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350                                        12  Carbon Capture and Storage

              Table 12.1 gives six leading GHGs that are under discussion in international
            climate change negotiations: CO 2 ,N 2 O, CH 4 , hydrofluorocarbons (HFC), perflu-
            orocarbons (PFC), and sulfur hexafluoride (SF 6 ). All the GHGs do not contribute
            equally to the global climate change, therefore, global warming potential (GWP) is
            used to quantify the contribution to global warming for a unit mass of greenhouse
            gas, taking carbon dioxide as a reference with GWP = 1. More detailed information
            such as the calculation of GWP and lifetime of GHGs can be found in the IPCC
            [32] Report. The GWPs of other GHGs are higher than CO 2 , due to difference in
            lifetime and radiation absorption behavior in the atmosphere. For example, the
            GWP of SF 6 is 23,900 times that of CO 2 due to its great stability and persistence. Its
            lifetime in atmosphere is estimated to be 3,200 years, making it the strongest GHG
            known today.
              However, over all CO 2 is responsible for most of the greenhouse effect, only
            second to water vapor, due to its large total quantity. SF 6 contributes to approxi-
            mately 0.1 % of the enhanced greenhouse effect.
              CH 4 emissions mainly result from landfills, agriculture, coal mining, oil, and gas
            handling and processing. One of the solutions to this problem is to capture the CH 4
            emission in a controlled environment, e.g., an anaerobic digester, and burn it into
            CO 2 to reduce its greenhouse effect. The chemical reaction is described as

                                 CH 4 þ 2O 2 ! CO 2 þ 2H 2 O             ð12:1Þ

              This reaction shows that one mole of CH 4 produces the same mole amount of
            CO 2 . It, however, reduces the greenhouse effect by 20 times. And this is also the
            motivation behind flaring in the oil and gas industry.
              N 2 O emissions result from agriculture, chemical plants such as nitric acid or
            nylon processing units, and combustion processes. Fluidized bed combustion
            (FBC) is the most problematic with respect to N 2 O emissions. Coal-fired FBC emits
            50–150 times higher N 2 O than pulverized coal firing plants. Vehicles emit more
            N 2 O than stationary sources; a typical passenger car emits 20 mg/km N 2 Oin
            addition to 50 mg/km CH 4 .
              HFCs and PFCs are synthetic chemicals, produced as alternatives for the ozone-
            depleting chlorofluorocarbons (CFCs) in response to the “phase out” of CFCs under
            the Montreal protocol of 1987. HFC-134a is the major substitute for CFCs in
            refrigerators.


            Table 12.1 Six leading  GHG name            Formula      GWP
            GHGs and their GWPs
            (excluding water vapor)  Carbon dioxide     CO 2         1
                                  Methane               CH 4         21
                                  Nitrous oxide         N 2 O        310
                                  Hydrofluorocarbons     HFC          140–11,700
                                  Perfluorocarbons       PFC          7,400
                                  Sulfur hexafluoride    SF 6         23,900
                                  Source EIA [21]
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