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Handbook for Methane Control in Mining - AMMSA

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techniques rely on match<strong>in</strong>g the actual gas production data plots (prepared with the same set ofunits and graphical <strong>for</strong>m as <strong>in</strong> the type-curves) to the theoretical curves. These techniques canalso be used to analyze production decl<strong>in</strong>e curves to predict rema<strong>in</strong><strong>in</strong>g gas-<strong>in</strong>-place and futureemissions <strong>for</strong> m<strong>in</strong>e safety assessments [Chen and Teufel 2000]. In addition, if the gas productionis exclusively from the coalbed to be m<strong>in</strong>ed, type-curve analysis can provide other reservoir<strong>in</strong><strong>for</strong>mation that needs to be determ<strong>in</strong>ed <strong>for</strong> emission <strong>for</strong>ecast<strong>in</strong>g studies (e.g., model<strong>in</strong>g).In summary, type-curves can contribute to:• Stimulation (fractur<strong>in</strong>g) effectiveness diagnosis• Recovery efficiency (recovery factor based on <strong>in</strong>itial gas-<strong>in</strong>-place)• Estimation of reservoir flow properties (permeability, flow capacity, etc.)• Reservoir storage properties• Future prediction of production119Both production decl<strong>in</strong>e analysis and type-curve match<strong>in</strong>gtechniques can be used to analyze methane dra<strong>in</strong>ageboreholes <strong>for</strong> future production rates and thus predict therema<strong>in</strong><strong>in</strong>g gas-<strong>in</strong>-place at the time of m<strong>in</strong><strong>in</strong>g. However,gas emissions from different gas sources may becomm<strong>in</strong>gled, especially dur<strong>in</strong>g longwall m<strong>in</strong><strong>in</strong>g.There<strong>for</strong>e, one can expect higher emission rates dur<strong>in</strong>gm<strong>in</strong><strong>in</strong>g compared to what is predicted by the analysis.PREDICTING GAS EMISSIONS DURING MININGThe ma<strong>in</strong> sources <strong>for</strong> gas (generally predom<strong>in</strong>antly methane) that can be released <strong>in</strong>to the undergroundm<strong>in</strong>e work<strong>in</strong>gs are the m<strong>in</strong>ed and adjacent coalbeds and other surround<strong>in</strong>g gas-bear<strong>in</strong>gstrata [Mucho et al. 2000; Diamond et al. 1992]. M<strong>in</strong><strong>in</strong>g activities disturb the exist<strong>in</strong>g stressequilibrium <strong>in</strong> the rock mass and create changes to the structural <strong>in</strong>tegrity of the affected strata.The m<strong>in</strong><strong>in</strong>g processes can thus create sudden and unstable gas problems, which may <strong>in</strong>crease therisk of an explosion <strong>in</strong> the underground workplace. Gas flow from these sources is <strong>in</strong>itiated andma<strong>in</strong>ta<strong>in</strong>ed by differential pressures between the source (higher pressure) and the m<strong>in</strong>e work<strong>in</strong>gs(lower pressure). The flow paths are both the naturally occurr<strong>in</strong>g rock jo<strong>in</strong>ts, faults, and coalcleat, as well as m<strong>in</strong><strong>in</strong>g-<strong>in</strong>duced fractures <strong>in</strong> the surround<strong>in</strong>g strata.It is generally observed that the amount of gas released dur<strong>in</strong>g the m<strong>in</strong><strong>in</strong>g process is greater thanthat conta<strong>in</strong>ed <strong>in</strong> the actual volume of coal m<strong>in</strong>ed at the face [Kissell et al. 1973]. This apparentdiscrepancy is due to the cont<strong>in</strong>ual emission of gas from the coal that is left <strong>in</strong> place as ribs andpillars, as well as the migration of gas from the surround<strong>in</strong>g strata, <strong>in</strong>clud<strong>in</strong>g the longwall gob[Mucho et al. 2000]. <strong>Methane</strong> emission rates change over time <strong>in</strong> the life cycle of a m<strong>in</strong>ebecause of the <strong>in</strong>teraction of variable geotechnical, m<strong>in</strong>e design, and operational factors. Thefollow<strong>in</strong>g mathematical <strong>for</strong>mula by Lunarzewski [1998] addresses this phenomenon and calculatesthe quantity of gas released <strong>in</strong>to a m<strong>in</strong>e dur<strong>in</strong>g various stages <strong>in</strong> the life of a m<strong>in</strong>e:

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