2014
DOI: 10.1016/j.marchem.2014.06.002
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Ultrahigh resolution mass spectrometric differentiation of dissolved organic matter isolated by coupled reverse osmosis-electrodialysis from various major oceanic water masses

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Cited by 59 publications
(76 citation statements)
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“…The molecular signatures of whole water tree-DOM as revealed by negative mode electrospray ionization FT-ICR MS (Figure 2) share many features of whole water and extracted DOM from other aquatic environments (Mopper et al, 2007;Singer et al, 2012;Chen et al, 2014;Dittmar and Stubbins, 2014;Cawley et al, 2016). Shared features include a high diversity of elemental formulas distributed broadly in van Krevelen space (Figures 6A-C) and spanning a range of molecular classes ( Table 2).…”
Section: Molecular Signatures Of Tree-dommentioning
confidence: 96%
“…The molecular signatures of whole water tree-DOM as revealed by negative mode electrospray ionization FT-ICR MS (Figure 2) share many features of whole water and extracted DOM from other aquatic environments (Mopper et al, 2007;Singer et al, 2012;Chen et al, 2014;Dittmar and Stubbins, 2014;Cawley et al, 2016). Shared features include a high diversity of elemental formulas distributed broadly in van Krevelen space (Figures 6A-C) and spanning a range of molecular classes ( Table 2).…”
Section: Molecular Signatures Of Tree-dommentioning
confidence: 96%
“…The extreme mass accuracy and precision of FT-ICR MS allows the exact elemental composition of ions to be calculated-a major breakthrough for the characterization of DOM and its molecular messages (Dittmar and Stubbins, 2013;Mopper et al, 2007). In each photochemical study employing FT-ICR MS, aromatic carbon or high double bond equivalent molecules constituted the most photolabile DOM fractions (Chen et al, 2014;Gonsior et al, 2009;Kujawinski et al, 2004;Stubbins et al, 2010). The average molecular weight of DOM also decreases during irradiations.…”
Section: Dom Photolability Spectrum and Fate Of Terrestrial Dom Imentioning
confidence: 99%
“…Spectral slope (S) and slope ratio (S R ) were calculated (Helms et al, 2013). DOC was measured as non-purgeable organic carbon using hightemperature catalytic combustion by high temperature combustion (720°C) on a Shimadzu TOC-VCPH (Shimadzu Scientific Instruments; Chen et al, 2014a). Specific UV absorbance (SUVA) was calculated by dividing decadic absorbance in units of m −1 by the DOC concentration in units of mg C L −1 (Weishaar et al, 2003).…”
Section: Uv-visible Spectroscopy and Dissolved Organic Carbon Analysismentioning
confidence: 99%
“…Initial seawater sample DOC concentrations were 39 to 88 μmol L −1 and were concentrated by RO/ED to 1076 to 4298 μmol L −1 (Table 1; Chen et al, 2014a). DOC recoveries for the RO/ED process ranged from 40 to 68% in the North Atlantic Ocean samples (3 samples average = 51%) and 83 to 86% in the Pacific Ocean samples (2 samples average = 84%; Chen et al, 2014a).…”
Section: Bulk Organic and Inorganic Properties Of Ro/ed Isolatesmentioning
confidence: 99%
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