Characterisation of colored dissolved organic matter in Hudson Bay and Hudson Strait using parallel factor analysis

被引:79
作者
Gueguen, C. [1 ]
Granskog, M. A. [2 ,3 ]
McCullough, G. [2 ]
Barber, D. G. [2 ]
机构
[1] Trent Univ, Dept Chem, Peterborough, ON K9J 7B8, Canada
[2] Univ Manitoba, Ctr Earth Observat Sci, Dept Geog & Environm, Winnipeg, MB, Canada
[3] Norwegian Polar Res Inst, Polar Environm Ctr, Tromso, Norway
基金
加拿大自然科学与工程研究理事会;
关键词
Absorption coefficient; Spectral slope; Dissolved organic matter; Fluorescence; Excitation emission matrix; PARAFAC model; Estuarine mixing; OPTICAL-PROPERTIES; FLUORESCENCE SPECTROSCOPY; ORINOCO RIVER; FRESH-WATER; NATURAL-WATERS; SEA-ICE; ABSORPTION; MARINE; CARBON; CDOM;
D O I
10.1016/j.jmarsys.2010.12.001
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Composition and concentration of colored dissolved organic matter (CDOM) have been determined in Hudson Bay and Hudson Strait by excitation emission matrix spectroscopy (EEM) and parallel factor analysis (PARAFAC). Based on 63 surface samples, PARAFAC identified three fluorescent components, which were attributed to two humic- and one protein-like components. One humic-like component was identified as representing terrestrial organic matter and showed a conservative behaviour in Hudson Bay estuaries. The second humic-like component, traditionally identified as peak M, originated both from land and produced in the marine environment. Component 3 had spectra resembling protein-like material and thought to be plankton-derived. The distribution and composition of CDOM were largely controlled by water mass mixing with protein-like component being the least affected. Distinctive fluorescence patterns were also found between Hudson Bay and Hudson Strait, suggesting different sources of CDOM. The optically active fraction of DOC (both absorbing and fluorescing) was very high in the Hudson Bay (up to 89%) suggesting that fluorescence and absorbance can be used as proxies of the DOC concentration. (C) 2010 Elsevier B.V. All rights reserved.
引用
收藏
页码:423 / 433
页数:11
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