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首页> 外文期刊>Journal of Physics, D. Applied Physics: A Europhysics Journal >Re-evaluation of rate coefficients for ozone decomposition by oxygen in wide range of gas pressures (20-1000 Torr) and temperatures (293-423 K)
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Re-evaluation of rate coefficients for ozone decomposition by oxygen in wide range of gas pressures (20-1000 Torr) and temperatures (293-423 K)

机译:在广泛的气体压力(20-1000托)和温度(293-423K)中,氧气对臭氧分解速率系数的重新评估

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The effective lifetime of ozone in a cylindrical cell filled with oxygen was measured in a wide range of gas pressures and temperatures by the HgI photoabsorption method. The observed effective lifetime of ozone increased with the gas pressure from 20 to 500 Torr, reached a maximum at approximately atmospheric pressure and then decreased in inverse proportion to the gas pressure. These characteristics were investigated at temperatures of 293-423 K and good agreement was observed with theoretical results derived by diffusion equation analysis of the ozone concentration in the photoabsorption cell. From the gas pressure and temperature dependencies of the effective lifetime of ozone, the diffusion coefficient of ozone in oxygen was determined together with the reflection coefficient of ozone at the surface, which was used to derive the loss rate of ozone at the surface of the cell at low gas pressures below 200 Torr. Moreover, we also simultaneously determined the rate coefficients for the decomposition of ozone by collisions with oxygen molecules and atoms which were used to derive the loss rate of ozone in the gas phase at high gas pressures of above 200 Torr. We have revealed that the Arrhenius plots, expressing the observed rate coefficients, comprised two linear portions with different slopes that transitioned from one to the other at around 353 K. Considering that the two trends reflected the decomposition of ozone by interactions with molecular and atomic oxygen, we obtained coefficients k(O-2) and k(O) taking into account the diffusion effect of ozone molecules. We derived the rate coefficient k(O-2) = 7.28 x 10(-14)exp(-9300/T) (cm(3) s(-1)) as a re-evaluated value in the present paper and k(O) = 9.52 x 10(-12)exp(-2080/T) (cm(3) s(-1)) which was consistent with data compiled in the original databases.
机译:通过HGI光吸收法测量填充有氧气的圆柱形电池中的臭氧的有效寿命。观察到的臭氧的有效寿命随着20至500托的气体压力而增加,达到大致大气压的最大值,然后与气体压力成反比。在293-423k的温度下研究了这些特性,并观察到臭氧细胞中臭氧浓度的扩散方程分析来源的良好协议。从臭氧的有效寿命的气体压力和温度依赖性,氧气中的臭氧的扩散系数与表面的反射系数一起测定,其用于导出细胞表面臭氧的损失率在低于200托的低气压下。此外,我们还同时确定了通过与氧分子和原子的碰撞分解臭氧的速率系数,其用于在高于200托的高气体压力下导出气相中的臭氧的损失率。我们已经透露,表达观察到的速率系数的Arhenius图包括两个线性部分,其具有不同的斜坡,其在353k左右从一个转变为另一个斜率。考虑到这两个趋势反映了通过与分子和原子氧的相互作用来分解臭氧的分解,考虑臭氧分子的扩散效果,我们获得系数K(O-2)和K(O)。我们衍生出速率系数K(O-2)= 7.28×10(-14)exp(-9300 / t)(cm(3)s(-1))作为本文的重新评估值和k( o)= 9.52 x 10(-12)exp(-2080 / t)(cm(3)s(-1)),它与原始数据库中编译的数据一致。

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