(127b) Carbon Storage and Methane Production Via Permafrost Gas Hydrate Deposits | AIChE

(127b) Carbon Storage and Methane Production Via Permafrost Gas Hydrate Deposits



Carbon Dioxide Storage and Natural Gas Production via Gas Hydrate Exchange Process: Down Hole Combustion Thermal Stimulation

AIChE 2013 Spring Meeting, April 28-May 2. Hyatt, San Antonio, Texas

Garrett C Fitzgerald, Marco J. Castaldi

Department of Earth and Environmental Engineering, Columbia University, 550 W 120 St., Room 926, New York, NY 10027

Methane hydrates present a vast potential for future alternative natural gas resources and have the unique ability to be combined with CO2 sequestration to produce a carbon neutral CH4 fuel source.  CO2 forms a stable gas hydrate in the same pressure –temperature environment that naturally occurring CH4 hydrates exist and can be exploited for an exchange process.  This work investigates the exchange process of simulated combustion gasses (CO2 and N2) with CH4 in hydrate bearing porous media systems.  Porous sediments are prepared with CH4 hydrate saturations of 50% pore volume and exposed to pure CO2, and variousCO2-N2 gas mixtures while being subjected to a point heat source for assisted hydrate dissociation.  This work will present the gas exchange potential of both pure CO2 and CO2 –N2 blends at various heating rates and exchange conditions.  The production of CH4 is used as a metric to evaluate energy potential of this gas production method, and the extent of gas exchange is used to quantify the degree of carbon intensity of the end use CH4 fuel. CH4 production rates via the gas exchange methods are compared to those produced via thermal stimulation alone without the co-injection of any exchange gas as a baseline for benefits/challenges associated with CO2 storage in CH4 hydrate bearing porous sediment deposits. Multiple CO2 injection rates are investigated where flow rates range from the lower limit as the amount of CO2 that would be released for a given amount of heat energy (CH4 as a fuel) input to the upper limit where enough CO2 is injected to replace all available CH4 hydrate in the formation. The benefits of using N2 as a co-injectent are relatively unknown in the literature and are proposed to enhance the maximum exchange potential and subsequently produce a greater percentage of the in place CH4.  The results of these experiments should present a better understanding of associated N2 potential benefits as well as quantify the ideal blend mixtures to achieve the highest gas exchange efficiency.