HOME Water Resources in Australian Mine Pit Lakes R N Kumar1, C D McCullough2 and M A Lund3 ABSTRACT In Australia and worldwide, open cut mining has become increasingly common over the last few decades through changes in excavation technology and ore economics. However, such operations frequently leave a legacy of open mine pits once mining ceases. Pit lakes will then form in mine pits that extend below the water table when dewatering operations cease. Pit lake waters are typically contaminated with metals, metalloids, saline or acidic/alkaline and rarely approach natural water body chemistry. Physically, pit lakes have unique bathymetries, are often strongly wind sheltered and have very small catchments. Nevertheless, pit lake waters often constitute a vast resource but of limited beneficial use (due to water quality issues); with a potential to contaminate regional surface and ground water resources. Water in pit lakes has the potential to be useful for a range of purposes in the Australian context of characteristic hot, dry climate and relatively few natural water bodies. Consequently, pit lakes can be seen to represent either a significant liability or a water resource to mining companies and regional communities. However, the lack of knowledge on pit lakes continues to hinder their proper management. This paper summarises the limited information currently available on water quality associated with Australian pit lakes. Information on pit lake occurrence, distribution and water quantity and quality is not nationally collated and requires immediate and ongoing attention from both mining companies and regulating authorities. Lack of a readily available database for pit lake occurrence, distribution and water quality fails to realise the potential for these water resources by both mining companies and Australian communities. Lack of access to pit lake quantity and water quality data may also lead to failure to manage this significant source of mining environmental risk. WA estimated that there are 1800 mine pits in the state potentially forming pit lakes (Johnson and Wright, 2003) (Figure 1). Additionally, although most states have created databases of derelict or abandoned mine workings, pit lakes are not specifically surveyed for, particularly those on active or unrelinquished leases, eg Ormsby, Howard and Eaton (2003). Many mining operations do not collect water quality data on their pit lakes as they are on unrelinquished mining leases with companies retaining them with an option to over-mine as technology and economics alter the viability of their remaining resources. Where pit lake water quality data are collected, these data are often only used for ad hoc purposes such as compliance reporting, with no central database even maintained by the reporting company. Such lack of detailed data of pit lake water quantity and quality for many regions currently renders it impossible to assess the risk and opportunities presented by pit lakes to Australia. INTRODUCTION Open cut mining is now common practice in modern Australian mining operations and, as backfilling is normally unfeasible practically or economically, their major legacy is typically an open pit on completion of extraction operations. Pit lakes form in mine pits that extend below the natural groundwater table. Most pit lakes fill with groundwater (as many pits are in low rainfall areas) supplemented by varying quantities of surface inputs. In some instances, pit lakes can be rapid filled with stream or river diversions (as these may have been diverted initially to allow mining to occur). In the absence of rapid fill options, pit lakes may take many years to naturally fill. For example, it has been estimated that the Muja pit in Collie (Western Australia) will take over 50 years to fill. The quality of catchment geology and of the filling water will contribute to the final water quality of the pit lake. It is not known how many pit lakes exist in Australia, as no pit lake-specific State or Commonwealth inventory has been undertaken. There have been some recent efforts in Queensland, New South Wales and Western Australia (WA) to create state-based databases or reports. For example, a recent study in 1. Post Doctoral Research Fellow, Mine Water and Environment Research Group (MiWER), Centre for Ecosystem Management, Edith Cowan University, 270 Joondalup Drive, Joondalup WA 6027. Email: [email protected] 2. Lecturer, Mine Water and Environment Research Group (MiWER), Centre for Ecosystem Management, Edith Cowan University, 270 Joondalup Drive, Joondalup WA 6027. Email: [email protected] 3. Associate Professor, Mine Water and Environment Research Group (MiWER), Centre for Ecosystem Management, Edith Cowan University, 270 Joondalup Drive, Joondalup WA 6027. Email: [email protected] Water in Mining Conference FIG 1 - One of the many abandoned pit lakes in the Goldfields region, WA. Pit lakes occur in all states and territories (Figure 2), yet for a country with limited water resources, neither ‘pit lake’ or even ‘lake’ are mentioned in the Federal government’s recent ‘Mine Rehabilitation Handbook’ guidelines (DITR, 2007). Pit lakes also occur across a broad range of climatic regions. Australia is one of the driest continents in the world and the demand for water resources in many of the most arid regions by industry and communities continues to increase as a result of population growth and expansion and development of mining operations. Pit lake water may therefore be of significant potential use to both industry and surrounding communities (McCullough and Lund, 2006). However, the potential use of pit lake water remains dependent on the pit lake water quantity and quality (Doupé and Lymbery, 2005). This paper aims to summarise the currently available information on pit lakes in Australia to highlight the need for a national inventory and demonstrate why monitoring of pit lakes is essential to prepare for relinquishment. MINE PIT LAKE ISSUES IN AUSTRALIA Pit lakes differ physically from natural Australian lakes in having markedly higher relative depths. For example, pit lakes commonly have relative depths between ten and 40 per cent compared to natural lakes which are between 0.4 and seven per cent (Doyle and Runnells, 1997). Where sides are battered for Perth, WA, 15 - 17 September 2009 247 R N KUMAR, C D McCULLOUGH and M A LUND FIG 2 - Distribution of historic and operating mines in Australia (Australian Mines Atlas, 2009). public access or to promote development of riparian zones, deep pits will still have a bathymetry unlike with natural lakes with steep sides below the battering. The size of mining pits in Australia ranges from relatively small urban borrow pits of about 100 m in diameter, to enormous open cut operations such as Mount Whaleback mine in the Central Pilbara, (WA) which will have final pit dimensions of 5.5 km by 2.2 km and a depth of 500 m (Johnson and Wright, 2003). These new mining pit lakes have few natural counterparts to their size in Australia, especially in depth and volume. Furthermore, as the water level in the pit lake equilibrates, it is frequently deep within the open-cut, creating very little opportunity for natural slopes to the water surface, this also influences water mixing due to sheltering from winds (Huber et al, 2008). With no natural catchments, inflows of rainwater can be limited which may be useful in preventing worsening water quality from exposed geologies but also limits the amount of freshwater inputs in areas where exposed geologies are not problematic. Pit lake water quality can be highly variable; particularly for acidity, salinity, hardness and metal concentrations which are primarily governed by the pit lake catchment hydrology and geochemistry (Miller, Lyons and Davis, 1996). For example, pit lake water quality may become acidic, through oxidation of reactive iron-bearing geologies as Acid Mine Drainage (AMD) (Klapper and Geller, 2002). Such acidic mine waters are often toxic to aquatic biota (Spry and Wiener, 1991; Stephens and Ingram, 2006; Storer, Whisson and Evan, 2002). Pit lakes waters affected by salinity and acidity may also adversely influence nearby and regional groundwater resources and receiving environments, eg wetlands with contaminated plumes from flow-through pit lakes extending large distances down-gradient. The extent of such an impact may vary from insignificant in low hydraulic conductivity rocks and groundwater systems already saline, to considerable in high hydraulic conductivity rocks and naturally low-salinity groundwater environments (Commander, Mills and Waterhouse, 1994; Johnson and Wright, 2003). 248 The majority of pit lake studies conducted in Australia have focused on physical and chemical characteristics of water quality (Boland and Padovan, 2002; Jones et al, 2008; McCullough, Lund and May, 2008a). These studies have demonstrated that pit lake water quality is influenced by many factors including climate, groundwater quality, depth, pit filling method and local mineralogy. Regionally representative water quality data from a selection of pit lakes across Australia is summarised in Table 1. TYPES OF PIT LAKES Australian pit lakes fall into four main categories in terms of their water quality. These are acidic (AMD affected), saline (can co-occur with AMD), neutral pH (but with some degree of contamination), and good water quality (but not necessarily comparable to natural regional waterbodies) (Kumar, McCullough and Lund, in press). 1. Acidic – As examples, water quality of pit lakes of Collie (WA) (Figure 3), Collinsville (Figure 4) and Mt Morgan (both Queensland) are all degraded by AMD. Nevertheless, Collie pit lakes have low pH and toxic concentrations of Al primarily due to low buffering rather than high acidity inputs. Collinsville and Mt Morgan show similar classic AMD conditions of extremely low pH and very high metal concentrations. These latter pit lakes also show effects of ongoing salinisation (see next). 2. Saline – In drier regions where net evaporation exceeds precipitation, and surface inflow to the pit is largely restricted to direct precipitation, can result in dramatic increases in salinity leading to brackish through to hyper-saline lakes. Such hyper-saline pit lakes of degraded value may also contaminate valuable regional groundwater resources in the future. For instance, in semi-arid regions such as the Collinsville region, high rates of evapoconcentration result in significant increases in pit lake salinity each year (McCullough, Lund and May, 2008b). Perth, WA, 15 - 17 September 2009 Water in Mining Conference WATER RESOURCES IN AUSTRALIAN MINE PIT LAKES TABLE 1 Characteristics of some Australia pit lakes. All values are in mg L-1 unless otherwise stated. N = Number of pit lakes in region considered. - = no data available (adapted from Kumar, McCullough and Lund, in press). Kemerton, Western Australia (N = 1) St. Barbara Mines, Western Australia (N = 2) Thalanga Mine, Queensland (N = 1) 12°41'S, 132°55'E 33°12'58"S, 115°45'25"E 28°50'25"S, 121°17'17"E 20°20' S, 145°46' E Ranger Mine, Mary Northern Kathleen, Territory Queensland (N = 1) (N = 1) Parameter Collie Basin, Western Australia (N = 4) Collinsville, North Bowen Basin, Queensland (N = 4) Mount Morgan, Queensland (N = 1) GPS coordinates 33°21'47 S, 116°09'22 E 20°33'51 S, 147°49'52 E 26°38'22 S, 150°22'02 E 20°45'1 S 140°0'6 E Ore type Coal Coal Au, Cu U U Silica sand Au Cu-Pb-Zn Depth (m) 8 - 70 4 - 14 - - - 6 - 70 0.06 - 1.03 0.01 - 0.06 - - - - 0.006 - 0.95 - 3.8 - 5.0 1.5 - 4.9 2.8 6.1 7.6 8.5 8.0 - 8.6 7.7 Total P <0.005 - 0.009 <0.005 - - 0.01 0.02 - - Total N <0.05 - 1.5 0.51 - - 1.96 0.573 7.3 - 22.8 - Dissolved Organic Carbon 3.1 - 7.3 1 - 59 - - - 22 - - Conductivity (mS cm-1) 0.42 - 1.4 7.8 - 23.5 11 5.05 0.89 1.2 - 1.07 Sulfate 31 - 107 300 - 25000 12 100 1840 782 296 2570 - 7190 7950 Area (km2) pH Aluminium 0.001 - 0.006 23 - 1300 740 0.032 0.026 0.1 0.02 - 0.06 <1 Calcium 2.3 - 6.0 124 - 519 520 464 0.02 67 334 - 1120 718 Cadmium <0.002 <0.01 - 0.023 0.15 - <0.0002 - 0.0002 0.16 Cobalt <0.005 0.6 - 7.2 - - 0.0005 - - - Chromium <0.10 <0.01 - 0.47 - - <0.002 - 0.002 - Copper <0.002 - <0.05 <0.05 - 2.5 36 1.17 0.0024 - 0.03 <1 Iron 0.0003 - 0.005 139 - 2463 248 3.23 <20 0.14 <0.05 - 0.06 0.575 Lead - <0.1 - 6.3 - - 0.001 <0.1 - <1 Magnesium 0.077 - 16.3 197 - 2239 1240 140 115 58 865 - 3150 1025 Manganese 0.0002 - 1.2 13 - 150 81 - 0.041 <0.01 - - Nickel 0.03 - 0.34 1.2 - 17 - 0.69 0.0053 - 0.09 - Uranium 0.020 - 0.029 - 0.460 1.76 - - - 0.0005 - 6.9 1 - 46 25.3 0.088 0.0037 0.15 0.01 53.5 Chlorophyll a (µg L-1) 0.1 - 64 0 - 64 - - - 6.5 - 8.5 - - Zooplankton studies? Yes Yes - - - No - - Macroinvertebrate studies? Yes Yes - - - Yes - - Periphyton studies? Yes No No No No No No No Catchment rehabilitation? Yes Yes Yes Yes Yes Yes Yes - Pit lake remediation? 1 lake 1 lake 1 lake 1 lake Backfilling No - Backfilling Proposed end use(s) Aquaculture, recreation Industry use - - - - None - Catchment lease Bonded Bonded - - Bonded Owned Bonded n/a Potential closure criteria Recreational use Bunded lake - - Backfilled Pond Bunded lake - Zinc Limited monitoring data from the Mount Goldsworthy pit, Western Australia also demonstrated that the salinity of the pit lake increased from 1400 to 5500 mg L–1 TDS over a 14 year period (Johnson and Wright, 2003). This phenomenon is particularly pronounced in lakes that are groundwater sinks (Commander, Mills and Waterhouse, 1994). Alternatively, arid Australian regions such as the southern Goldfields of WA may produce hyper-saline pit lakes from Water in Mining Conference inputs of saline groundwaters (Johnson and Wright, 2003). Periodic addition of fresh rainwater to pit lakes can result in a salinity stratified lake (Johnson and Wright, 2003) or with sufficient flows can form a freshwater recharge pit lake (sensu Commander, Mills and Waterhouse, 1994; Gerrard, 2002). Contamination of groundwater in such arid areas can often be a minimal risk as high evaporation rates ensure the pit lake remains a groundwater sink. Perth, WA, 15 - 17 September 2009 249 R N KUMAR, C D McCULLOUGH and M A LUND FIG 3 - Lake Ewington, a small historic Collie mining lake currently being remined. FIG 4 - Collinsville (Queensland) acidic pit lake water quality beginning to improve following bioremediation treatment (after McCullough, Lund and May, 2008a). 3. Neutral – Mary Kathleen and Thalanga (Queensland), Ranger (Northern Territory) and Wedge Pit (WA) pit lakes have generally good water quality that is nevertheless contaminated by one or more metals; in these cases Cu, Zn, U and As respectively. Nevertheless, these pit lakes remain well suited to a variety of end-uses as individual contaminants can often be more readily remediated or treated than more complex pit lake chemistries. For example, As contaminated water is extracted from bores a few meters away from Wedge Pit, treated and used to supply potable water to Laverton. 4. Good water quality – Kemerton (WA) is a silica sand mining operation with few geological considerations or mining processes that result in contamination of pit lake waters, hence water quality is very good. However, there remain significant differences in lake shape and water quality compared to shallow naturally acidic wetlands nearby (McCullough and Lund, 2008). management strategies are required for officially closed leases, as well as mining operations under care and maintenance. However, there are no specific state or national guidelines for pit lake water quality. Instead, often general environmental water quality guidelines are used to determine acceptability of pit lake water quality (ANZECC/ARMCANZ, 2000). In some cases, pit lake water quality is regulated according to end use requirements or for safety of nearby environments (Batley et al, 2003). Some states, eg WA, regulates water quality in pit lakes on a case-by-case basis depending on mine closure options (Johnson and Wright, 2003). Present strategies for pit lakes closure in Australia can be grouped into three main categories (Evans and Ashton, 2000): 1. enclose and forget approach, this involves construction of a bund around the void to prevent access and protect mining companies from litigation arising from accidents; 2. strategic closures addressing environmental issues often mainly concerned with development of environmental values such as biodiversity conservation, eg remediation of water quality and development of wildlife habitat in mine lakes (McCullough, Hunt and Evans, 2009); or 3. initiatives that will result in the creation of employment and business enterprise opportunities (eg aquaculture, ecotourism, various forms of horticulture) or result in the creation of a community resource such as a recreational facility, eg Harper et al (1997). PIT LAKE RELINQUISHMENT A number of pit lakes are now being managed by local and state governments, mainly through abandonment (eg Stockton and Black Diamond lakes in Collie) or through agreements for the government to accept environmental liabilities in return for facilitating new mining (eg Mt Morgan). Ongoing pit lake 250 Perth, WA, 15 - 17 September 2009 Water in Mining Conference WATER RESOURCES IN AUSTRALIAN MINE PIT LAKES This first strategy of enclosing pit lakes addresses immediate legislative requirements, and liability issues, but creates a future potential liability and fails to provide any benefits to local communities. The other two closure strategies hold more promise for significant local community benefit (Evans and Ashton, 2000; McCullough and Lund, 2006). However, of equal importance to identification of social aspects of mine closure is the application of sound and well-researched science to the end use development process, be it catchment rehabilitation or water quality remediation (Evans, 2006; McCullough, Hunt and Evans, 2009). Nevertheless, the continuing paucity of regulatory direction given to mining companies ensures there remain few examples of successful pit lake closure and associated lease relinquishment back to government. Currently there are no Commonwealth or state guidelines for developing pit lakes as useful water resources. For instance, acidic and/or saline pit lakes influenced by AMD with acidic and metal contaminated water will need to be remediated using either chemical or biological methods (McCullough, 2008; McCullough, Lund and May, 2008b; Neil et al, in press). Pit lakes contaminated with one or two metals but otherwise with good water quality can be used for a range of activities following chemical treatment such as selective precipitation. On the other hand, pit lakes with good water quality can be used immediately for uses such as aquaculture, water sports and recreation, etc. Even partial remediation of highly acidic and saline waters can allow this water to be used for activities such as dust suppression, potentially reducing demands on other higher quality water sources (McCullough and Lund, 2006). However, despite the potential and existing examples of possible beneficial end uses for pit lakes, there are many pit lakes across the Australian continent with no current or future use by current or proposed mining operations (Farrell, 1998). END USES FOR PIT LAKES Water quality in pit lakes plays a dominant role in determining the range of end uses the lake can be used for (see Lund and McCullough, 2006). It is therefore surprising for a country which has been facing scarcity of water for a number of years that so little is known of the significant water resources available in pit lakes and how they might be remediated and used. The chosen end use will necessitate a certain water quality within the pit lake and remediation technologies will be needed in many cases to achieve the required end use water quality. Research is therefore required into water quality development in pit lakes by incorporating hydro-geological, limnological, biological and biogeochemical processes. Current predictive models do not adequately account for sufficient of these processes for pit lakes to allow for useful predictions to be made (Jones, 1997). Instead, such models are likely to provide information for advancing current conceptual models and provide advice of pit lake response to different management scenarios (McCullough, Hunt and Evans, 2009). CONCLUSIONS Planned closure or remediation of pit lakes could avoid many of these adverse effects of degraded pit lake water quality to the environment (Figure 5). Furthermore, the major steps that needed to achieve pit lake sustainability in Australia involve developing better understanding of the hydrology, water quality and other limiting ecological factors of pit lakes. Based on an understanding of limiting water quality parameters, appropriate remediation and rehabilitation strategies may then be available to achieve beneficial end uses. Key recommendations for future study of Australian pit lakes are that a focus should be on: OPEN CUT MINING MINE VOIDS BACKFILLING Expensive & Unfeasible Left as open pits PIT LAKES CURRENT UNSUSTAINABLE SCENARIO POTENTIAL SUSTAINABLE SCENARIO Low pit lake water quality - acidic, saline, metal rich - LIMITED USE/LIABILITY Good (potentially remediated) pit lake Water USEFUL RESOURCE Threat to groundwater and regional environment; risk to local communities (drowning etc.); liability to mining company, community, environment and government Safe to environment; possible drinking water; recreation & tourism - water sports; resource for mining company, government; and community KNOWING THE RESOURCE Liability & Wasted Resource UNSUSTAINABLE Beneficial & Optimum Use of Water SUSTAINABLE FIG 5 - Management for realisation of water resources from Australian pit lakes. Water in Mining Conference Perth, WA, 15 - 17 September 2009 251 R N KUMAR, C D McCULLOUGH and M A LUND • addressing many problems of water quality such as AMD in pit lakes by considering and addressing these possibilities in the planning stages of open-pit mining development, • development of a nationwide inventory for pit lakes across Australia including determining the number and distribution (regionally and geographically) of pit lakes, • developing and trialling new rehabilitation and water quality remediation technologies, and • developing and trialling beneficial end uses. As a result of current and likely future mining practices pit lakes will continue to increase in distribution, frequency and size in Australia. Australia experiences relatively low rainfall in many areas and coupled with an increasing demand for water which is rapidly developing into a very valuable resource, including for the mining industry (Barger, 2006). Water in the pit lakes can therefore either be a liability or a resource depending on how it is managed. Sustainable pit lake management has the potential to provide great benefit to mining companies, regulating agencies and communities but this will only be realised through pro-active involvement by the mining industry and through leadership by State and Commonwealth regulators. REFERENCES Australian and New Zealand Environment and Conservation Council (ANZECC)/Agriculture and Resource Management Council of Australia and New Zealand (ARMCANZ), 2000. Australian and New Zealand guidelines for fresh and marine water quality, National Water Quality Management Strategy Paper No 4 (Australian and New Zealand Environment and Conservation Council and Agriculture and Resource Management Council of Australia and New Zealand: Canberra). Australian Mines Atlas, 2009. Australian Mines Atlas [online]. Available from: <http://www.australianminesatlas.gov.au/?site=atlas> [Accessed: 7 July 2009]. 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