GEOC 13 |
| Information on the chemical composition of dissolved organic matter (DOM) is crucial to understand its source and reactivity. We sampled water from a transect, beginning in the Dismal Swamp, continuing up to the Chesapeake Bay and out to its adjacent coastal areas. DOM characterization was achieved using HPLC and Fourier transform ion cyclotron resonance mass spectrometry (FTICR-MS). Our results showed that there is a major shift from aromatic to aliphatic components in DOM from the Elizabeth River to the Chesapeake Bay mouth. Based on the ion fragment analysis, the aromatic components source from lignin in degraded woods, and the lignin-derived compounds are either decomposed or highly modified into aliphatic compounds by micro-organisms or photochemistry. This new elemental approach for the analysis of DOM has allowed for its extensive characterization and is the first time that molecular level information has been acquired for DOM along this type of transect. |
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The Biogeochemical Cycling of Natural Organic Matter in the Coastal Zone
8:30 AM-11:55 AM, Sunday, August 19, 2007 Boston Park Plaza -- Thoreau Rm, Oral
Sci-Mix
Division of Geochemistry |