Features of hydrate formation in porous formations during gas blowing

2012 ◽  
Vol 9 (1) ◽  
pp. 72-75
Author(s):  
I.K. Gimaltdinov ◽  
M.K. Khasanov ◽  
M.V. Stolpovsky ◽  
S.R. Kildibaeva

Theoretically, the processes of gas hydrate formation in gases saturated with gas and water porous media of finite length when they are blown with cold gas. The influence of initial parameters of the porous medium, as well as blowdown conditions on the features of the evolution of the hydration-saturation fields and temperature. It is shown that for some parameters of the injected gas, the boundary can be stopped phase transition.

The purpose of this paper is to study the thermodynamic modeling of the conditions for methane and ethane gas hydrate formation and their mixtures in a porous and non-porous environment. In this paper, the Van der Waals- Platteeuw thermodynamic model was used for prediction of gas hydrate formation conditions. Also, the SRK and PTV equations of state were used for calculations of driving force. In this research, the results of thermodynamic modeling in a porous were compared with the non-porous environment and laboratory data in the literature. Studies have shown that the results of the modeling are in good agreement with the laboratory data and the percentage of errors is low. The results also showed that with increasing pressure of porous and non-porous media, the equilibrium temperature increases. In addition, the effect of the pore diameter of porous media on the results of modeling was investigated for methane, ethane and their mixtures during gas hydrates formation. The results showed that by increasing the pressure for any size of the pore diameter of the porous medium, hydrate formation temperature increases. In addition, by increasing the pore diameter of the porous medium, hydrate formation temperature methane, ethane and their mixture increase at a constant pressure. The results also showed that the equilibrium temperature of the non-porous medium is higher than the equilibrium temperature of the non-porous medium. This shows that the hydrate formation in the porous medium has a deterrent effect and leads to lower temperatures and higher temperatures conditions for gas hydrate formation. The results showed that by increasing the percentage of methane in a porous or non-porous medium, the temperature of hydrate formation of the binary gas mixture of methane and ethane decreases.


2016 ◽  
Vol 11 (2) ◽  
pp. 233-239 ◽  
Author(s):  
V.Sh. Shagapov ◽  
A.S. Chiglintseva ◽  
S.V. Belova

Considered the problem of gas hydrate formation during injection of cold gas in the snow massif, initially saturated with the same gas. In work some limited scheme according to which, intensity of hydrate formation is limited by diffusion of gas through the hydrate layer formed between the phases of gas and ice, to the boundary of contact ice-hydrate, and is determined by the introduction of only one parameter the given diffusion coefficient. Shows the distributions of pressure, temperature, hydrate saturation and the saturation of the snow at different points in time. Held influence analysis of the effect of the pressure of the injected gas and the permeability of the snow massif on the intensity of hydrate formation.


1999 ◽  
Vol 38 (6) ◽  
pp. 2485-2490 ◽  
Author(s):  
Matthew A. Clarke ◽  
Mehran Pooladi-Darvish ◽  
P. Raj Bishnoi

2008 ◽  
Vol 6 ◽  
pp. 178-183
Author(s):  
M.K. Khasanov ◽  
N.G. Musakaev

The features of the gas hydrates formation at the gas injection into the porous medium initially saturated with gas and water are considered. Self-similar solutions of the axisymmetric problem describing the distribution of the main parameters in a reservoir are constructed. The solutions have been found according to which the gas hydrate formation can occur at the frontal surface or in the extended area.


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