GeoGas Application of Outburst Thresholds to Non-Bull
GeoGas Application of Outburst Thresholds to Non-Bull
GeoGas Application of Outburst Thresholds to Non-Bull
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<strong>Outburst</strong> initiation<br />
• With continued mining the highly stressed barrier suddenly fails:<br />
• The stress is suddenly reduced<br />
• The ambient fluid pressure on the coal changes from being mostly above<br />
desorption pressure <strong>to</strong> suddenly being well below the desorption pressure for<br />
the gas content <strong>of</strong> the coal<br />
• The rapid increase in gas pressure (free gas) in the fractured coal over comes<br />
the resistance <strong>of</strong> the weakened coal mass, resulting in the sudden release <strong>of</strong><br />
large volumes <strong>of</strong> gas with entrained coal particles<br />
• The initiation <strong>of</strong> the outburst is defined by the rate <strong>of</strong> gas desorption<br />
and in turn the rapid increase in gas pressure in combination with the strength<br />
<strong>of</strong> the confining coal barrier<br />
BU seam checks<br />
Gas Content at 900 DRI (m3/t)<br />
16<br />
14<br />
12<br />
10<br />
8<br />
6<br />
4<br />
2<br />
Part <strong>of</strong> the Runge Group<br />
Gas content threshold @<br />
100% CH4 = 9.4 - 9.7 m3/t<br />
Part <strong>of</strong> the Runge Group<br />
<strong>Bull</strong>i Seam Mines<br />
0<br />
0 0.2 0.4 0.6 0.8 1<br />
WW seam thresholds<br />
• 6.5 – 7.5 m3/t<br />
• 0 – 65% CO2<br />
• Little variation in<br />
desorption rate with<br />
gas composition<br />
GasContent at 900 DRI (m3/t)<br />
16<br />
15<br />
14<br />
13<br />
12<br />
11<br />
10<br />
9<br />
8<br />
7<br />
6<br />
5<br />
4<br />
3<br />
2<br />
1<br />
CO2/CO2+CH4<br />
Wongawilli Seam<br />
Part <strong>of</strong> the Runge Group<br />
Lama Structured (BU)<br />
Wongawilli (T)<br />
Wongawilli (N)<br />
Wongawilli (D)<br />
Gas content threshold @<br />
100% CO2 = 6.9 - 7.1 m3/t<br />
DRICalcsAugust2010_MB.xls<br />
0<br />
0 10 20 30 40 50 60 70 80 90 100<br />
CO2 (%)<br />
DRI900<br />
• In assessing gas content data from the <strong>Bull</strong>i seam using cores derived initially<br />
from West Cliff Colliery it was found that<br />
• The relationship between gas content and desorption rate was linear<br />
• The desorption rate for CO2 was higher than for CH4<br />
• A gas content <strong>of</strong> 9.5 m3/t (CH4) has essentially the same desorption rate as a gas<br />
content <strong>of</strong> 6.2 m3/t (CO2)<br />
• The threshold values coincide with a DRI <strong>of</strong> 900<br />
10<br />
9<br />
8<br />
7<br />
6<br />
5<br />
4<br />
3<br />
2<br />
1<br />
0<br />
GeoGAS Fast Desorption method<br />
0 200 400 600 800 1000 1200 1400 1600<br />
Gas volume 30 sec crushing 200 g (ml ( ml)<br />
Gas content (m3/t)<br />
Part <strong>of</strong> the Runge Group<br />
<strong>Non</strong> <strong>Bull</strong>i seam thresholds<br />
• DRI900 has been used <strong>to</strong> establish outburst<br />
thresholds in the Wongawilli seam, Hunter<br />
Valley seams, Gunnedah and Bowen Basins<br />
seams<br />
• No GDIs regardless <strong>of</strong> the severity <strong>of</strong> other<br />
fac<strong>to</strong>rs<br />
• <strong>Thresholds</strong> vary by seam and by composition<br />
Part <strong>of</strong> the Runge Group<br />
<strong>Thresholds</strong> – Newcastle Mines<br />
• 10 – 11 m3/t<br />
• 95 – 100% CH4<br />
• 8.4 m3/t<br />
• 80% CO2<br />
Qm at 900 DRI (m3/t)<br />
Newcastle<br />
16<br />
15<br />
14<br />
13<br />
12<br />
11<br />
10<br />
Part <strong>of</strong> the Runge Group<br />
9<br />
8<br />
7<br />
6<br />
5<br />
4<br />
3<br />
2<br />
1<br />
Lama Structured (BU)<br />
West Wallarah<br />
Fassifern<br />
Donaldson<br />
Greta<br />
Wallarah / Great Northern<br />
>90% CO2