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Posted:
3 years ago
Aug 25, 2021, 4:46 a.m. EDT
Henry's law+diffusion in water.
Henry's law+diffusion in water.
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Posted:
3 years ago
Aug 25, 2021, 5:28 a.m. EDT
Thank you Lasse.
The problem is that for Henry's law implementation, I use the partition condition node as a boundary condition. Since this node prescribes the ratio between the concentration of CO2 in two different phases, I need to model the gas phase, too, besides the water phase. However, By considering a geometry for the gas phase I need to use a module for modeling its physics. So, I used again Transport of Diluted Species (tds) module for the gas phase which requires identification of diffusion coefficient (D). But considering a diffusion coefficient for the gas phase which consists of %100 CO2 does not have any physical meaning.
Thank you Lasse.
The problem is that for Henry's law implementation, I use the partition condition node as a boundary condition. Since this node prescribes the ratio between the concentration of CO2 in two different phases, I need to model the gas phase, too, besides the water phase. However, By considering a geometry for the gas phase I need to use a module for modeling its physics. So, I used again Transport of Diluted Species (tds) module for the gas phase which requires identification of diffusion coefficient (D). But considering a diffusion coefficient for the gas phase which consists of %100 CO2 does not have any physical meaning.
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Posted:
3 years ago
Sep 13, 2021, 5:18 a.m. EDT
Updated:
3 years ago
Sep 13, 2021, 5:57 a.m. EDT
There is no mass transfer in gas phase. Use mass balance and ideal gas law to estimate the pressure drop:
n° = n_gas + n_w = p·V_g/RT + V_w·c_w
p = Kc·c_w at the interface; Kc = Henry's law constant on the conc. scale.
n° = p°·V_g/RT; p° = initial pressure
How to implement the gas phase with Comsol, I have not checked.
But I calculated that assuming that the volume of water phase is much larger than that of the gas phase. This is what I got:
p/p° = exp(K²t)·erfc(K√t)
K = RT√D/[Kc·(V_g/A)] where A is the interfacial area of the gas-water interface, and D is the diffusion coefficient of CO2 in water.
Lasse
There is no mass transfer in gas phase. Use mass balance and ideal gas law to estimate the pressure drop:
n° = n_gas + n_w = p·V_g/RT + V_w·c_w
p = Kc·c_w at the interface; Kc = Henry's law constant on the conc. scale.
n° = p°·V_g/RT; p° = initial pressure
How to implement the gas phase with Comsol, I have not checked.
But I calculated that assuming that the volume of water phase is much larger than that of the gas phase. This is what I got:
p/p° = exp(K²t)·erfc(K√t)
K = RT√D/[Kc·(V_g/A)] where A is the interfacial area of the gas-water interface, and D is the diffusion coefficient of CO2 in water.
Lasse