4.6 Article

Characterization of aquatic dissolved organic matter by asymmetrical flow field-flow fractionation coupled to UV-Visible diode array and excitation emission matrix fluorescence

期刊

JOURNAL OF CHROMATOGRAPHY A
卷 1218, 期 27, 页码 4188-4198

出版社

ELSEVIER SCIENCE BV
DOI: 10.1016/j.chroma.2010.12.038

关键词

Dissolved organic matter; Optical properties; Excitation emission matrix; UV/Visible absorbance; Athabasca River; Humic

资金

  1. National Sciences and Engineering Research Council of Canada
  2. Canada Research Chairs Program

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Flow field-flow fractionation (FIFFF) with on-line UV/Visible diode array detector (DAD) and excitation emission matrix (EEM) fluorescence detector has been developed for the characterization of optical properties of aquatic dissolved organic matter (DOM) collected in the Otonabee River (Ontario, Canada) and Athabasca River (Alberta, Canada). The molecular weight (MW) distribution of DOM was estimated using a series of organic macromolecules ranging from 479 to 66,000 Da. Both the number-average (M-n) and weight-average (M-w) molecular weights of Suwannee River fulvic acid (SRFA) and Suwannee River humic acid (SRHA) determined using these macromolecular standards were comparable to those obtained using polystyrenesulfonate (PSS) standards, suggesting that organic macromolecules can be used to estimate MW of natural organic colloids. The MW of eight river DOM samples determined by this method was found to have an M-n range of 0.8-1.1 kDa, which agrees with available literature estimates. The FIFF-FDAD-EEM system provided insight into the MW components of river DOM including the optical properties by on-line absorbance and fluorescence measurement. A red-shift in emission and excitation wavelength maxima associated with lower spectral slope ratios (S-R = S275-29:S350-400) was related to higher MW DOM. However, DOM of different origins at similar MW also showed significant difference in optical properties. A difference of 47 and 40 nm in excitation and emission peak C maxima was found. This supports the hypothesis that river DOM is not uniform in size and optical composition. (C) 2010 Elsevier B.V. All rights reserved.

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