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182                          Advances in Productive, Safe, and Responsible Coal Mining

         In general, coal can store about six to seven times more methane than the equivalent
         volume of rock in a conventional reservoir.
            From the author’s viewpoint, it is possible to categorize gases derived from coal
         mines into four key forms: (i) coal mine methane (CMM) or working mine methane
         (WMM), (ii) coal seam methane (CSM) or coal bed methane (CBM) collected from
         unmined coal beds, (iii) abandoned mine methane (AMM) drained from depleted or
         inactive mines, and (iv) syngas from underground coal gasification (UCG) by which
         coal is gasified in situ.
            As mentioned, CMM is a general term for all methane released mainly during and
         after coal-mining operations. Therefore, CMM is a type of coal gas present in active
         working mine sites, and may be captured through a drainage system or vented from
         coal mines by a ventilation system; i.e., ventilation air methane (VAM). In drainage
         systems, CMM may be captured via surface vertical premining boreholes, horizontal
         premining boreholes ahead of the coal face, or postmining wells drilled into the
         gob area.


         10.2.1 Methane chemistry
         Methane is a colorless, odorless, tasteless, and flammable chemical compound with
         the chemical formula CH 4 . Methane is the second most abundant GHG accounting
         for about 15% of global GHG emissions produced by human activities and is respon-
         sible for more than a third of total anthropogenic radiative forcing. Methane is more
         than 20 times more effective at trapping heat than CO 2 , making it one of the most
         potent GHGs.
            Methane is lighter than air, having a specific gravity of 0.554. It is only slightly
         soluble in water. It burns readily in air, forming CO 2 and water vapor; the flame is
         pale, slightly luminous, and very hot. The boiling point of methane is  161.5°C
         (258.7°F) and the melting point is  182.5°C (296.5°F) [5]. Methane is not toxic when
         inhaled, but it can produce suffocation by reducing the concentration of oxygen
         inhaled. In general, methane is very stable, but mixtures of methane and air, with
         the methane content between 5% and 15% by volume, are explosive. Explosions of
         such mixtures have been frequent in coal mines, causing many disasters worldwide.
         It is worth mentioning that methane content more than 15% may not necessarily be
         explosive.
            Even though methane-air mixtures under 5% are not explosive, a considerable mar-
         gin of safety must be provided (usually to less than 2%) due to the compounding effect
         of coal dust. An effective mine ventilation system will therefore ensure that the vol-
         ume of gas mixture is minimized below the explosive range in a safe level (usually less
         than 1% or up to 1.25%). In addition, due to the fact that inert gases such as nitrogen or
         CO 2 cannot chemically react with methane, they can be added to an explosive
         methane-air mixture to make it nonexplosive [4].
            Methane, which is also known as methyl hydride, is a group 14 hydride and the
         simplest alkane, a series of hydrocarbons. It is the main constituent of natural gas.
         In coal mining, methane is the main constituent of marsh gas (swamp gas) and fire-
         damp (flammable gas), and may be captured commercially from gaseous coal seams
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