Experimental controls on D/H and 13C/12C ratios of kerogen, bitumen and oil during hydrous pyrolysis

Abstract : Large isotopic transfers between water-derived hydrogen and organic hydrogen occurred during hydrous pyrolysis experiments of immature source rocks, in spite of only small changes in organic 13C/12C. Experiments at 330'C over 72 h using chips or powder containing kerogen types I and III identify the rock/water ratio as a main factor affecting ASD for water and organic hydrogen. Our data suggest that larger rock permeability and smaller rock grain size increase the H-isotopic transfer between water-derived hydrogen and thermally maturing organic matter. Increasing hydrostatic pressure may have a similar effect, but the evidence remains inconclusive
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Organic Geochemistry, Elsevier, 2003, 32, pp.1009-1018. 〈10.1016/S0146-6380(01)00059-6〉
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Arndt Schimmelmann, Jean-Paul Boudou, Michael D. Lewan, Robert P. Wintsch. Experimental controls on D/H and 13C/12C ratios of kerogen, bitumen and oil during hydrous pyrolysis. Organic Geochemistry, Elsevier, 2003, 32, pp.1009-1018. 〈10.1016/S0146-6380(01)00059-6〉. 〈bioemco-00156849〉

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