焦耳-汤姆逊效应
反演(地质)
状态方程
热力学
反转温度
数学
物理
地质学
气象学
地貌学
无线电探空仪
构造盆地
作者
Behzad Haghighi,Mohammad Reza Hussaindokht,Mohammad Reza Bozorgmehr,Naser Seyed Matin
标识
DOI:10.1016/j.cclet.2007.07.002
摘要
In this paper five equations of state are tested for checking their ability to predict the Joule–Thomson inversion curve. These five equations of state are: Mohsennia–Modarres–Mansoori (MMM), Ji-Lemp (JL), modified Soave–Redlich–Kwang (SRK) equation of state by Graboski (MSRK1), modified SRK equation of state by Peneloux and Rauzy (MSRK2), and modified Peng–Robinson (PR) equation of state by Rauzy (PRmr). The investigated equations of state give good prediction of the low-temperature branch of the inversion curve, except for MMM equation of state. The high-temperature branch and the peak of the inversion curve have been observed, in general, to be sensitive to the applied equation of state. The values of the maximum inversion temperature and maximum inversion pressure are calculated for each component used in this work.
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