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由O+CO产生的二氧化碳中异常氧同位素富集:基于实验结果和模型预测的估计

Anomalous oxygen isotope enrichment in CO2 produced from O+CO: estimates based on experimental results and model predictions.

作者信息

Pandey Antra, Bhattacharya S K

机构信息

Physical Research Laboratory, Navrangpura, Ahmedabad 380 009, India.

出版信息

J Chem Phys. 2006 Jun 21;124(23):234301. doi: 10.1063/1.2206584.

Abstract

The oxygen isotope fractionation associated with O+CO-->CO(2) reaction was investigated experimentally where the oxygen atom was derived from ozone or oxygen photolysis. The isotopic composition of the product CO(2) was analyzed by mass spectrometry. A kinetic model was used to calculate the expected CO(2) composition based on available reaction rates and their modifications for isotopic variants of the participating molecules. A comparison of the two (experimental data and model predictions) shows that the product CO(2) is endowed with an anomalous enrichment of heavy oxygen isotopes. The enrichment is similar to that observed earlier in case of O(3) produced by O+O(2) reaction and varies from 70 0/00 to 136 0/00 for (18)O and 41 0/00 to 83 0/00 for (17)O. Cross plot of delta (17)O and delta (18)O of CO(2) shows a linear relation with slope of approximately 0.90 for different experimental configurations. The enrichment observed in CO(2) does not depend on the isotopic composition of the O atom or the sources from which it is produced. A plot of Delta(delta (17)O) versus Delta(delta (18)O) (two enrichments) shows linear correlation with the best fit line having a slope of approximately 0.8. As in case of ozone, this anomalous enrichment can be explained by invoking the concept of differential randomization/stabilization time scale for two types of intermediate transition complex which forms symmetric ((16)O(12)C(16)O) molecule in one case and asymmetric ((16)O(12)C(18)O and (16)O(12)C(17)O) molecules in the other. The delta (13)C value of CO(2) is also found to be different from that of the initial CO due to the mass dependent fractionation processes that occur in the O+CO-->CO(2) reaction. Negative values of Delta(delta (13)C) ( approximately 12.1 0/00) occur due to the preference of (12)C in CO(2)* formation and stabilization. By contrast, at lower pressures (approximately 100 torr) surface induced deactivation makes Delta(delta (13)C) zero or slightly positive.

摘要

研究了与O + CO→CO₂反应相关的氧同位素分馏,其中氧原子来源于臭氧或氧光解。通过质谱分析产物CO₂的同位素组成。使用动力学模型,根据可用反应速率及其对参与分子同位素变体的修正来计算预期的CO₂组成。两者(实验数据和模型预测)的比较表明,产物CO₂具有重氧同位素的异常富集。这种富集类似于早期在O + O₂反应产生O₃的情况下观察到的情况,¹⁸O的富集范围为70‰至136‰,¹⁷O的富集范围为41‰至83‰。CO₂的δ¹⁷O和δ¹⁸O交叉图显示,对于不同的实验配置,斜率约为0.90的线性关系。在CO₂中观察到的富集不取决于O原子的同位素组成或其产生的来源。Δ(δ¹⁷O)与Δ(δ¹⁸O)(两种富集)的图显示线性相关,最佳拟合线的斜率约为0.8。与臭氧的情况一样,这种异常富集可以通过引入两种类型的中间过渡络合物的差异随机化/稳定时间尺度的概念来解释,一种情况下形成对称的(¹⁶O¹²C¹⁶O)分子,另一种情况下形成不对称的(¹⁶O¹²C¹⁸O和¹⁶O¹²C¹⁷O)分子。由于在O + CO→CO₂反应中发生的质量依赖分馏过程,还发现CO₂的δ¹³C值与初始CO的不同。由于¹²C在CO₂*形成和稳定中的偏好,出现了Δ(δ¹³C)的负值(约12.1‰)。相比之下,在较低压力(约100托)下,表面诱导失活使Δ(δ¹³C)为零或略为正值。

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