Characterization of CDOM in saline and freshwater lakes across China using spectroscopic analysis

被引:121
作者
Song, Kaishan [1 ]
Shang, Yingxin [1 ,2 ]
Wen, Zhidan [1 ]
Jacinthe, Pierre-Andre [3 ]
Liu, Ge [1 ]
Lyu, Lili [1 ]
Fang, Chong [1 ,2 ]
机构
[1] Chinese Acad Sci, Northeast Inst Geog & Agroecol, Changchun 130102, Jilin, Peoples R China
[2] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[3] Indiana Univ Purdue Univ Indianapolis, Dept Earth Sci, Indianapolis, IN USA
基金
中国国家自然科学基金;
关键词
Absorption; CDOM; EEMs; Freshwater; Saline water; DISSOLVED ORGANIC-MATTER; PARALLEL FACTOR-ANALYSIS; PHOTOCHEMICAL PRODUCTION; FLUORESCENCE EXCITATION; CARBON; DECOMPOSITION; MARINE; ABSORPTION; REACTIVITY; PHOTODEGRADATION;
D O I
10.1016/j.watres.2018.12.004
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Colored dissolved organic matter (CDOM) is a major component of DOM in waters, and plays a vital role in carbon cycling in inland waters. In this study, the light absorption and three-dimensional excitation emission matrix spectra (EEMs) of CDOM of 936 water samples collected in 2014-2017 from 234 lakes in five regions across China were examined to determine relationships between lake water sources (fresh versus saline) and their fluorescence/absorption characteristics. Results indicated significant differences regarding DOC concentration and a(CDOM)(254) between freshwater (6.68 mg C L-1, 19.55 m(-1)) and saline lakes (27.4 mg C L-1, 41.17 m(-1)). While humic-like (F-5) and fulvic-like (F-3) compounds contributed to CDOM fluorescence in all lake waters significantly, their contribution to total fluorescence intensity (F-T) differed between saline and freshwater lakes. Significant negative relationships were also observed between lake altitude with either F-5 (R-2 = 0.63, N = 306) or F-T (R-2 = 0.64, N = 306), suggesting that the abundance of humic-like materials in CDOM tends to decrease with increased in lakes altitude. In high altitude lakes, strong solar irradiance and UV exposure may have induced photo-oxidation reactions resulting in decreased abundance of humic-like substances and the formation of low molecular weight compounds. These findings have important implications regarding our understanding of C dynamics in lacustrine systems and the contribution of these ecosystems to the global C cycle. (C) 2018 Elsevier Ltd. All rights reserved.
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页码:403 / 417
页数:15
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