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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

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