• Spectroscopy and Spectral Analysis
  • Vol. 41, Issue 10, 3286 (2021)
Yu-yang LI1、*, Yan-ni GUO2、2;, Jun-yu ZHU2、2;, Lei ZHOU2、2; 3;, Yong-qiang ZHOU2、2; 3;, and Chun-hua HU1、1; *;
Author Affiliations
  • 11. Key Laboratory of Poyang Lake Environment and Resource Utilization, Ministry of Education, School of Resources Environmental & Chemical Engineering, Nanchang University, Nanchang 330031, China
  • 22. Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China
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    DOI: 10.3964/j.issn.1000-0593(2021)10-3286-08 Cite this Article
    Yu-yang LI, Yan-ni GUO, Jun-yu ZHU, Lei ZHOU, Yong-qiang ZHOU, Chun-hua HU. Characterizing Chromophoric Dissolved Organic Matter (CDOM) in Lake Chaohu in Different Hydrologic Seasons[J]. Spectroscopy and Spectral Analysis, 2021, 41(10): 3286 Copy Citation Text show less
    Location of sampling sites in Lake Chaohu in January, April, and July 2018
    Fig. 1. Location of sampling sites in Lake Chaohu in January, April, and July 2018
    Mothly average rainfall in the Chaohu Lake Basin from (1961—2018)
    Fig. 2. Mothly average rainfall in the Chaohu Lake Basin from (1961—2018)
    Spatial distribution of dead, flat water and water-rich a350, DOC, S275~295
    Fig. 3. Spatial distribution of dead, flat water and water-rich a350, DOC, S275~295
    The three fluorescent components obtained using parallel factor analysis and the split-half validation results were also shown
    Fig. 4. The three fluorescent components obtained using parallel factor analysis and the split-half validation results were also shown
    Spatial distribution of the four fluorescent components in the dry, the wet-to-dry transition, and the wet seasons
    Fig. 5. Spatial distribution of the four fluorescent components in the dry, the wet-to-dry transition, and the wet seasons
    Correlation between DOC, TN, TP and shortwave humus components C1, tryptophan component scoline C2, tyrosine component C3, and longwave humus components C4
    Fig. 6. Correlation between DOC, TN, TP and shortwave humus components C1, tryptophan component scoline C2, tyrosine component C3, and longwave humus components C4
    Spatial distribution of Chl-a, TP, TN in Lake Chaohuin the dry, the wet-to-dry transition, and the wet seasons
    Fig. 7. Spatial distribution of Chl-a, TP, TN in Lake Chaohuin the dry, the wet-to-dry transition, and the wet seasons
    时期DOC/
    (mg·L-1)
    S275~295/
    μm-1
    a350/
    m-1
    荧光强度/R.U.
    C1C2C3C4
    枯水期3.89±0.1919.24±0.983.50±0.640.84±0.070.71±0.160.26±0.050.15±0.02
    丰水期3.90±0.4021.48±1.563.31±0.900.76±0.170.48±0.070.25±0.030.17±0.05
    p>0.05<0.001>0.05>0.05<0.001>0.05<0.05
    Table 1. Comparison of mean and t-test results of the CDOM optical indices of Lake Chaohu during the dry and the wet seasons
    TNTPChl-aDOC
    C10.57**0.51**0.42**0.78**
    C20.16-0.10-0.150.35*
    C30.260.01-0.060.01
    C40.69**0.70**0.57**0.57**
    Table 2. Pearson correlation coefficient between microbial humic-like C1, tryptophan-like C2, tyrosine-like C3, and terrestrial humic-like C4 and water quality parameters
    Yu-yang LI, Yan-ni GUO, Jun-yu ZHU, Lei ZHOU, Yong-qiang ZHOU, Chun-hua HU. Characterizing Chromophoric Dissolved Organic Matter (CDOM) in Lake Chaohu in Different Hydrologic Seasons[J]. Spectroscopy and Spectral Analysis, 2021, 41(10): 3286
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