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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 Envir Sci Eng Chin    2011, Vol. 5 Issue (3) : 426-434    https://doi.org/10.1007/s11783-010-0264-4
RESEARCH ARTICLE
Three-dimensional fluorescence spectral characterization of soil dissolved organic matters in the fluctuating water-level zone of Kai County, Three Gorges Reservoir
Fang FANG, Yan YANG, Jinsong GUO(), Hong ZHOU, Chuan FU, Zhe LI
Key Laboratory of Three Gorges Reservoir Region’s Eco-Environment of Ministry of Education, Chongqing University, Chongqing 400045, China
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Abstract

Three-dimensional fluorescence spectroscopy was used to investigate the fluorescent properties of soil dissolved organic matter (DOM) in the water-level-fluctuation zone (WLFZ) of Kai County, Three Gorges Reservoir (TGR). Most of the soil DOM analyzed in this study was found to contain four fluorescence peaks. Peaks A and C represent humic-like fluorescence, whereas peaks B and D represent tryptophan-like fluorescence. Peaks E and F, which represent tyrosine-like fluorescence, only appeared in certain soils. Soil humus was the main source of DOM in soil, and higher concentration of soil DOM was found in the exposed soil than submerged soil. Compared to the peaks A and B, the fluorescence intensities of peaks C and D were strongly influenced by the fluctuating water level. Analysis of fluorescence intensities of different peaks in soil DOM showed that WLFZ soil was not contaminated significantly. Soil DOM contained at least two types of humic-like fluorescence groups and two types of protein-like fluorescence groups. The proportion of the content of peak A in soil organic matter was quite stable. The soil DOM in exposed soil had relatively high humification and aromaticity, and periodic submerging and exposure of soil had an impact on the humification of soil DOM.

Keywords water-level-fluctuation zone (WLFZ)      soil      dissolved organic matter (DOM)      three-dimensional fluorescence spectra     
Corresponding Author(s): GUO Jinsong,Email:guo0768@126.com   
Issue Date: 05 September 2011
 Cite this article:   
Jinsong GUO,Fang FANG,Yan YANG, et al. Three-dimensional fluorescence spectral characterization of soil dissolved organic matters in the fluctuating water-level zone of Kai County, Three Gorges Reservoir[J]. Front Envir Sci Eng Chin, 2011, 5(3): 426-434.
 URL:  
https://academic.hep.com.cn/fese/EN/10.1007/s11783-010-0264-4
https://academic.hep.com.cn/fese/EN/Y2011/V5/I3/426
fluorescence peakEx(excitation wavelength)/Em(emission wavelength)/nmtypereferences
A310-360/410-480visible humic-like[9-11]
B270-290/320-350high excitation wavelength tryptophan-like[9,11]
C240-270/370-480UV humic-like[9-11]
D220-230/320-350low excitation wavelength tryptophan-like[9,11]
E270-290/300-320high excitation wavelength tyrosine-like[9,11]
F220-230/300-320low excitation wavelength tyrosine-like[9]
Tab.1  Fluorescent matters and the corresponding peak positions in DOM
Fig.1  Map of sampling locations in research area
Fig.2  Three-dimensional fluorescence spectra of DOM in WLFZ of Kai County
DOM samplesample elevation/mfluorescence intensity/arbr(C, A)r(D, B)r(B, A)HIXsoil organic matter/%
Flu AFlu BFlu CFlu DFlu EFlu F
submerged areaFengle 1154-155728.8532.0570.7237.0627.8211.50.780.450.732.402.46
Fengle 2154-156385.5220.5473.6205.7162.21.230.930.573.161.41
Linjiang 1169-17113511281748.11129422.90.550.952.122.69
Linjiang 2170-171166.4285.7217.1151.21.722.921.06
Zhuxi 1170-171376.1274.2345.0133.40.920.490.732.401.61
Hanfeng 1162-163319.1133.8416.3191.91.301.430.425.340.52
Hanfeng 2170-171150.1113.3243.4125.71.621.110.753.000.63
Hanfeng 3170-171331.7211.9429.2312.41.291.470.643.230.78
Hanfeng 4169-170176.6269.1127.51.523.500.63
exposed areaLinjiang 3173-174663.7425.2858.210411.292.450.644.331.98
Zhuxi 2172-173192.2252.0339.6239.51.770.951.314.390.90
Zhuxi 3173-174466.1251.9757.3829.31.623.290.544.561.09
Zhuxi 4174-175513.6265.7663.8287.11.291.080.525.091.51
Zhuxi 5173-174762.5390.8783.8300.21.030.770.514.642.73
Zhenan 1174-175314.4233.1554.6740.81.763.180.744.170.91
Zhenan 2174-175317.2351.9432.3318.31.360.901.117.040.70
Zhenan 3173-174448.6652.3281.31.455.141.18
Zhenan 4173-174449.7462.4652.2666.71.451.441.033.221.21
Zhenan 5173-174372.8273.9583.9441.41.571.610.733.410.95
Zhenan 6173-174593.6453.1769.4636.91.301.410.763.751.52
Houba 1172-173526.4514.0570.4317.41.080.620.983.161.88
Houba 2174-175494.2679.1230.61.375.361.01
Houba 3173-174414.2605.6281.41.465.941.08
Houba 4173-174408.3427.7582.31.056.101.12
Tab.2  Fluorescence intensities and ratios of DOM and soil organic matter in WLFZ
Fig.3  Average fluorescence intensities of different peaks of soil DOM in WLFZ of Kai County
r(B, A)r(C, A)r(D, B)
submerged area average distribution0.68±0.060.42-0.951.21±0.130.55-1.720.98±0.440.45-1.47
exposed area average distribution0.81±0.080.51-1.311.39±0.061.03-1.771.61±0.950.62-3.29
Tab.3  Ratios of soil DOM in WLFZ of Kai County
typesoil organic matterpeak Apeak Bpeak Cpeak D
peak Acorrelation coefficient r0.857**1.000
sample number n2324
peak Bcorrelation coefficient r0.711**0.913**1.000
sample number n171818
peak Ccorrelation coefficient r0.590**0.714**0.492*1.000
sample number n24241824
peak Dcorrelation coefficient r0.1560.3730.3100.641**1.000
sample number n2323172323
Tab.4  Correlations between fluorescence intensities of soil DOM and correlations between fluorescence intensities and soil organic matter in WLFZ of Kai County
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