The spectral characteristics of dissolved organic matter from sediments in Lake Baiyangdian, North China

被引:20
|
作者
Yuan, Dong-hai [1 ]
Guo, Ni [2 ]
Guo, Xu-jing [3 ]
Zhu, Neng-min [3 ]
Chen, Lu [3 ]
He, Lian-sheng [4 ]
机构
[1] Beijing Univ Civil Engn & Architecture, Minist Educ, Key Lab Urban Stormwater Syst & Water Environm, Beijing 100044, Peoples R China
[2] Sichuan Univ, Sch Hydraul & Hydroelect Engn, Chengdu 610065, Peoples R China
[3] Minist Agr, Biogas Sci Res Inst, Key Lab Dev & Applicat Rural Renewable Energy, Chengdu 610041, Peoples R China
[4] Chinese Res Inst Environm Sci, Res Ctr Water Pollut Control Technol, Beijing 100012, Peoples R China
基金
中国国家自然科学基金;
关键词
Dissolved organic matter; Fluorescence spectroscopy; Aromaticity; Parallel factor analysis; Principal component analysis; EXCITATION-EMISSION MATRIX; PARALLEL FACTOR-ANALYSIS; MUNICIPAL SOLID-WASTE; POLYCYCLIC AROMATIC-HYDROCARBONS; FLUORESCENCE SPECTROSCOPY; HUMIC SUBSTANCES; PARAFAC; DOM; ENVIRONMENTS; FRACTIONS;
D O I
10.1016/j.jglr.2014.05.006
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Dissolved organic matter (DOM) extracted from sediment samples in Lake Baiyangdian was investigated using UV -Vis absorption and fluorescence spectroscopy. Two parameters, the ratios of absorbance and dissolved organic carbon at 254 degrees nm (SUVA(254)) and the integral area from 240 degrees nm to 400 degrees nm (A(240-400)), were used to assess the molecular weight and aromaticity of DOM. The surface sediments showed a relatively low aromaticity of DOM due to the impact of environmental pollution. Synchronous fluorescence spectra showed an extremely high fraction of the protein-like region (PLR). Parallel factor analysis (PARAFAC) of excitation -emission matrix spectra revealed four fluorescent components occurring in sediment DOM: two humic-like (C1 and C2) components and two protein-like (C3 and C4) components. The PARAFAC-PCA displayed three PCA factors (factors 1,2 and 3) which accounted for 48.250%, 25.927% and 25.391%, respectively, of the variance in fluorescent component. The humic-like components 1 and 2 concurrently showed positive factor 1 loadings. Factor 2 was mainly explained by the tryptophan-like component C3. A non-humic component 4, having a low factor loading in the other two factors, showed an extremely high factor 3 loading. The EEM -PARAFAC-PCA showed varying contributions of terrestrial versus autochthonous DOM sources in lake sediments. (C) 2014 International Association for Great Lakes Research. Published by Elsevier B.V. All rights reserved.
引用
收藏
页码:684 / 691
页数:8
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