The objective of the Bioregional Assessment Programme is to understand and predict regional-scale on water resources and caused by coal resource developments in Australia’s major coal-bearing basins. The distinguish areas where water resources and water-dependent assets are very unlikely to be impacted (with a less than 5% chance) from those where water resources and water-dependent assets are potentially impacted. Given the regional-scale focus, the modelling does not account for local-scale details (e.g. the presence of local ; stream condition). Areas identified in a BA as at of potentially significant changes serve as ‘red flags’ for directing further local investigation. Governments, industry and the community can then focus on areas that are potentially impacted when making regulatory, water management and planning decisions. In some cases, the risk of adverse may be substantially diminished or negligible when local-scale factors are brought to bear. An example of using local geological and hydrogeological information to constrain results from the regional-scale assessment is presented as part of the BA for the (see companion product 2.6.2 for the Hunter subregion (); Sections 3.3 and 3.4).
The impact and risk analysis considers only biophysical , such as changes in hydrology or ecology; fully evaluating consequences requires value judgments and non-scientific information that is beyond the scope of BAs. A full risk assessment (with risk evaluation and risk treatment) is not conducted as part of BAs.
The purpose of this section is to highlight design choices that have steered the direction of this BA and culminated in the impact and risk analysis. Further details about the design choices are provided in companion submethodology M10 (as listed in Table 1) for analysing impacts and risks ().
188.8.131.52 Choice of modelled futures
A is a regional analysis that compares two futures of coal resource development. In BAs, the term ‘coal resource development’ specifically includes coal mining (both open-cut and underground) as well as CSG extraction. Other forms of coal-related development , such as underground coal gasification and microbial enhancement of gas resources, were not within the scope of the assessment.
The two futures considered in a BA are:
- baseline coal resource development (baseline): a future that includes all coal mines and CSG fields that are commercially producing as of December 2012
- coal resource development pathway (CRDP): a future that includes all coal mines and CSG fields that are in the as well as those that are expected to begin commercial production after December 2012.
The difference in results between and baseline is the change that is primarily reported in a BA. This change is due to the additional coal resource development – all coal mines and CSG fields, including expansions of baseline operations that are expected to begin commercial production after December 2012.
In December 2012, there were 42 mining operations in the , comprising 22 open-cut mines and 20 underground mines. As of September 2015, 22 proposals for coal resource developments were identified for the Hunter subregion (companion product 2.3 ()). Thus, the Hunter CRDP includes 64 mining operations (Table 3; Figure 5). Of these, 41 baseline mines and 17 additional coal mines were represented in the modelling (companion product 2.6.2 for the Hunter subregion ()); and 28 baseline mines and 17 additional coal mines in the modelling (companion product 2.6.1 for the Hunter subregion (Zhang et al., 2018)). The potential due to the non-modelled coal mines are considered further in Section 3.6.
Table 3 Coal mines in the coal resource development pathway for the Hunter subregion
The mines in the coal resource development pathway are the sum of those in the baseline and the additional coal resource development (ACRD).
The CRDP is the most likely future, based on the analysis and expert judgment of the Assessment team in consultation with coal and gas industry representatives, state agencies and the Australian Government. The CRDP was finalised for the Hunter subregion based on information available in September 2015 (see companion product 2.3 ()) to allow the hydrological numerical modelling to commence. It is acknowledged that developments in the CRDP may ultimately be implemented in different ways (e.g. changes to timing), or circumstances may change (e.g. a proposal may be rejected, as was the case for the Drayton South Project, which was rejected by the NSW Planning Assessment Commission in February 2017 for the fourth time). This reflects the dynamic nature of resource investment decision making, related to diverse economic, environmental, political and social factors. Consequently, the CRDP needs to be viewed as an indicative future that highlights potential changes for water resources and that may need to be considered further in local analyses or via approval conditions required by regulators. Equally as important, the CRDP plays a role in identifying where changes will not occur, flagging where potential impacts to water resources and water-dependent assets are very unlikely.
BAs primarily focus on the potential impacts to water resources and water-dependent assets that are attributable to . Potentially important impacts under the baseline, which might occur in parts of the Hunter subregion that are not further affected by additional coal resource development, are afforded less attention in the assessment. However, they could be important in interpreting impacts due to additional coal resource development. For instance, the implications for a of an additional 2 m of in the may depend on whether the is 0.1, 1.0 or even 10 m.
Factors such as climate change and land use (e.g. agriculture) were held constant between the two futures. Although the future climate and/or land use may differ from those assumed in BAs, the effect of this choice is likely to be small because the focus of BAs is on reporting the difference in results between the CRDP and baseline.
184.108.40.206 Focus on water quantity and availability
focus solely on water-related , and specifically those related to water quantity and availability. Potential water quality are identified, but the analysis, as determined by the BA scope, is limited to salinity and is only addressed qualitatively. BAs are also concerned with those and that may accumulate, either over extended time frames or as a result of multiple coal resource developments. These typically correspond to changes in surface water and groundwater that are sustained over long periods of time, sometimes decades, and which may create the potential for flow-on effects through the wider hydrological system.
Many related to coal resource development may cause local or on-site changes to surface water or groundwater. These are not considered in the BA because they are assumed to be adequately managed by site-based management and mitigation procedures, and are unlikely to create potential . Impacts and risks associated with water quality attributes other than salinity that are potentially affected by coal resource development are identified, but not analysed further, in this BA.
220.127.116.11 Assessment of regional-scale cumulative developments
are designed to analyse the of coal resource developments at a regional scale, and not focus specifically on individual mines or CSG operations. The and for the each comprise a suite of developments, which are distributed across the at variable distances from each other and have variable, but often overlapping, periods of operation. Thus, there is potential for the to accumulate to varying degrees in both space and time.
Regional-scale models are used to predict the cumulative hydrological changes and potential impacts of those developments on and from multiple developments over time. The area of potential impact is expected to be more extensive and extend greater distances downstream of developments than what is predicted from site-scale, single mine models. In some cases the spatial or temporal alignment of certain coal resource developments can allow for attribution of potential effects to individual developments, but that occurs because of that alignment rather than by design.
Results of the impact and analysis reported in this product do not replace the need for the detailed site- or project-specific investigations that are currently required under existing state and Commonwealth legislation. The hydrological and ecological systems modelling undertaken for a BA are appropriate for assessing the potential impacts on and risks to water resources and water-dependent assets at the ‘whole-of-basin’ scale, whereas the modelling undertaken by a mining proponent for an individual development, as part of an environmental assessment, occurs at a much finer scale and makes use of local information to more accurately represent the local situation. Therefore, results from these detailed mine-specific studies are expected to differ from those from a BA. However, as a range of potential parameter values are considered in a BA, it is expected that the range of possible outcomes predicted by a BA will encompass the results from individual site-specific studies. This is illustrated in this product using local hydrogeological data from the Wyong river basin to constrain the set of results based on the regional parameter set.
18.104.22.168 Focus on predictive uncertainty
In , parameter is considered as fully as possible when predicting hydrological outcomes (i.e. changes to or ) and ecological outcomes (i.e. changes to ecologically relevant ). For example, groundwater models are run many thousands of times using a wide range of plausible input parameters for the critical hydraulic properties, such as the hydraulic conductivity and storage coefficients of all modelled hydrogeological layers. This differs from the traditional deterministic approach used more routinely for groundwater and surface water modelling.
While models are constrained to data, the density of reliable observation data is sparse, so results may not represent local conditions well. However, they do consistently represent the and uncertainty at all sites through of possible hydrological changes, where the area, depth, timing and assumed pumping rates of each development largely determine the spatial variation, and lack of detail about the physical environment at any given point in the define the uncertainty.
Given the wide range of plausible input parameters used in the regional modelling, the hydrological changes due to at any given location within the assessment extent can be assumed to lie within the distribution of modelled changes. This assumption may not be valid near open-cut mines where potentially steep hydraulic gradients at the mine pit interface are poorly resolved in the regional groundwater models. These areas are excluded from the ecological analysis for this reason. Where the BA regional-scale analysis identifies an area as ‘at risk’ of large hydrological changes and potentially significant on ecological, economic and/or sociocultural values, local scale information may be necessary to constrain the predictive uncertainty to something more representative of local conditions, and more appropriate for informing the management response.
The quantitative representation of the predictive uncertainty through probability distributions allows BAs to consider the of impacts with a specified magnitude and underpins the impact and risk analysis. Sources of uncertainty that cannot be quantified are considered qualitatively.
22.214.171.124 A landscape classification
Subregions are complex landscapes with a wide range of human and ecological systems. The systems can be discrete, overlapping or integrated. Because of this complexity, a direct analysis of each and every point, or , in the landscape across the subregion is not currently possible, nor warranted in a regional-scale assessment. Abstraction and a systems-level classification can simplify the challenges of the dimensionality of the task and direct the focus to those that are water dependent.
A landscape class represents an with characteristics that are expected to respond similarly to changes in and/or due to coal resource development. A set of landscape classes was defined for the that builds on existing well-accepted classifications and is described in detail in companion product 2.3 for the Hunter subregion (). While it is generally assumed that there will be less heterogeneity in the response within a landscape class than between landscape classes, the grouping of some landscape classes into one (companion product 2.7 for the Hunter subregion ()) suggests that at least some responses can be the same between landscape classes.
The assessment of on and to water-dependent ecological relies heavily on the landscape classification. Potential impacts to individual assets are assessed via their constituent landscape classes. For each of those landscape classes, the assessment is based on the qualitative mathematical models for those landscape classes and the indicators of hydrological change or ecosystem change identified as important for that landscape class.
126.96.36.199 Ruling out potential impacts
An important outcome of the multiple components of this is to identify areas of the that are very unlikely to be impacted by . Potential are ruled out where possible, both spatially and in terms of specific or , in order to focus the analysis on where potential impacts have a higher probability of occurring. This process starts with defining a (PAE) for a subregion or that is a conservative spatial boundary, encompassing areas of potential impact based on the most likely coal resource developments within the subregion. The is where assessment effort was preferentially focused when collating , defining to summarise key surface , and constructing numerical surface water and groundwater models.
Results of the hydrological modelling are used to finalise the ‘assessment extent’ used in the impact and analysis. No changes to the Hunter PAE were deemed necessary, and the ‘assessment extent’ for the Hunter subregion is the same as the PAE identified in companion product 1.3 for the Hunter subregion ().
Results of the hydrological modelling are also used to define the (Section 3.3.1). Potential impacts on water-dependent landscape classes and are ruled out if they are wholly outside the zone of potential hydrological change. Thus, the is used to identify landscape classes that should be investigated further through qualitative mathematical modelling and receptor impact modelling, and, as required, through use of local information to better define the risk and appropriate management response. Equally important, this logical and consistently applied process rules out landscape classes or water-dependent assets where potential impacts due to additional coal resource development are very unlikely (less than 5% chance) to occur.
Product Finalisation date
- 3.1 Overview
- 3.2 Methods
- 3.3 Potential hydrological changes
- 3.4 Impacts on and risks to landscape classes
- 3.5 Impacts on and risks to water-dependent assets
- 3.6 Commentary for coal resource developments that are not modelled
- 3.7 Conclusion
- Contributors to the Technical Programme
- About this technical product