Outbursts Underground Coal Mines

OUTBURSTS IN UNDERGROUND COAL MINES

Outbursts are expulsions of gas and coal from the working face. They are energy release phenomena that may cause injury by mechanical force or by asphyxiation.

Most outbursts that are severe occur on geological structures in the coal seam that contain gouge (ground up) material. Some however occur from solid coal which fragments during the outburst. Examples of two kinds of outburst can be seen in the following diagrams.
Figure 1 shows a sketch of an outburst that occurred at Westcliff Colliery, NSW which moved the continuous miner backwards. The base of this was a sheared zone of coal behind the face.

outburst fig. 1

Figure 2 (overleaf) shows an sketch of a typical outburst that occurred from solid coal at Leichhardt Colliery, Queensland. Here the outbursts always occurred across the cleat often proceeded by an onion ring appearance in the face before buckling occurred outwards leaving a cone in the ribside. The size of these outbursts varied from 1 to 350 tonnes.

For an outburst to occur failure must first take place, failure is commonplace in mining and is due to the effective stress in the coal exceeding its strength. In an outburst the failure is accompanied with the release of energy and gas. The key to understanding outbursts is determining the likely sources of energy release while the key to controlling them is in minimising the potential for energy release.

outburst fig. 2

The sources of energy for an outburst are:
Strain Energy from Rock and Coal – This is dependent on the state of stress in the coal and its elastic properties. Very often the state of maximum stress is limited by failure at the face. In the case of outbursts that progressively erode from the face into
solid coal the state of stress varies from that at the face, which is limited by coal strength, to that in the virgin condition. Strain energy may also be supplied to an outburst by the movement of the surrounding strata.

The Expansion of Gas from Free Void Space – This comes from the adiabatic expansion of gas from the free void space (cleats). It is a virtually linear function of void space and gas pressure. If the coal is water saturated then there is no gas in the cleats to expand.

The Diffusion of Gas from Coal Particles – Gas may diffuse from the coal particles to an intermediate pressure within the failing coal mass in an outburst. This gas may then expand adiabatically to provide energy. The key to the energy release is the gas content which is linked to the gas pressure through the sorption isotherm, the coal particle size distribution and the diffusion coefficient. These factors determine the rate of gas release.

There is also significant energy absorbed during the failure process. It is related to the toughness of the coal. Toughness is by definition a measure of energy absorbed in causing failure.

Determining the Outburst Hazard
The process of determining the level of risk from an outburst is one of estimating the energy release per unit volume of the outburst and the likely volume that may be involved.

The energy release per unit volume is calculated by the determination of the stress within the coal and its elastic properties. The free void space is usually a very small component and may be ignored while the diffusive behaviour of the coal is very important.
It requires the measurement of gas pressure and content, the initial diffusion coefficient of the coal and the determination of likely particle sizes that will be produced during an outburst. Air drilling simulates an outburst and the collection of particles from such drilling gives a conservative (fine) indication of the particle sizes that may be generated. In the case of fault gouge material the particle size distribution is determined by measurement or estimated from historical data.

The energy absorbed by coal failure per unit volume is difficult to measure but indications of the coal toughness may come from grindability testing, drop hammer tests or by gassing up solid stressed coal and suddenly releasing the pressure to determine the level of fracturing that may occur.

The size of a potential outburst is also important as this directly effects the total energy release. Failures from solid coal are limited to the zone of coal that will fail. As failure is related to effective stress and strength the likely failure zone may be calculated bearing in mind that the fluid pressure contributes to effective stress. Most outbursts are however associated with fault gouge material and the size of such zones has a great bearing on the severity of outbursts from them. Therefore the determination of the likely gouge material volume is important.

The approach to outburst management may be to drain gas to blanket low level so that even if gouge zones are mined they will not produce an outburst of any severity. This may however be completely impractical in coals of low permeability where the
solid coal could be safely mined at a higher threshold. In this case a multiple gas threshold level may be adopted to suit solid coal or coal in faulted zones. The important control on this is that such faulted zones need to be detected and therefore the
confidence in the exploration procedure needs to be very high. This can only be achieved with a combination of approaches using in-seam drilling with measurement and geophysical techniques.

The Importance of Coal Permeability
The permeability of the coal has no direct bearing on the severity of an outburst at a given gas content and level of stress. However coals with low permeabilities are far more prone to outbursting because they are much harder to drain.

The Dangers of Shotfiring through Outburst Prone Coals
The approach of shotfiring through outburst prone coals should not be followed. Historically outbursts have occurred after shotfiring catching returning crews unaware. Indeed in some cases the outbursts have occurred from the ribside behind the face. In other instances the outburst initiated by shotfiring is so large that it has totally overtaken the mine’s ventilation system and led to an explosion.

Sigra’s approach to outbursts is to first understand the geological conditions. Then to measure the coal stresses and its elastic and post elastic properties so as to understand the net strain energy available when failure occurs. This is followed by careful testing to determine the gas storage and desorption behaviour of the coal, including its fragmentation behaviour on
sudden desorption. From these measurements we can determine risk and recommend levels to which gas should be drained to minimise the risk of outbursts. It is important to recognise that a single threshold level does not suit all conditions.

Sigra can characterise the coal seam reservoir behaviour and design the most appropriate drainage system to suit the mine.

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