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12.8  CO 2 Storage                                              383

            12.8.2 Coal Bed Methane Recovery

            Coal bed methane is the methane adsorbed in underground coals. Coal bed methane
            recovery is then a methane desorption process based on pressure swing desorption.
            The process is similar to EOR above; liquefied CO 2 is injected into a deep well,
            which is drilled into the coal bed, to reduce the hydrostatic pressure. As a result,
            methane is released from coal bed and transported to gas pipeline.
              CO 2 injection also results in enhanced methane recovery from coal bed methane
            by the competitive adsorption between CO 2 and methane. According to physical
            adsorption mechanisms, CO 2 and methane compete for the adsorption sites in the
            pores of the coal. As seen Fig. 12.9, coal adsorbs CO 2 more effectively than
            methane [37], this adsorption preference results in desorption of methane from the
            coal when CO 2 is injected into the coal bed. Liberated methane from the coal bed is
            also delivered to the surface facilities.
              Meanwhile, the replacement of methane with CO 2 on the pores of the coal also
            results in swelling of the coal matric and this may lead to reduced permeability, and
            consequent coal softening and more CO 2 injection in order to recover more
            methane.
              Cost-effective coal bed methane recovery requires high initial concentration of
            methane and adequate permeability for gas flow. Both depend on the pressure or
            depth of the coal bed: the deeper, the higher methane concentration but the lower
            permeability. This contradictory effect requires economical coal bed methane recovery
            to be executed at a depth in the range of 300–1,000 m or so.



            Fig. 12.9 Excess sorption
            isotherms of CO 2 and CH 4 in
            a coal (Data source Krooss
            et al. [37])
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