中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
An accurate model for calculating C2H6 solubility in pure water and aqueous NaCl solutions

文献类型:期刊论文

作者Mao, SD; Zhang, ZG; Hu, JW; Sun, R; Duan, ZH
刊名FLUID PHASE EQUILIBRIA
出版日期2005-11-25
卷号238期号:1页码:77-86
关键词C2h6 Solubility Water Aqueous Nacl Solutions Equation Of State
ISSN号0378-3812
DOI10.1016/j.fluid.2005.09.014
文献子类Article
英文摘要An accurate model is presented to calculate the solubilities of C2H6 in pure water (273-444 K and 0-1000 bar) and in aqueous NaCl solutions (273-348 K, 0-16 bar and 0-6.3 mol kg(-1)). This model is based on a specific particle interaction theory for liquid phase and a new accurate equation of state developed in this study for vapor phase. Precision of the model is within or close to the uncertainty of experimental solubilities (about 7%). A FORTRAN code is developed for this model and can be downloaded from the website: www.geochem-model.org/programs.htm. (c) 2005 Elsevier B.V. All rights reserved.
WOS关键词VAPOR-LIQUID-EQUILIBRIA ; MONTE-CARLO-SIMULATION ; PHASE-EQUILIBRIA ; TEMPERATURE RELATIONS ; GASEOUS HYDROCARBONS ; LIGHT-HYDROCARBONS ; NATURAL-WATERS ; IONIC-STRENGTH ; HIGH-PRESSURE ; HEAVY-WATER
WOS研究方向Thermodynamics ; Chemistry ; Engineering
语种英语
WOS记录号WOS:000233374800013
出版者ELSEVIER SCIENCE BV
源URL[http://ir.iggcas.ac.cn/handle/132A11/65677]  
专题中国科学院地质与地球物理研究所
通讯作者Duan, ZH
作者单位Chinese Acad Sci, State Key Lab Lithospher Evolut, Inst Geol & Geophys, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714
Mao, SD,Zhang, ZG,Hu, JW,et al. An accurate model for calculating C2H6 solubility in pure water and aqueous NaCl solutions[J]. FLUID PHASE EQUILIBRIA,2005,238(1):77-86.
APA Mao, SD,Zhang, ZG,Hu, JW,Sun, R,&Duan, ZH.(2005).An accurate model for calculating C2H6 solubility in pure water and aqueous NaCl solutions.FLUID PHASE EQUILIBRIA,238(1),77-86.
MLA Mao, SD,et al."An accurate model for calculating C2H6 solubility in pure water and aqueous NaCl solutions".FLUID PHASE EQUILIBRIA 238.1(2005):77-86.

入库方式: OAI收割

来源:地质与地球物理研究所

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