水蒸气吸收系数的声谱仪测量

B. L. Bean, K. O. White
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引用次数: 0

摘要

众所周知,实验的水蒸气吸收系数比理论方法得到的要大[1]。这在小于100厘米的区域是很明显的,在这个区域,使用标准线形的计算结果与实验数据相差2、3倍或更大。对这一现象的解释包括不正确的线形函数、二聚体或水团簇的存在,或由几种原因引起的综合影响。我们做这个实验的目的是产生一个大的数据库,包括在几个频率和许多不同组合的水蒸气和总压的吸收系数。希望这些数据能够提供足够的信息,以便生成更准确的水蒸气吸收模型,并了解实验值与理论值差异的原因。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Spectrophone Measurements of Water Vapor Absorption Coefficients
It is well known that the experimental water vapor absorption coefficients are larger than those generated by theoretical methods [1]. This is readily _, apparent in the region less than 100 cm where calculations using standard line-shapes differ from experimental data by factors of 2, 3 or larger. Explanations for this include incorrect lineshape functions, the presence of dimers or water clusters, or a combined effect due to several causes. Our purpose in doing this experiment has been to generate a large data base including absorption coefficients at several frequencies and for many different combinations of water vapor and total pressure. Hopefully, this data will provide sufficient information in order to generate a more accurate water vapor absorption model and understand the cause of the difference in the experimental and theoretical values.
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