(728h) Replacement of CH4 in the Hydrate By CO2 and N2 for Methane Recovery and Carbon Dioxide Sequestration: A Modeling Approach | AIChE

(728h) Replacement of CH4 in the Hydrate By CO2 and N2 for Methane Recovery and Carbon Dioxide Sequestration: A Modeling Approach

Authors 

Bhawangirkar, D. - Presenter, Indian Institute of Technology Bombay
Sangwai, J., Indian Institute of Technology Madras

Replacement of CH4
in the hydrate by CO
2
and N
2
for methane recovery and carbon dioxide sequestration: A Modeling
Approach

Dnyaneshwar R. Bhawangirkar1,2, Jitendra S. Sangwai2*

1Department of Chemical Engineering, Indian Institute of
Technology Bombay, Powai, Mumbai 400076, India

2Gas Hydrate and Flow Assurance Laboratory, Petroleum
Engineering Program, Department of Ocean Engineering, Indian
Institute of Technology Madras, Chennai 600036, India




Keywords: Gas hydrates; Thermodynamic modeling; High pressure phase
equilibria

ABSTRACT

The
replacement mechanism is considered as one of the emerging techniques
for methane gas recovery from the hydrate reservoirs by sequestering
carbon dioxide deep in the oceans mitigating the climate change, and
also by retaining the original form of the hydrate reservoir avoiding
any catastrophic geo-mechanical hazards such as landslides or
earthquakes. When methane (CH4) hydrate reservoir is
exposed to carbon dioxide (CO2) gas, the in situ exchange
of methane gas molecules trapped in the hydrate phase is forced to
happen with CO2 molecules. The CO2 molecule is
large in size than the CH4 molecule, resulting in more
affinity towards the larger cages of the hydrate. Hence, CO2
molecules prefer to replace most of the CH4 molecules from
the larger cages of the hydrate, leaving behind CH4
molecules in small cages almost intact. Now, to increase the methane
gas production; it is necessary to introduce new small size gas
molecules which can replace CH4 gas molecules left behind
in the small cages of the hydrate. Nitrogen (N2) molecule
is smaller in size than a CH4 molecule, and it will have
more affinity towards smaller cages of the hydrate. Adding N2
along with CO2 will serve the purpose of replacing most of
the CH4 gas molecules form both small as well as large
cages of the hydrate.

However, it is very important to understand at what ratio the N2/CO2
gas mixture needs to be injected into the hydrate reservoir. When CO2
and N2 gas mixture is injected into the hydrate reservoir,
it forms a mixed hydrate. Therefore, we have made use of Klauda and
Sandler’s thermodynamic model to understand the distribution of gas
molecules in the hydrate phase. This model utilizes the concept of
equal fugacities of water in the hydrate phase to that in the liquid
phase. The Peng-Robinson-Stryjek-Vera equation of state is used for
evaluating the vapour phase fugacity. Fugacity has found to be
increasing with the increase in temperature. Liquid phase activity
coefficients are determined by using a modified UNIFAC method.

We
have used a total of 109 experimental data points having a different
composition of CH4+CO2+N2 for
calculating the equilibrium pressures from the model, and found that
the percent absolute average deviation is 6.46%. The cage occupancy
which is a function of Langmuir constant and fugacity is being
calculated to know the distribution of gas molecules in the hydrate
phase at equilibrium. We have observed most of the small cages are
occupied by N2 and CH4 molecules; displaying
the competitive behavior of N2 and CH4
molecules to occupy smaller cages of the hydrate; whereas the
competition between CO2 and CH4 molecules is
observed to occupy large cages of the hydrate. We found that the
occupancy of N2 molecules in smaller cages of the hydrate
is ~20 times larger than in large cages revealing the capability of
N2 molecules to replace most of the CH4
molecules from the small cages of the hydrate. We also observed that
the occupancy of CO2 molecules in larger cages is much
higher than in small cages which will certainly help in replacing
most of the CH4 gas molecules from the larger cages of the
hydrate. The also observed that with the increase in N2/CO2
ratio and at constant CH4 composition, the total occupancy
of N2+CO2 has found to decrease in the hydrate
phase, and CH4 molecules in the hydrate phase have found
to be increased. This information helped us in deciding the N2/CO2
gas ratio to be injected into the hydrate reservoir for better
recovery of methane gas. We conclude that a 1:3 ratio of N2/CO2
gas mixture is a good choice to be injected into the hydrate
reservoirs for more methane gas production maintaining the higher CO2
gas sequestration deep into the ocean reservoir.