An enthalpy model of CO2-CH4-H2S-N2-brine systems applied in simulation of non-isothermal multiphase and multicomponent flow with high pressure, temperature and salinity

被引:10
|
作者
Guo, Yongfan [1 ,3 ]
Li, Jun [1 ]
Ahmed, Raheel [2 ]
Shen, Nao [1 ,3 ]
Li, Xiaochun [1 ]
机构
[1] Chinese Acad Sci, Inst Rock & Soil Mech, State Key Lab Geomech & Geotech Engn, Wuhan 430071, Hubei, Peoples R China
[2] Dimue Technol Co Ltd, Wuhan 430071, Hubei, Peoples R China
[3] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
基金
中国国家自然科学基金; 国家重点研发计划;
关键词
Enthalpy model; CO2-CH4-H2S-N-2-brine; Non-isothermal effect; Multiphase and multicomponent flow; Carbon geological utilization and storage (CGUS); Numerical simulation; AQUEOUS SODIUM-CHLORIDE; EQUATION-OF-STATE; CALCULATING CO2 SOLUBILITY; CARBON-DIOXIDE; THERMODYNAMIC PROPERTIES; NACL SOLUTIONS; GASEOUS-MIXTURES; PHASE-EQUILIBRIA; EXCESS ENTHALPY; PREDICTIVE; 1978;
D O I
10.1016/j.jcou.2019.02.018
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
An accurate enthalpy model for CO2-CH4-H2S-N-2-brine fluid system is proposed in this work. For the gas system (CO2-CH4-H2S-N-2), the model is based on Peng-Robinson EOS enthalpy deviation to calculate real gas system specific enthalpy. For the brine system, the model extends conventional saturation state enthalpy model considering pressure effect along with the temperature and salinity effects. For the dissolution heat, the model combines phase equilibrium parameters to describe the gas dissolved enthalpy. The model can predict CO2-CH4-H2S-N-2-brine fluid system enthalpy well with temperature range from 0 to 300 degrees C, pressure range from 0 to 1000 bar and salinity range from 0 to 6 mol/kg water. The model performs favorable with respect to existing experimental data and other models and reproduces reliable data for pure water, various salinity of brine and gas systems.
引用
收藏
页码:85 / 97
页数:13
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