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Handbook for Methane Control in Mining - AMMSA

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103Figure 7–4.—<strong>Methane</strong> dra<strong>in</strong>age of a reverse fault from the“hang<strong>in</strong>g” wall side.Jo<strong>in</strong>ts, cleats, and fractures.Jo<strong>in</strong>ts, cleats, and fractures areubiquitous features <strong>in</strong> most coalmeasure rocks and are related tothe conf<strong>in</strong><strong>in</strong>g stress fields act<strong>in</strong>gupon those strata dur<strong>in</strong>g burial,diagenesis, and uplift. Generally,these features follow asystematic pattern. Jo<strong>in</strong>ts areclosely spaced with even walls,whereas fractures are morewidely spaced with irregularwalls [Nickelsen and Hough1967]. Jo<strong>in</strong>ts usually occur <strong>in</strong>orthogonal pairs (at an approximately90° orientation to eachother), and <strong>in</strong> coalbeds, thesejo<strong>in</strong>t sets are referred to as“cleats.”Figure 7–5.—<strong>Methane</strong> dra<strong>in</strong>age of a reverse fault from the“footwall” side.The ma<strong>in</strong> jo<strong>in</strong>ts and cleats of anygiven set are generally morecont<strong>in</strong>uous and are the dom<strong>in</strong>antmigration pathways <strong>for</strong> gas[McCulloch et al. 1974]. Theyare referred to as “systematicjo<strong>in</strong>ts” and “face cleats,” respectively.The correspond<strong>in</strong>g jo<strong>in</strong>tsand cleats at 90° to the ma<strong>in</strong>features are referred to as“nonsystematic jo<strong>in</strong>ts” and “buttcleats,” respectively. Thesejo<strong>in</strong>ts and cleats generally term<strong>in</strong>ateaga<strong>in</strong>st the systematic jo<strong>in</strong>tsand face cleats, mak<strong>in</strong>g themnotably less cont<strong>in</strong>uous. Whencoalbeds are m<strong>in</strong>ed, the redistribution of stresses allows cleats to expand and facilitates gasmigration through the coal to the face. Similarly, the stress redistribution opens jo<strong>in</strong>ts andfractures <strong>in</strong> roof and floor strata, facilitat<strong>in</strong>g gas migration from adjacent strata.The ubiquitous nature of jo<strong>in</strong>ts and the unpredictable spac<strong>in</strong>g of fractures make prediction andremediation of abnormal gas emissions related to these features difficult. It is important <strong>for</strong>operators to realize that although jo<strong>in</strong>ts and fractures may conta<strong>in</strong> free gas at the face, their realhazard potential is as a conduit <strong>for</strong> unexpected gas flows to the m<strong>in</strong>e work<strong>in</strong>gs from with<strong>in</strong> thecoalbed and/or other source beds adjacent to the m<strong>in</strong>ed coalbed. These types of conditions aremost often recognized when the cont<strong>in</strong>uous m<strong>in</strong>er or longwall shearer is deenergized due to themach<strong>in</strong>e-mounted methane sensors read<strong>in</strong>g concentrations above the allowable limits. The most

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