Spectral Characteristics Variations of Chromophoric Dissolved Organic Matter During Growth of Filamentous Green Macroalgae

被引:2
作者
Jiang De-gang [1 ]
Huang Qing-hui [1 ]
Li Jian-hua [1 ]
机构
[1] Tongji Univ, Key Lab Yangtze River Water Environm, Minist Educ, Coll Environm Sci & Engn, Shanghai 200092, Peoples R China
关键词
Chromophoric dissolved organic matter; Filamentous green macroalgae; Fluorescence excitation-emission matrix spectrum; Parallel factor analysis; FLUORESCENCE; MARINE; SPECTROSCOPY; ENVIRONMENTS; TERRESTRIAL; SUBSTANCES; SEA;
D O I
10.3964/j.issn.1000-0593(2010)07-1880-06
中图分类号
O433 [光谱学];
学科分类号
0703 ; 070302 ;
摘要
As an important component of dissolved organic matter (DOM), chromophoric dissolved organic matter (CDOM) plays a central role in the global biogeochemical carbon cycle. Macroalgae are essential producers in aquatic ecosystems. They can release a considerable part of photosynthetic products as CDOM. So changes in optical properties of CDOM are studied on filamentous green macroalgae-Chadophorasle found in tidal flats of a brackish Lake Beihu in natural field condition by using spectrometry. Humic-like fluorescence peaks and protein-like fluorescence peaks detected by fluorescence excitation-emission matrix spectrum (EEMS) change little in control experiment but increase dramatically in incubation experiment. Applying parallel factor analysis (PARAFAC) together with fluorescence excitation-emission matrix can get four components of CDOM (C-1, C-2 C-3 and C-4) which are relative to humic-like fluorescence peak A(C), M and protein-like fluorescence peak B, T respectively. In incubation experiment four components increase by 211.5%, 255.8%, 75.3% and 129.3% respectively while in control experiment components have little changes except C-1 decreasing by 34.3%. Absorption coefficient a(355) increases by 92.9% and has positive significant correlation(P<0.01) with the four components in incubation experiment while a(355) decreases by 59.8% and only has correlation (P<0.05) with C-1 in control experiment. As the parameters representing CDOM molecular weight and composition, M and S values in incubation experiment are smaller than in control experiment, which illustrate that aromatic and macromolecular CDOM is produced in growth of Chadophorasle. All results indicate that growth of Chadophorasle can change the content and composition of CDOM.
引用
收藏
页码:1880 / 1885
页数:6
相关论文
共 20 条
[1]   Impact of chromophoric dissolved organic matter on UV inhibition of primary productivity in the sea [J].
Arrigo, KR ;
Brown, CW .
MARINE ECOLOGY PROGRESS SERIES, 1996, 140 (1-3) :207-216
[2]   Changes in CDOM fluorescence from allochthonous and autochthonous sources during tidal mixing and bacterial degradation in two coastal estuaries [J].
Boyd, TJ ;
Osburn, CL .
MARINE CHEMISTRY, 2004, 89 (1-4) :189-210
[3]   Marine optical biogeochemistry: The chemistry of ocean color [J].
Coble, Paula G. .
CHEMICAL REVIEWS, 2007, 107 (02) :402-418
[4]   Characterization of marine and terrestrial DOM in seawater using excitation emission matrix spectroscopy [J].
Coble, PG .
MARINE CHEMISTRY, 1996, 51 (04) :325-346
[5]   Bacterial growth in humic waters exposed to UV-radiation and simulated sunlight [J].
Corin, N ;
Backlund, P ;
Wiklund, T .
CHEMOSPHERE, 1998, 36 (09) :1947-1958
[6]   Factors influencing photoreactions of dissolved organic matter in a coastal river of the southeastern United States [J].
Gao, HZ ;
Zepp, RG .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 1998, 32 (19) :2940-2946
[7]  
GUO WD, 2008, ENV SCI, V29, P4641
[8]   Further evidence of elemental composition as an indicator of the bioavailability of humic substances to bacteria [J].
Hunt, AP ;
Parry, JD ;
Hamilton-Taylor, J .
LIMNOLOGY AND OCEANOGRAPHY, 2000, 45 (01) :237-241
[9]  
LI HB, 2006, J ATMOSPHERIC ENV OP, V1, P216
[10]  
MORAN MA, 1997, LIMNOLOGY OCEANOGRAP, V42, P1317