13.07.2015 Views

Handbook for Methane Control in Mining - AMMSA

Handbook for Methane Control in Mining - AMMSA

Handbook for Methane Control in Mining - AMMSA

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

coalbed is assumed, as is the case <strong>for</strong> Figure 8–3. Above the coalbed from 0 to 66 ft (20 m) andbelow the coalbed from 0 to -36 ft (-11 m), the degree of gas emission is assumed to be 100%.Because these curves are empirical correlations or standard assumed degrees of emissions, theremay be considerable variations when they are applied to other locations. As always, it should beremembered that the best <strong>in</strong><strong>for</strong>mation <strong>for</strong> prediction is the measured data and the derived empiricalcorrelations at a specific site of <strong>in</strong>terest.On the other hand, if the roof and floor have not been fractured be<strong>for</strong>e, the prediction can bebased on gas pressure, and thus a rema<strong>in</strong><strong>in</strong>g gas content. In this case, the proportion of gasemitted depends on the gas pressure (gas content) and the location of the strata. The gas emissionprediction <strong>for</strong> such a situation can be based on the rema<strong>in</strong><strong>in</strong>g gas profiles, as shown <strong>in</strong>Figure 8–4. There are three zones designated <strong>in</strong> the roof and two <strong>in</strong> the floor, which are characterizedby vary<strong>in</strong>g the rema<strong>in</strong><strong>in</strong>g gas gradients.Based on Figure 8–4, the residual gas pressures are first determ<strong>in</strong>ed layer by layer <strong>in</strong> accordancewith the mean normal distance of a gas-bear<strong>in</strong>g layer from the m<strong>in</strong>ed coal seam. The residualgas pressures are converted torema<strong>in</strong><strong>in</strong>g gas contents us<strong>in</strong>gthe Langmuir isotherm. Thedifference between the rema<strong>in</strong><strong>in</strong>gand <strong>in</strong>itial gas contentsrepresents the emitted portionof the adsorbed gas, which isthe required value [Noack1998]. Free gas is then addedto this value.121The gas pressure method hasthe advantage of not def<strong>in</strong><strong>in</strong>gupper and lower zones strictlycompared to the predictionbased on the degree of gasemission. Also, this methodtakes <strong>in</strong>to account both theadsorbed gas and the free gas<strong>in</strong> the surround<strong>in</strong>g strata.Figure 8–4.—Gas pressure method: residual gas pressure l<strong>in</strong>es aredependent on thickness of the m<strong>in</strong>ed coalbed [Noack 1998].There is another method basedon us<strong>in</strong>g zones of emission,reviewed extensively by Curl[1978]. This model describesmethane emissions <strong>in</strong> terms ofthe geometry of the zone ofemissions, the size of the zoneof emissions, and the degree of

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!