Coal mine and CSG operations can induce changes in and ; such changes depend on varying factors such as hydraulic properties of the rocks and sediments near operations, and geological fracturing and faulting. This in turn can potentially reduce the quantity of water that would otherwise discharge to a stream, or may cause a drop in water level in a groundwater , which makes water more difficult, or cause the bore to dry out (periodically or permanently).
The assessment identified the associated with CSG operations that could potentially result in hydrological changes; this process provided a crucial underpinning to hydrological modelling. The chain of events that commonly arise from these hazards were subsequently analysed and categorised into four major groups (Figure 4):
- ‘Subsurface depressurisation and dewatering’ includes extraction of groundwater to enable CSG production. It has the potential to directly affect the regional groundwater system, and indirectly affect surface water – groundwater interactions. Potential effects are in the medium term (5 to 10 years) to long term (10 to 100 years).
- Changes to ‘Subsurface physical flow paths’ might occur due to hydraulic fracturing of coal seams (fracking) or when wells drilled for groundwater or gas extraction leak. Potential effects are in the medium to long term and are probably restricted to aquifer or aquifer outcrop areas, but can also affect connected watercourses within and downstream of coal resource development.
- Changes to ‘Surface water drainage’ might occur when CSG operations alter surface water systems or cause the land surface to sink ( subsidence). These changes have potential medium-term to long-term cumulative effects on watercourses within and downstream of coal resource development.
- ‘Operational water management’ involves storing, disposing, processing and using extracted water. Potential effects are in the medium to long term and include watercourses that are within and downstream of coal resource development.
Hazards and causal pathways associated with coal mining were not considered further because no coal mines were modelled. Hazards ruled out of the assessment include accidents and those managed by regulation or site-based risk management.
This schematic diagram is not drawn to scale and is generic. In a hydrologically confined aquifer or coal measure, the water pressure level may rise above the top of the geological layer. Groundwater drawdown caused by coal seam gas extraction does not necessarily translate to changes in depth to the watertable (Box 4). The inset schematic shows hydraulic fracturing of a coal seam, where a mixture predominantly composed of water (blue) and sand (yellow), with minor amounts of chemical additives, is injected at high pressure into the well to produce small cracks in the coal (lighter grey zone). This process enhances the permeability of the coal seam, enabling larger volumes of gas and water to be subsequently pumped from the well.
Product Finalisation date
- Explore this assessment
- About the bioregion
- How does the bioregion's geology and hydrogeology influence water movement?
- How could coal resource development result in hydrological changes?
- What are the potential hydrological changes?
- What are the potential impacts of the hydrological changes?
- How to use this assessment
- Building on this assessment
- References and further reading
- Contributors to the Technical Programme