Abstract Details
(2020) Mass-Independent Fractionation of Triple Oxygen Isotopes Induced by Hyperfine Effect: The Role of (O2)2 Dimerization
Yan H, Peng Y & Bao H
https://doi.org/10.46427/gold2020.2967
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Hao Yan
Yongbo Peng View all 5 abstracts at Goldschmidt2020
Huiming Bao View all 4 abstracts at Goldschmidt2020 View abstracts at 15 conferences in series
Yongbo Peng View all 5 abstracts at Goldschmidt2020
Huiming Bao View all 4 abstracts at Goldschmidt2020 View abstracts at 15 conferences in series
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Submitted by Jingjun Liu on Thursday 25th June 03:59
I am not sure if this is the right revenue to ask, as the question really concerns the original 2011 Sun and Bao papers. At any rate, my question is whether the thermally induced non-mass-dependent production of 17 & 18O was caused by the ozone recombination reaction. The experiment was set at a Pyrex enclosure, so a small portion of the O2 can be photo-dissociated into O(1D), and combine with O2 molecule to form O3, similar to what happened in the troposphere today. Because the O(1D) production is small, the production of cap-delta-17O in both the O3 and then O2 are small( again, analogous to the troposphere)?
I am not sure if this is the right revenue to ask, as the question really concerns the original 2011 Sun and Bao papers. At any rate, my question is whether the thermally induced non-mass-dependent production of 17 & 18O was caused by the ozone recombination reaction. The experiment was set at a Pyrex enclosure, so a small portion of the O2 can be photo-dissociated into O(1D), and combine with O2 molecule to form O3, similar to what happened in the troposphere today. Because the O(1D) production is small, the production of cap-delta-17O in both the O3 and then O2 are small( again, analogous to the troposphere)?
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