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Handbook for Methane Control in Mining - AMMSA

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10Figure 1–4.—Estimated methane content of coalversus depth and rank. Values shown are an upper limit.differences <strong>in</strong> coalbed depth, differences<strong>in</strong> production rate, and geological anomalies12 such as faults. Some of these correctionsare simple, if <strong>in</strong>exact. 13When no other m<strong>in</strong>e is nearby, a veryrough emission <strong>for</strong>ecast <strong>for</strong> the entirem<strong>in</strong>e may be obta<strong>in</strong>ed us<strong>in</strong>g the gascontent of the coal. For example, Saghafiet al. [1997] have reported the relationshipbetween gas content and m<strong>in</strong>e emission<strong>for</strong> Australian m<strong>in</strong>es (Figure 1–5). Theamount of methane released from the m<strong>in</strong>eexceeded the methane <strong>in</strong> the m<strong>in</strong>ed coalby a factor of 4. This differs from theresults of Kissell et al. [1973], whomeasured a factor of about 7 <strong>for</strong> someU.S. m<strong>in</strong>es. The difference is probablydue to methane emissions from adjacentcoalbeds and porous rock. Other associationsbetween m<strong>in</strong>e emission and gascontent have been made without us<strong>in</strong>gproduction data. Grau and LaScola [1984]have correlated the m<strong>in</strong>e emission of some U.S. m<strong>in</strong>es <strong>in</strong> cubic feet per day with the <strong>in</strong> situ gascontent <strong>in</strong> cubic feet per ton. 14Much more on <strong>for</strong>ecast<strong>in</strong>g <strong>for</strong> coal m<strong>in</strong>es is covered <strong>in</strong> thecoal m<strong>in</strong>e <strong>for</strong>ecast<strong>in</strong>g chapter (Chapter 8). Forecast<strong>in</strong>g<strong>for</strong> metal and nonmetal m<strong>in</strong>es is covered <strong>in</strong> this section.Forecast<strong>in</strong>g <strong>for</strong> tunnels is covered <strong>in</strong> the tunnel<strong>in</strong>g chapter(Chapter 14).12 The effect of geological anomalies is discussed <strong>in</strong> Chapter 7.13 Sometimes very <strong>in</strong>exact. For example, the methane emission can be assumed as roughly proportional to depth.However, Diamond and Garcia [1999] compared the methane emission rates of two longwall panels a mile apart.The second panel was 37% deeper than the first, but gave 61% higher emissions. The emissions were much higherbecause the elapsed time between development of the panel and retreat of the longwall face was much less <strong>in</strong> thesecond panel. Thus, there was less time <strong>for</strong> the second panel to dra<strong>in</strong> gas <strong>in</strong>to the returns, so when it was m<strong>in</strong>ed theemission was higher than expected.14 Grau and LaScola report 1980 m<strong>in</strong>e emission data. Reliable U.S. data after 1980 are not available. As degasificationprograms became widespread, the degas quantities were reta<strong>in</strong>ed as confidential <strong>in</strong><strong>for</strong>mation by coal companies.

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