2009
DOI: 10.1016/j.gca.2009.07.028
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Diamond dissolution and the production of methane and other carbon-bearing species in hydrothermal diamond-anvil cells

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Cited by 27 publications
(12 citation statements)
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“…2). This observation also accords with results of a recent study of pure H 2 O by Kawamoto et al (2004), and contrasts with a suggestion that H 2 O may interact with diamond in the diamond cell to form CH 4 (Chou and Anderson, 2009). Moreover, interaction of C with H 2 O should also yield CO 2 , which was not reported in the latter study.…”
Section: Na5supporting
confidence: 88%
“…2). This observation also accords with results of a recent study of pure H 2 O by Kawamoto et al (2004), and contrasts with a suggestion that H 2 O may interact with diamond in the diamond cell to form CH 4 (Chou and Anderson, 2009). Moreover, interaction of C with H 2 O should also yield CO 2 , which was not reported in the latter study.…”
Section: Na5supporting
confidence: 88%
“…2b). This is likely related to the presence of methane (CH 4 ), as documented by bands at 2918 cm À1 (Chou and Anderson, 2009). The band at 2913 cm À1 is typically observed in the Raman Spectra collected during the cooling (Fig.…”
Section: Blank Experimentsmentioning
confidence: 76%
“…There was no evidence of reduced C‐bearing species in the experiments under oxidizing conditions (i.e., methane, other hydrocarbons, elemental carbon, or carbon monoxide). Methane, a species suggested by Chou and Anderson [] to form in HDAC experiments, was suggested to form because H 2 O might have reacted with carbon of the diamond anvils. Methane would be evident in Raman spectra by a sharp Raman band near 2920 cm −1 [ Dubessy et al ., ].…”
Section: Experimental Methodsmentioning
confidence: 99%