基金;
关键词
Sediment dissolved organic matter (SDOM); Yangtze River Basin (YRB); heavy metals (HMs); EEM-PARAFAC; 2D-SF; FTIR-COS; EXTRACELLULAR POLYMERIC SUBSTANCES; PARALLEL FACTOR-ANALYSIS; 2-DIMENSIONAL CORRELATION; HEAVY-METALS; FLUORESCENCE; DOM; SPECTROSCOPY; TEMPERATURE; COPPER; ENVIRONMENTS;
D O I
10.1016/j.watres.2023.119605
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The nature of sediment dissolved organic matter (SDOM) can reflect the environmental background, nutritional status and human activities and is an important part of lakes. The differences in the binding capacity of heavy metals and organic matter in lake sediments with different trophic states at the catchment scale and the mechanism of the differences in binding are still unclear. To solve this problem, we collected bulk SDOMs (< 0.7 mu m) from 6 respective lakes (from upstream to downstream) in the Yangtze River Basin (YRB) to qualitatively and quantitatively characterize their properties and metal binding behaviors using excitation-emission matrix spectroscopy combined with parallel factor analysis (EEM-FARAFAC) and two-dimensional correlation spec-troscopy of synchronous fluorescence spectroscopy and Fourier transform infrared spectroscopy (2D-SF-COS and 2D-FTIR-COS). The results showed that sediment dissolved organic carbon (SDOC) was mainly enriched in low molecular weight (LMW: < 1 kDa) fractions. The total fluorescence intensity (Fmax) of SDOM from upstream was larger than that from downstream (p = 0.033), and humic-like fluorophores were dominant in these lakes. The Fmax of sediment humic-like components (C1+C2) was closely related to the trophic levels of the lakes. Protein -like substances and oxygen-containing functional groups (C-OH, C=O, and C-O) were preferred in the reaction between SDOM and copper (Cu2+) or cadmium (Cd2+), while a unique binding path was exhibited in the moderately eutrophic DCL. In terms of fluorophore types, higher Cu2+-binding abilities (LogKCu) were observed in the humic-like matter for the lakes in the upper reaches and tryptophan-like matter for the lakes from the midstream and downstream areas of the YRB. Although Cd2+ complexed only with humic-like matter, LogKCd was higher than LogKCu. In terms of molecular weight (MW), the LogKCu/Cd of components were enhanced after MW fractionation. The HMW (0.7 mu m - 1 kDa) components possessed higher LogKCu in most lakes (except for CHL and C4). The different fluorophores and molecular weight fractions in SDOM make an important contri-bution to reducing the ecological risks of heavy metals in lakes.
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页数:12
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