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Handbook for Methane Control in Mining - AMMSA

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19MINE EXPLOSIONS, BAROMETRIC PRESSURE,AND THE SEASONAL EXPLOSION TRENDAlthough m<strong>in</strong>e explosions are far less common than <strong>in</strong> the past, this deadly hazard to m<strong>in</strong>ers hasnot disappeared. M<strong>in</strong>e operators must always be alert to the circumstances that make a m<strong>in</strong>eexplosion more likely. The chapter on dust explosions (Chapter 12) outl<strong>in</strong>es what must be doneto prevent a methane ignition from trigger<strong>in</strong>g a dust explosion, which is usually lethal. Twoother important factors, discussed here, are barometric pressure lows and drier dust <strong>in</strong> the w<strong>in</strong>ter.In South Africa, most m<strong>in</strong>e explosions have followed a low<strong>in</strong> the barometric pressure; however, there is no seasonalfrequency trend. In the United States, m<strong>in</strong>e explosions havebeen more frequent <strong>in</strong> the w<strong>in</strong>ter because the dust is drier.Barometric pressure lows and m<strong>in</strong>e explosions. Many researchers have documented an<strong>in</strong>verse relationship between barometric pressure and the amount of methane flow<strong>in</strong>g from am<strong>in</strong>e [Carter and Durst 1955; Stevenson 1968; Füssell and Hudewentz 1974; Eschenburg 1977].A fall<strong>in</strong>g barometric pressure causes expansion of the methane that has accumulated <strong>in</strong> undergroundcavities and crevices. The methane then flows <strong>in</strong>to the m<strong>in</strong>e, mak<strong>in</strong>g an ignition morelikely.Fauconnier [1992] has exam<strong>in</strong>ed the role of barometric pressure changes <strong>in</strong> South African m<strong>in</strong>eexplosions. Us<strong>in</strong>g barometric data correspond<strong>in</strong>g to 59 methane explosions (26 <strong>in</strong> coal, 33 <strong>in</strong>gold m<strong>in</strong>es) <strong>for</strong> the period 1970–1989, he concluded that most of the explosions were associatedwith medium-term (longer than 1 day) downward trends <strong>in</strong> barometric pressure. He also concludedthat explosions occur randomly dur<strong>in</strong>g the year, <strong>in</strong> contrast with U.S. coal m<strong>in</strong>es, whichare known to have a seasonal trend.The seasonal trend <strong>in</strong> U.S. coal m<strong>in</strong>e explosions. Historically, U.S. coal m<strong>in</strong>e explosions havebeen more frequent <strong>in</strong> the w<strong>in</strong>ter than the summer [Boyer 1964]. Although barometric pressuremight be a cause because changes <strong>in</strong> barometric pressure are more abrupt and <strong>in</strong>tense <strong>in</strong> thew<strong>in</strong>ter months, it is also true that m<strong>in</strong>es are drier <strong>in</strong> the w<strong>in</strong>ter because of the low moisture contentof the air [Williams 1914; Pappas et al. 2002]. This means that coal dust is drier and moreeasily dispersed and ignited dur<strong>in</strong>g the cold months.Accord<strong>in</strong>g to a study by Kissell et al. [1973], the second factor—drier coal dust—is the most<strong>in</strong>fluential <strong>in</strong> mak<strong>in</strong>g w<strong>in</strong>ter explosions <strong>in</strong> U.S. coal m<strong>in</strong>es more frequent. In this study, coalm<strong>in</strong>e accident reports from 1911 to 1970 were exam<strong>in</strong>ed to see whether w<strong>in</strong>ter explosions weremore likely to occur <strong>in</strong> regions of the m<strong>in</strong>e more susceptible to barometric pressure fluctuations(e.g., gobs). No such tendency was found. Next, based on the accident reports, explosions weredivided <strong>in</strong>to five different categories:

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