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Frontiers of Environmental Science & Engineering

ISSN 2095-2201

ISSN 2095-221X(Online)

CN 10-1013/X

Postal Subscription Code 80-973

2018 Impact Factor: 3.883

Front. Environ. Sci. Eng.    2021, Vol. 15 Issue (5) : 96    https://doi.org/10.1007/s11783-020-1340-z
RESEARCH ARTICLE
Identification of sources, characteristics and photochemical transformations of dissolved organic matter with EEM-PARAFAC in the Wei River of China
Yuanyuan Luo, Yangyang Zhang, Mengfan Lang, Xuetao Guo(), Tianjiao Xia, Tiecheng Wang, Hanzhong Jia, Lingyan Zhu()
College of Natural Resources and Environment, Northwest A&F University, Yangling 712100, China
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Abstract

• The source of DOM in surface water and sediment is inconsistent.

• The DOC content changes differently in surface water and sediment.

• The content of DOC in the surface water is lower than that in the sediment.

• The DOM in the surface water had higher photodegradation potentials than sediment.

Dissolved organic matter (DOM) in rivers is a critical regulator of the cycling and toxicity of pollutants and the behavior of DOM is a key indicator for the health of the environment. We investigated the sources and characteristics of DOM in surface water and sediment samples of the Wei River, China. Dissolved organic carbon (DOC) concentration and ultraviolet absorbance at 254 nm (UV254) increased in the surface water and were decreased in the sediment downstream, indicating that the source of DOM in the water differed from the sediment. Parallel factor (PARAFAC) analysis of the excitation-emission matrices (EEM) revealed the presence of terrestrial humus-like, microbial humus-like and tryptophan-like proteins in the surface water, whereas the sediment contained UVA humic-like, UVC humic-like and fulvic-like in the sediment. The DOM in the surface water and sediment were mainly derived from microbial metabolic activity and the surrounding soil. Surface water DOM displayed greater photodegradation potential than sediment DOM. PARAFAC analysis indicated that the terrestrial humic-like substance in the water and the fulvic-like component in the sediment decomposed more rapidly. These data describe the characteristics of DOM in the Wei River and are crucial to understanding the fluctuations in environmental patterns.

Keywords Dissolved organic matter      Parallel factor analysis      Excitation-emission matrices      Photodegradation     
Corresponding Author(s): Xuetao Guo,Lingyan Zhu   
Issue Date: 12 January 2021
 Cite this article:   
Yuanyuan Luo,Yangyang Zhang,Mengfan Lang, et al. Identification of sources, characteristics and photochemical transformations of dissolved organic matter with EEM-PARAFAC in the Wei River of China[J]. Front. Environ. Sci. Eng., 2021, 15(5): 96.
 URL:  
https://academic.hep.com.cn/fese/EN/10.1007/s11783-020-1340-z
https://academic.hep.com.cn/fese/EN/Y2021/V15/I5/96
Fig.1  Levels of DOC content and UV254 of the DOM samples collected from the surface water and sediment ((a), (b): DOC content of the surface water and sediment; (c), (d): UV254 of the surface water and sediment. Upstream: Sample site 1–5; Midstream: Sample site 6–10; Downstream: Sample site 11–15).
Fig.2  The correlations of DOC and UV254 of the surface water and sediment ((a): the surface water; (b): the sediment).
Fig.3  Emission and excitation loadings of the three fluorescent components obtained by PARAFAC in the surface water and sediment: (a), (c): Em loading of water and sediment; (b), (d): Ex loading of water and sediment.
Fig.4  Contour plots (C1、C2、C3) of the three fluorescent components obtained by PARAFAC in the surface water and sediment (a, b, c: the three components of surface water; d, e, f: the three components of sediment).
Fig.5  Box plot of FI and BIX indicator of the surface water and sediment: (a) FI value of the surface water and sediment; (b) BIX value of the surface water and sediment.
Fig.6  Variations of the FImax of PARAFAC-components during the photodegradation incubations with (w/) and without (w/o) exposure to artificial natural light (SE): (a–c) FImax of the surface water; (d–f) FImax of the sediment.
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