Inflow rate-driven changes in the composition and dynamics of chromophoric dissolved organic matter in a large drinking water lake

被引:121
作者
Zhou, Yongqiang [1 ,2 ,3 ]
Zhang, Yunlin [1 ]
Jeppesen, Erik [2 ,4 ,5 ]
Murphy, Kathleen R. [6 ]
Shi, Kun [1 ]
Liu, Mingliang [7 ]
Liu, Xiaohan [1 ,2 ]
Zhu, Guangwei [1 ]
机构
[1] Chinese Acad Sci, Nanjing Inst Geog & Limnol, State Key Lab Lake Sci & Environm, Taihu Lab Lake Ecosyst Res, 73 East Beijing Rd, Nanjing 210008, Jiangsu, Peoples R China
[2] Sino Danish Ctr Educ & Res, Beijing 100190, Peoples R China
[3] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[4] Aarhus Univ, Dept Biosci, Vejlsovej 25, DK-8600 Silkeborg, Denmark
[5] Aarhus Univ, Arctic Res Ctr, Vejlsovej 25, DK-8600 Silkeborg, Denmark
[6] Chalmers Univ Technol, Water Environm Technol, S-41296 Gothenburg, Sweden
[7] Inst Environm Protect Sci, Hangzhou 310014, Zhejiang, Peoples R China
基金
瑞典研究理事会; 中国国家自然科学基金;
关键词
Chromophoric dissolved organic matter (CDOM); Inflow rate; Drinking water; Parallel factor analysis (PARAFAC); Lake Qiandao; EMISSION MATRIX FLUORESCENCE; NONPOINT-SOURCE POLLUTION; PARALLEL FACTOR-ANALYSIS; XINANJIANG CATCHMENT; SHALLOW LAKE; QUALITY; RIVER; ENVIRONMENTS; TAIHU; CHINA;
D O I
10.1016/j.watres.2016.05.021
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Drinking water lakes are threatened globally and therefore in need of protection. To date, few studies have been carried out to investigate how the composition and dynamics of chromophoric dissolved organic matter (CDOM) in drinking water lakes are influenced by inflow rate. Such CDOM can lead to unpleasant taste and odor of the water and produce undesirable disinfection byproducts during drinking water treatment. We studied the drinking water Lake Qiandao, China, and found that the concentrations of suspended particulate matter (SPM) in the lake increased significantly with inflow rate (p < 0.001). Similarly, close relationships between inflow rate and the CDOM absorption coefficient at 350 nm a(350) and with terrestrial humic-like fluorescence C3 and a negative relationship between inflow rate and the first principal component (PC1) scores, which, in turn, were negatively related to the concentrations and relative molecular size of CDOM (p < 0.001), i.e. the concentration and molecular size of CDOM entering the lake increased proportionately with inflow rate. Furthermore, stable isotopes (delta D and delta O-18) were depleted in the upstream river mouth relative to downstream remaining lake regions, substantiating that riverine CDOM entering the lake was probably driven by inflow rate. This was further underpinned by remarkably higher mean chlorophyll-a and in situ measured terrestrial CDOM fluorescence (365/480 nm) and apparent oxygen utilization (AOU), and notably lower mean PC1 and CDOM spectral slope (S275-295) recorded in the upstream river mouth than in the downstream main lake area. Strong negative correlations between inflow rate and a(250):a(365), S275-295, and the spectral slope ratio (S-R) implied that CDOM input to the lake in rainy period was dominated by larger organic molecules with a more humic-like character. Rainy period, especially rainstorm events, therefore poses a risk to drinking water safety and requires higher removal efficiency of CDOM during drinking water treatment processes. (C) 2016 Elsevier Ltd. All rights reserved.
引用
收藏
页码:211 / 221
页数:11
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