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Lookup NU author(s): Dr Gordon Love, Jonathan Watson
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The major organic component of carbonaceous chondrites is a solvent-insoluble, high molecular weight macromolecular material that constitutes at least 70% of the total organic content in these meteorites. Analytical pyrolysis is often used to thermally decompose macromolecular organic matter in an inert atmosphere into lower molecular weight fragments that are more amenable to conventional organic analytical techniques. Hydropyrolysis refers to pyrolysis assisted by high hydrogen gas pressures and a dispersed catalytically-active molybdenum sulfide phase. Hydropyrolysis of meteorites has not been attempted previously although it is ideally suited to such studies due to its relatively high yields. Hydropyrolysis of the Murchison macromolecular material successfully releases significant amounts of high molecular weight PAH including phenanthrene, carbazole, fluoranthene, pyrene, chrysene, perylene, benzoperylene and coronene units with varying degrees of alklyation. Analysis of both the products and residue from hydropyrolysis reveals that the meteoritic organic network contains both labile (pyrolysable) and refractory (nonpyrolysable) fractions. Comparisons of hydropyrolysis yields of Murchison macromolecular materials with those from terrestrial coals indicate that the refractory component probably consists of a network dominated by at least five- or six-ring PAH units cross-linked together. © 2004 Elsevier Ltd.
Author(s): Sephton MA, Love GD, Watson JS, Verchovsky AB, Wright IP, Snape CE, Gilmour I
Publication type: Article
Publication status: Published
Journal: Geochimica et Cosmochimica Acta
Year: 2004
Volume: 68
Issue: 6
Pages: 1385-1393
ISSN (print): 0016-7037
ISSN (electronic): 1872-9533
Publisher: Pergamon
URL: http://dx.doi.org/10.1016/j.gca.2003.08.019
DOI: 10.1016/j.gca.2003.08.019
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