Page 86 - Fundamentals of Gas Shale Reservoirs
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66   GEOCHEMICAL ASSESSMENT OF UNCONVENTIONAL SHALE GAS RESOURCE SYSTEMS

            This appears to be due to mixing and dilution by organic   Barker C. Pyrolysis techniques for source rock evaluation. AAPG
            lean sediments overlying organic‐rich shales.  The best   Bull 1974;58 (11):2349–2361.
            shales often have an organic‐lean carbonate overlying them,   Barker  C,  Takach NE.  Prediction of  natural  gas composition  in
            which functions as a seal and frac barrier. TOC, oil, and   ultradeep sandstone reservoirs. AAPG Bull 1992;76:1859–1873.
            pyrolysis yields, and T max  values are shown to be reduced   Baskin DK. Atomic H/C ratio of kerogen as an estimate of thermal
            with long‐term storage (20 years or more), whereas car­  maturity and organic matter conversion. AAPG Bull 1997;81:
            bonate contents increase. This suggests weathering‐induced   1437–1450.
            oxidation effects.                                   Behar F, Jarvie D. Compositional modeling of gas generation from
              Based on both experimental and empirical results, excess   two shale gas resource systems: Barnett Shale (United States)
            thermal maturity appears to reduce the amount of gas found   and Posidonia Shale (Germany).  AAPG Memoir 2013;103:
            in shale reservoirs.  This is hypothesized  to be  due to   25–44.
            oxidation of methane, but may also be due to destruction of   Behar F,  Vandenbroucke M. Experimental determination of the
            the porosity in the rock fabric and the subsequent loss of   rate constants of the n‐C  thermal cracking at 120, 400, and
                                                                                      25
            retained gas.                                          800  bar: implications for high‐pressure/high‐temperature
                                                                     prospects. Energy Fuels 1996;10:932–940.
              The top resource plays in North America are highly vari­
            able in terms of production due primarily to porosity and   Behar F, Lorant F, Lewan MD. Role of NSO compounds during
                                                                   primary cracking of a Type II kerogen and Type III lignite. Org
            pressure. Both porosity and pressure evolve in part from   Geochem 2008a;39:1–22.
            organic matter decomposition as the kerogen mass is con­  Behar F, Lorant F, Mazeas L. Elaboration of a new compositional
            verted to petroleum creating organoporosity and increased   kinetic schema for oil cracking. Org Geochem 2008b;39:
            pressure from petroleum cracking or gas generation.  The   764–782.
            shale gas system showing the lowest decline rate is the   Behar F, Roy S, Jarvie D. Artificial maturation of a Type I kerogen
            hybrid Montney Shale of the Western Canada Sedimentary   in closed system: mass balance and kinetic modelling. Org
            Basin.                                                 Geochem 2010;41 (11):1235–1247.
              Shale drilling has been completed safely and under envi­  Burnham  AK, Braun RL. Development of a detailed model of
            ronmentally sound operations in North America. There are   petroleum formation, destruction, and expulsion from lacustrine
            always concerns for safety and environment in all drilling   and marine source rocks, Advances in Organic Geochemistry
            operations, but with over 50,000 shale wells drilled over the   1989. Org Geochem 1990;16 (1–3):27–39.
            past 10 years a safe and sound track record is evident. In   Burnham AK, Gregg HR, Ward RL, Knauss KG, Copenhaver SA,
            cases where known geological conditions such as near pre­  Reynolds JG, Sanborn R. Decomposition kinetics and mecha­
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            existing intraplate plates, saltwater disposal wells should   nism of n‐hexadecane‐1,2‐ C  and dodec‐1‐ene‐1,2‐ C  doped
                                                                                                           2
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            either not be drilled or handled differently. Regulations for   in petroleum and  n‐hexadecane. Geochim  Cosmochim  Acta
            cementing of casing protecting freshwater aquifers should   1997;61 (17):3725–3737.
            always be updated for any changes in known operational or   Claypool GE, Mancini EA. Geochemical relationships of petro­
            geological conditions just as safety measures are taken in   leum in Mesozoic reservoirs to carbonate source rocks of
            any other industry.                                    Jurassic Smackover formation, Southwestern Alabama. AAPG
              Overall, shale gas resource systems provide a remark­  Bull 1989;73:904–924.
            able energy resource that is the best carbon‐based resource   Cooles  GP,  MacKenzie AS,  Quigley TM.  Calculation  of  petro­
            that we have in terms of carbon dioxide and other emissions   leum masses generated and expelled from source rocks.
            as well as being quite inexpensive over the course of the   Advances in Organic Geochemistry 1985. Org Geochem
                                                                   1986;10 (1–3):235–245.
            last 100 years. It represents a solution to reduced energy
            dependence, if not near complete independence for North   Dahl JEP, Moldowan JM, Moldowan S. Determination of thermal
                                                                   maturity and extent of oil cracking in tight shales using extract
            America. Hopefully, this resource can be adequately and   biomarker and diamondoid concentrations and distributions.
            safely tapped elsewhere to provide comparable energy   Unconventional Resources Technology Conf (URTeC), URTeC
            benefit to global energy consumers.                    paper 1574980; 2013. 5 p.
                                                                 di Primio R, Horsfield B, Guzman‐Vega MA. Determining the tem­
                                                                   perature of petroleum formation from the kinetic properties of
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