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高温高压下两元系H_2O-CH_4的摩尔体积 被引量:1

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摘要 利用人造流体包裹体数据和甲烷笼合物熔化温度和压力的实验数据获得了在高温高压下N_2O-CH_4两元系的摩尔体积。并将所得数据与用传统的高温高压设备和状态方程所获得的数据进行了比较。这三组数据均吻合的很好。这表明用人造流体包裹体方法获得流体系统摩尔体积的可行性和已有的状态方程在描述该两元系在高温高压下的摩尔体积的正确性。本项工作对H_2O-CH_4系统高温高压下实验数据的重要补充。同时将已有的状态方程的适用性推广到更高的温度和压力。
作者 张毅刚
出处 《地质科学》 CAS CSCD 北大核心 1997年第3期299-307,共9页 Chinese Journal of Geology(Scientia Geologica Sinica)
基金 国家自然科学基金
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参考文献4

  • 1张毅刚,Chem Geol,1992年,100卷,51页
  • 2Duan Z H,Geochim Cosmochim Acta,1992年,56卷,2605页
  • 3Duan Z H,Geochim Cosmochim Acta,1992年,56卷,2619页
  • 4Song K Y,Fluid Phase Equilib,1989年,47卷,295页

同被引文献103

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