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Origin of Gases in Coal Mines                                     219

           13.3.1 Proximate Analysis

           This analysis basically measures four constituents of coal as follows:
           1. Moisture
           2. Volatile matter
           3. Fixed carbon
           4. Ash
              American Standards for Testing Material (ASTM) uses the ash-freeefixed carbon
           and calorific value of coal to rank coal seams. Table 13.4 shows a complete list.
              International coal classification standards were developed by the Coal Committee
           of the Economic Commission for Europe. Table 13.5 shows both ASTM and European
           classifications side by side for ease in comparison.
              International system uses a three digit number to describe three different properties
           of the coal. The first digit shows the rank as shown in Table 13.5. The second digit
           shows the Roga index or free swelling index when coal is heated rapidly. The third
           digit shows the coking properties of metallurgical coal when it is heated slowly and
           is measured by Gray-King Coke index [5].

           13.3.2 Ultimate Analysis

           Ultimate analysis of coal breaks it into four elements: O 2 ,H 2 , C, and N 2 . Usually car-
           bon content increases with the rank of coal but H 2 and O 2 contents go down. Oxygen
           on dry, ash-free basis is used to determine the liability of coal to spontaneous combus-
           tion (discussed in Chapter 21).



           13.3.3 Rank of Coal Versus Vitrinite Reflectance, R o
           Vitrinite reflectance is a measure of percentage of incident light reflected from the
           surface of vitrinite particle/bands in coal seams. R o is usually an average of several
           readings. A typical coal seam has four megascopic bands known as vitrain, clarain,
           durain and fusain. Only vitrain is used for the ranking of coal (Table 13.6).



           13.4   Characterization of Methane from Coal

           Most coalbed methane (CBM) can be classified in two groups: (a) biogenic and
           (b) thermogenic. Low-rank coal usually contains methane of biogenic origin, whereas
           more mature, high-rank coals have thermogenic methane. Besides rank (or R o ), there
           are other indices that characterize CBM as either biogenic or thermogenic. Most
           important indices are listed below.


           13.4.1 Hydrocarbon Index
           It is defined as the ratio of CH 4 to (C 2 H 6 þ C 3 H 8 ).
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