Page 68 - Fundamentals of Gas Shale Reservoirs
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48   GEOCHEMICAL ASSESSMENT OF UNCONVENTIONAL SHALE GAS RESOURCE SYSTEMS

            it is absolutely necessary to stimulate or fracture a sufficient   to be enforced, but are often based on outdated information.
            volume of rock to release large volumes of gas. In general,   As such, they should be continually evaluated for their
            recoveries from these systems range from 10 to about     efficacy with regard to present‐day drilling operations and
            20%  of  the  gas  in  place  (GIP),  although  higher  numbers   updated as necessary.
            are often cited.                                       As shale gas development requires hundreds to thousands
              Gas flow requires not only large amounts  of GIP and   of wells, this also puts a strain on infrastructure such as roads
            sufficient storage but also a brittle rock fabric as well as exten­  and water use when wells are stimulated with freshwater.
            sive knowledge of rock mechanics and stress fields in the   Noise pollution is likely a large concern albeit over a short
            prospect area to enable stimulation of sufficient volume of   period of time. Both can be dealt with by appropriate actions
            rock. Even with high‐energy stimulation, the typical shale gas   of governments and drilling operations.
            well will ultimately produce only a few billion cubic feet (bcf)   Seismic activity or small‐scale earthquakes have also
            of gas, and as such, requires drilling hundreds to thousands of   been associated with shale gas development, although it is
            wells to recover large amounts of gas, for example, over   actually saltwater disposal wells that  have caused such
            15,000 wells have been drilled into Barnett Shale gas reser­    seismicity. When disposal wells are drilled near preexisting
            voirs to date yielding about 15 tcf of gas. Prospective shale   faults, low‐magnitude  earthquakes can  occur. One of the
            gas areas may be located beneath commercial and residential   most widely reported seismic events occurred at the Dallas/
            areas limiting drilling access. Where such plays are located in   Fort Worth (DFW) Airport in 2008–2009, having a maximum
            areas where drilling costs are extremely high, the economics   moment magnitude scale (M  or M) of 3.3 and was likely
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            of drilling a gas well(s) to produce a few bcf of gas may not be   due to injection of saltwater into a disposal well (Frolich and
            commercially viable at a given price level. Low natural gas   Potter,  2013).  However,  these  authors  also  reported  that
            prices (ca. $3.69/mcf on average in 2013) in North America   more than a decade before this event (1997), a M3.4 natural
            have currently resulted in diminished drilling of shale gas   earthquake occurred within 100 km (ca. 62 miles) of DFW
            wells except in high‐return areas such as the Marcellus Shale   Airport. Frolich and Potter (2013) proposed five hypotheses
            of the Appalachian Basin, Northeastern United States.  for the origin and nature of small intraplate earthquakes as
              The search for shale gas outside of North America has   might be originated from saltwater injection wells. They cite
            identified promising shale gas systems, but to date has only   that the consensus of earthquake seismologists agrees that
            resulted in marginal commercial success. However, the ear­  small earthquakes (ca. M2.0) are ubiquitous and not indica­
            liest wells are typically the most expensive and least pro­  tive of the occurrence or onset of larger earthquakes. Often
            ductive, but as companies learn what is necessary to obtain   increased seismicity is related to increased recording stations
            high gas flow from a given system, commercial development   being deployed, so many more low‐level quakes are recorded.
            often follows.                                       They also cite that all 50 states in the United States experi­
              In addition, there has been much resistance to drilling   ence earthquakes, but are small and go undetected. In Texas,
            such wells that require high‐energy stimulation that has   most M3.5 earthquakes go unrecorded unless near areas of
            often cited as concern for the environment, which is a con­  dense population where seismographs are located (Frolich
            cern for all including the companies hoping to develop such   and Potter, 2013).  Avoidance of injection well‐induced
            a system. Commercial success requires environmental suc­  earthquakes can be accomplished by understanding regional
            cess too, otherwise development would be halted. Operations   stress patterns and not locating such wells in areas with
            in  North America  have  been  safe  with  over  60,000  shale     preexisting faults (Frolich and Potter, 2013).
            resource wells drilled and stimulated. While groundwater   The societal and political power of developing shale gas
            contamination has occurred by ongoing geological processes   resources in a friendly and environmentally sound manner is a
            and are often reported in shallow water wells prior to drilling   tremendous asset in terms of supplying energy needs and also
            shale gas wells, these have often been cited as being derived   reducing carbon dioxide levels. Natural gas is the most envi­
            from the high‐energy stimulation efforts. Shale gas reser­  ronment‐friendly carbon‐based energy source as combustion
            voirs  are  often  at  depths  from  6000  to  15,000 ft  or  more,   emits lower carbon dioxide and other oxide emissions. The
            which is one to three miles below the nearest freshwater   major source of carbon dioxide emissions in the United States
            aquifers. Adequate and effective regulations on cementing   is electricity generation, and reduction of CO  emissions is
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            and testing of the upper portion of the well bore where it   due in part to increased implementation of gas‐fired power
            passes through freshwater aquifers should be the focus of   plants. In 2012, the United States had its lowest carbon dioxide
            tighter regulation. For example, the largest and most tragic   emissions in over 20 years (EIA, 2012). Natural gas power is
            oil field operation in recent time has been the massive blow   certainly not a green solution as there remains a carbon foot­
            out in the Gulf of Mexico, where the casing cement job was   print; however, it does give us additional time to develop
            the cause of various failures and also likely improper well   green energy resources. Shale gas is a tremendous resource
            testing (National Commission on the BP Deepwater Horizon   for our ongoing energy needs resulting in lower emissions
            Oil Spill and Offshore Drilling, 2011). Regulations need   and lower costs for both consumers and industrial concerns.
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