Hydrate phase equilibria for gas mixtures containing carbon dioxide: A proof-of-concept to carbon dioxide recovery from multicomponent gas stream

2000 ◽  
Vol 17 (6) ◽  
pp. 659-667 ◽  
Author(s):  
Yu-Taek Seo ◽  
Seong-Pil Kang ◽  
Huen Lee ◽  
Chul-Soo Lee ◽  
Won-Mo Sung
2001 ◽  
Vol 46 (2) ◽  
pp. 381-384 ◽  
Author(s):  
Yu-Taek Seo ◽  
Huen Lee ◽  
Ji-Ho Yoon

2021 ◽  
Vol 83 (3) ◽  
pp. 372-378
Author(s):  
A. A. Sizova ◽  
S. A. Grintsevich ◽  
M. A. Kochurin ◽  
V. V. Sizov ◽  
E. N. Brodskaya

Abstract Grand canonical Monte Carlo simulations were performed to study the occupancy of structure I multicomponent gas hydrates by CO2/CH4, CO2/N2, and N2/CH4 binary gas mixtures with various compositions at a temperature of 270 K and pressures up to 70 atm. The presence of nitrogen in the gas mixture allows for an increase of both the hydrate framework selectivity to CO2 and the amount of carbon dioxide encapsulated in hydrate cages, as compared to the CO2/CH4 hydrate. Despite the selectivity to CH4 molecules demonstrated by N2/CH4 hydrate, nitrogen can compete with methane if the gas mixture contains at least 70% of N2.


2010 ◽  
Vol 55 (10) ◽  
pp. 4406-4411 ◽  
Author(s):  
Qing-Lan Ma ◽  
Xiu-Lin Wang ◽  
Guang-Jin Chen ◽  
Chang-Yu Sun ◽  
Lan-Ying Yang

2000 ◽  
Vol 123 (3) ◽  
pp. 450-457 ◽  
Author(s):  
Vladimir P. Solovjov ◽  
Brent W. Webb

An efficient approach for predicting radiative transfer in high temperature multicomponent gas mixtures with soot particles is presented. The method draws on the previously published multiplication approach for handling gas mixtures in the spectral line weighted-sum-of-gray-gases (SLW) model. In this method, the gas mixture is treated as a single gas whose absorption blackbody distribution function is calculated through the distribution functions of the individual species in the mixture. The soot is, in effect, treated as another gas in the mixture. Validation of the method is performed by comparison with line-by-line solutions for radiative transfer with mixtures of water vapor, carbon dioxide, and carbon monoxide with a range of soot loadings (volume fractions). Comparison is performed also with previously published statistical narrow band and classical weighted-sum-of-gray-gases solutions.


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