2007
DOI: 10.1021/ie070846c
|View full text |Cite
|
Sign up to set email alerts
|

Phase Equilibrium in Two-Phase, Water-Rich-Liquid, Hydrate Systems:  Experiment and Theory

Abstract: Two-phase equilibrium between CO 2 hydrate (H) and a water-rich liquid (L) are experimentally measured and theoretically described between 273 and 281 K, at pressures below 30 MPa, and at aqueous CO 2 concentrations between 0.0163 and 0.0242 mole fraction. These data represent the conditions where hydrates form from a single-phase aqueous solution of fixed composition. Both theoretical and experimental results indicate that the equilibrium pressure is very sensitive to concentration at all temperatures. The co… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
1
1

Citation Types

6
37
0

Year Published

2009
2009
2017
2017

Publication Types

Select...
7

Relationship

1
6

Authors

Journals

citations
Cited by 22 publications
(43 citation statements)
references
References 28 publications
(96 reference statements)
6
37
0
Order By: Relevance
“…The value of A ij for the CO 2 /H 2 O system is 0.04532 according to the reference results. k ij is fitted again in this work from the experimental data of gas‐liquid‐hydrate three‐phase equilibria of the CO 2 /H 2 O system, because the reference data were obtained at a high temperature without CO 2 hydrate existing. Figure and Equation show the relationship between k ij and the temperature.…”
Section: Calculationmentioning
confidence: 99%
“…The value of A ij for the CO 2 /H 2 O system is 0.04532 according to the reference results. k ij is fitted again in this work from the experimental data of gas‐liquid‐hydrate three‐phase equilibria of the CO 2 /H 2 O system, because the reference data were obtained at a high temperature without CO 2 hydrate existing. Figure and Equation show the relationship between k ij and the temperature.…”
Section: Calculationmentioning
confidence: 99%
“…Therefore, gas hydrate is somewhat of a "precipitate" form of gas that resides between dissolved gas saturation and free gas bubbles (Chen et al, 2006). Other research illustrating various relationships of Lw-H systems is available (Kim et al, 2008;Englezos, 2001, 2002;Zhang et al, 2008).…”
Section: Heterogeneous Nucleation Of Gas Hydratesmentioning
confidence: 98%
“…The temperature and pressure dependencies of the solubility of hydrate former in water are different at two-phase liquid water-vapor (L w -V) equilibrium and two-phase hydrate-liquid water (H-L w ) equilibrium [9][10]. The solubility of hydrate-former in water at L w -V equilibrium decreases with an increase in temperature at a given pressure, while at H-L w equilibrium the solubility in water increases with an increase in temperature [7,[10][11][12]. Two-phase H-L w equilibrium conditions can occur at the same high pressure and cold temperature conditions as the three-phase hydrate-liquid water-vapor (H-L w -V) equilibrium, which are common to Arctic regions, the deep sea, and underlying sediments.…”
Section: Introductionmentioning
confidence: 99%
“…Most of the available hydrate thermodynamic equilibrium experimental data are three-phase H-L w -V equilibria [1]. Experimental two-phase H-L w equilibrium data are comparatively scarce and limited to pure component methane, carbon dioxide, ethane and propane [1,7,[10][11][12]17]. To our knowledge there are no reliable experimental data on the solubility of hydrocarbon mixtures containing methane-ethane and propane in the aqueous phase at H-L w equilibrium.…”
Section: Introductionmentioning
confidence: 99%