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Handbook for Methane Control in Mining - AMMSA

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152• In Eastern Europe, petroleum and gas has been observed <strong>in</strong> igneous and metamorphicrocks <strong>in</strong> Yugoslavia, <strong>in</strong> some copper m<strong>in</strong>es <strong>in</strong> Hungary, and <strong>in</strong> mica schists conta<strong>in</strong><strong>in</strong>glimestone <strong>in</strong>trusions <strong>in</strong> Romania.• In the United K<strong>in</strong>gdom, granites <strong>in</strong> Cornwall and Aberdeen and iron ore deposits <strong>in</strong>Cleveland all report hydrocarbon gases associated with overly<strong>in</strong>g bitum<strong>in</strong>ous shales.Also, Derbyshire lead m<strong>in</strong>es have reported methane along with bitumen.• Canadian Shield m<strong>in</strong>es conta<strong>in</strong> methane, other hydrocarbons, and sometimes hydrogenand helium [Fritz et al. 1987; Andrews 1987]. These are widespread and occur <strong>in</strong> almostall the m<strong>in</strong>es, particularly where carbonaceous materials are found <strong>in</strong> the rocks. Theemissions are usually associated with boreholes [Sherwood et al. 1988] and are relativelyshort-lived and easily dissipated. The Kidd Creek m<strong>in</strong>es have methane pockets associatedwith sulfide deposits. At some m<strong>in</strong>es, the occurrences of methane and hydrogen<strong>in</strong>crease with depth, and the result<strong>in</strong>g gas mixtures reduce the lower explosive limit to aslow as 4.5%. 4 The Ontario M<strong>in</strong>istry of Labour (OML) has approximately eight reportsper year of combustible gas <strong>in</strong> an underground work<strong>in</strong>g place [OML 1996]. Thesereports are almost always <strong>for</strong> boreholes, with measured concentrations of 0.1%–10%.Gas is very seldom detected <strong>in</strong> the general body of the m<strong>in</strong>e’s atmosphere, althoughmethane ignitions due to cigarette smok<strong>in</strong>g and friction between metal and sandstonehave been reported to the OML.• U.S. m<strong>in</strong>es report methane emissions associated with oil shales, salt, trona, potash, limestone,copper, and uranium ores.• In Australia, hydrocarbon gases are reported from copper m<strong>in</strong>es and from Precambrianrocks at Kalgoorlie. The usual type of methane encounter is a diamond drill blower andmethane is readily dispersed.• The Republic of South Africa has combustible gases <strong>in</strong> almost all gold and plat<strong>in</strong>umm<strong>in</strong>es, as well as kimberlite pipes. Along with the methane, there can be hydrogen andhelium. The usual assumption is that the methane is associated with overly<strong>in</strong>g Karoostrata, which are coal-bear<strong>in</strong>g [Searra 1990; Eschenburg 1980; Jackson 1957]. The gas istransported downward through the rock dissolved <strong>in</strong> water.REGULATIONS FOR GASSY METAL/NONMETAL MINESIN THE UNITED STATESThe United States developed new federal standards <strong>for</strong> controll<strong>in</strong>g methane hazards <strong>in</strong> metal/nonmetal m<strong>in</strong>es <strong>in</strong> 1985. These are conta<strong>in</strong>ed <strong>in</strong> 30 CFR 5 57, Subpart T—Safety Standards <strong>for</strong><strong>Methane</strong> <strong>in</strong> Metal and Nonmetal M<strong>in</strong>es. Consider<strong>in</strong>g that there is such a wide variety of metal/nonmetal m<strong>in</strong>es <strong>in</strong> the United States, these standards are quite comprehensive and detailed.4 For more <strong>in</strong><strong>for</strong>mation on the lower explosive limit, see Chapter 1.5 Code of Federal Regulations. See CFR <strong>in</strong> references.

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