Ozone isotope enrichment:: Isotopomer-specific rate coefficients

被引:193
作者
Mauersberger, K [1 ]
Erbacher, B [1 ]
Krankowsky, D [1 ]
Günther, J [1 ]
Nickel, R [1 ]
机构
[1] Max Planck Inst Kernphys, Div Atmospher Phys, D-69029 Heidelberg, Germany
关键词
D O I
10.1126/science.283.5400.370
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Six rate coefficients of relative ozone formation contradict the role of molecular symmetry in the process that results in the enrichment of heavy ozone isotopomers. The results show that collisions between Light atoms, such as O-16, and heavy molecules, such as O-34(2) O-36(2), have a rate coefficient advantage of about 25 and 50 percent, respectively. over collisions involving heavy atoms and Light molecules, These results suggest that the observed isotope effect for each isotopomer may be caused by the preponderance of a single reaction channel and not through molecular symmetry selection.
引用
收藏
页码:370 / 372
页数:3
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