Groundwater hydrology
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This report presents groundwater level information collected during Geoscience Australia’s Musgrave Palaeovalley Project. The Musgrave Palaeovalley Project was conducted as part of Exploring for the Future (EFTF), an Australian Government funded geoscience data and information acquisition program. The eight-year, $225 million program aims to deliver new geoscience data and knowledge to inform decision-making by government, community, and industry on the sustainable development of Australia's mineral, energy, and groundwater resources.</div><div>Groundwater level data was collected during two hydrogeochemical surveys undertaken in March and May 2023 based around the remote communities of Warburton, Kaltukatjara, Wanarn, Blackstone and Jameson in Western Australia and the Northern Territory. Sixteen bores were measured for their groundwater levels. The results are contained herein and within the attached CSV file.
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<div>The Lake Eyre surface water catchment covers around 1,200,000 km2 of central Australia, about one-sixth of the entire continent. It is one of the largest endorheic river basins in the world and contains iconic arid streams such as the Diamantina, Finke and Georgina rivers, and Cooper Creek. The Lake Eyre region supports diverse native fauna and flora, including nationally significant groundwater-dependent ecosystems such as springs and wetlands which are important cultural sites for Aboriginal Australians.</div><div><br></div><div>Much of the Lake Eyre catchment is underlain by the geological Lake Eyre Basin (LEB). The LEB includes major sedimentary depocentres such as the Tirari and Callabonna sub-basins which have been active sites of deposition throughout the Cenozoic. The stratigraphy of the LEB is dominated by the Eyre, Namba and Etadunna formations, as well as overlying Pliocene to Quaternary sediments.</div><div><br></div><div>The National Groundwater Systems Project, part of Geoscience Australia's Exploring for the Future Program (https://www.eftf.ga.gov.au/), is transforming our understanding of the nation's major aquifer systems. With an initial focus on the Lake Eyre Basin, we have applied an integrated geoscience systems approach to model the basin's regional stratigraphy and geological architecture. This analysis has significantly improved understanding of the extent and thickness of the main stratigraphic units, leading to new insights into the conceptualisation of aquifer systems in the LEB.</div><div><br></div><div>Developing the new understanding of the LEB involved compilation and standardisation of data acquired from thousands of petroleum, minerals and groundwater bores. This enabled consistent stratigraphic analysis of the major geological surfaces across all state and territory boundaries. In places, the new borehole dataset was integrated with biostratigraphic and petrophysical data, as well as airborne electromagnetic (AEM) data acquired through AusAEM (https://www.eftf.ga.gov.au/ausaem). The analysis and integration of diverse geoscience datasets helped to better constrain the key stratigraphic horizons and improved our overall confidence in the geological interpretations.</div><div><br></div><div>The new geological modelling of the LEB has highlighted the diverse sedimentary history of the basin and provided insights into the influence of geological structures on modern groundwater flow systems. Our work has refined the margins of the key depocentres of the Callabonna and Tirari sub-basins, and shown that their sediment sequences are up to 400 m thick. We have also revised maximum thickness estimates for the main units of the Eyre Formation (185 m), Namba Formation (265 m) and Etadunna Formation (180 m).</div><div><br></div><div>The geometry, distribution and thickness of sediments in the LEB is influenced by geological structures. Many structural features at or near surface are related to deeper structures that can be traced into the underlying Eromanga and Cooper basins. The occurrence of neotectonic features, coupled with insights from geomorphological studies, implies that structural deformation continues to influence the evolution of the basin. Structures also affect the hydrogeology of the LEB, particularly by compartmentalising groundwater flow systems in some areas. For example, the shallow groundwater system of the Cooper Creek floodplain is likely segregated from groundwater in the nearby Callabonna Sub-basin due to structural highs in the underlying Eromanga Basin.</div><div> Abstract submitted and presented at the 2023 Australian Earth Science Convention (AESC), Perth WA (https://2023.aegc.com.au/)
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<div>This report details results and methodology from two hydrochemistry sampling programs performed as part of Geoscience Australia’s Musgrave Palaeovalley Project. The Musgrave Palaeovalley Project is a data acquisition and scientific investigation program based around the central west of Australia. It is aimed at investigating groundwater processes and resources within the Cenozoic fill and palaeovalleys of the region. This project, and many others, have been performed as part of the Exploring for the Future (EFTF) program, an eight-year, $225 million Australian Government funded geoscience data and precompetitive information acquisition program.</div><div>Data released here is from 18 bores sampled for groundwater and tested for a range of analytes including field parameters, major and minor elements, isotopes and trace gases. The sampling methods, quality assurance/quality control procedures, analytical methods and results are included in this report.</div>
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<div>Previous work by the SA government and CSIRO[i] highlighted the value of integrating AEM data with other geological and hydrogeological data to model palaeovalley groundwater systems and develop regional hydrogeological conceptualisations. This allows better-informed water supply decisions and management for communities in remote parts of Australia where these systems provide the only available and long-term water resource. The Exploring for the Future Musgrave Palaeovalley module seeks to apply similar work flows across the western Musgrave Province and adjacent Officer and Canning basins.</div><div>Open file mineral exploration AEM data from 11 surveys in WA and SA flown between 2009 and 2012 were re-processed and inverted to produce conductivity models and a suite of derived datasets. Geoscience Australia’s Layered-Earth-Inversion was used as a single standard processing and inversion method to improve continuity and data quality.</div><div>These legacy AEM data, originally for mineral exploration, have been incorporated with DEM-derived landscape attributes, previous palaeovalley mapping and available bore lithologies to model palaeovalley base surfaces. This presentation will provide an example from four blocks of AEM data to show how repurposing data from mineral exploration, public bore data and landscape analysis can be used to identify palaeovalley systems which provide critical water supplies for remote and regional communities and industry[ii].</div><div>This approach can be used to model palaeovalley systems from a range of geoscientific and other datasets. The Exploring for the Future Musgrave Palaeovalley module has acquired ~23,000 line km of AEM across parts of WA and the NT at line spacings of 1 and 5 km. This new precompetitive data will be used to model palaeovalley system geometry and integrate with new and existing AEM, drilling, landscape, groundwater chemistry and surface geophysics data to test hydrogeological conceptualisations of these groundwater systems.</div><div><br></div><div><br></div><div> [i] Costar, A., Love, A., Krapf, C., Keppel, M., Munday, T., Inverarity, K., Wallis, I. & Sørensen, C. (2019). Hidden water in remote areas – using innovative exploration to uncover the past in the Anangu Pitjantjatjara Yankunytjatjara Lands. MESA Journal 90(2), 23 - 35 pp.</div><div>Krapf, C., Costar, A., Stoian, L., Keppel, M., Gordon, G., Inverarity, K., Love, A. & Munday, T. (2019). A sniff of the ocean in the Miocene at the foothills of the Musgrave Ranges - unravelling the evolution of the Lindsay East Palaeovalley. MESA Journal 90(2), 4 - 22 pp.</div><div>Krapf, C. B. E., Costar, A., Munday, T., Irvine, J. A. & Ibrahimi, T., 2020. Palaeovalley map of the Anangu Pitjantjatjara Yankunytjatjara Lands (1st edition), 1:500 000 scale. Goyder Institute for Water Research, Geological Survey of South Australia, CSIRO.</div><div>https://sarigbasis.pir.sa.gov.au/WebtopEw/ws/samref/sarig1/wci/Record?r=0&m=1&w=catno=2042122. </div><div>Munday, T., Taylor, A., Raiber, M., Sørensen, C., Peeters, L. J. M., Krapf, C., Cui, T., Cahill, K., Flinchum, B., Smolanko, N., Martinez, J., Ibrahimi, T. & Gilfedder, M., 2020a. Integrated regional hydrogeophysical conceptualisation of the Musgrave Province, South Australia, Goyder Institute for Water Research Technical Report Series 20/04, Goyder Institute for Water Research, Adelaide.</div><div>Munday, T., Gilfedder, M., Costar, A., Blaikie, T., Cahill, K., Cui, T., Davis, A., Deng, Z., Flinchum, B., Gao, L., Gogoll, M., Gordon, G., Ibrahimi, T., Inverarity, K., Irvine, J., Janardhanan, Sreekanth, Jiang, Z., Keppel, M., Krapf, C., Lane, T., Love, A., Macnae, J., Mariethoz, G., Martinez, J., Pagendam, D., Peeters, L., Pickett, T., Robinson, N., Siade, A., Smolanko, N., Sorensen, C., Stoian, L., Taylor, A., Visser, G., Wallis, I. & Xie, Y., 2020b. Facilitating Long-term Outback Water Solutions (G-Flows Stage 3): Final Summary Report. Goyder Institute for Water Research, Adelaide, http://hdl.handle.net/102.100.100/376125?index=1. </div><div>[ii] Symington, N. J., Ley-Cooper, Y. A. & Smith, M. L., 2022. West Musgrave AEM conductivity models and data release. Geoscience Australia, Canberra, https://pid.geoscience.gov.au/dataset/ga/146278. </div> This Abstract was submitted/presented to the 2022 Sub 22 Conference 28-30 November (http://sub22.w.tas.currinda.com/)
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<div>This study investigates the feasibility of mapping potential groundwater dependent vegetation (GDV) at a regional scale using remote sensing data. Specifically, the Digital Earth Australia (DEA) Tasseled Cap Percentiles products, integrated with the coefficient of greenness and/or wetness, are applied in three case study regions in Australia to identify and characterise potential terrestrial and aquatic groundwater dependent ecosystems (GDE). The identified high potential GDE are consistent with existing GDE mapping, providing confidence in the methodology developed. The approach provides a consistent and rapid first-pass approach for identifying and assessing GDEs, especially in remote areas of Australia lacking detailed GDE and vegetation information.</div>
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<div>GeoInsight was an 18-month pilot project developed in the latter part of Geoscience Australia’s Exploring for the Future Program (2016–2024). The aim of this pilot was to develop a new approach to communicating geological information to non-technical audiences, that is, non-geoscience professionals. The pilot was developed using a human-centred design approach in which user needs were forefront considerations. Interviews and testing found that users wanted a simple and fast, plain-language experience which provided basic information and provided pathways for further research. GeoInsight’s vision is to be an accessible experience that curates information and data from across the Geoscience Australia digital ecosystem, helping users make decisions and refine their research approach, quickly and confidently. </div><div><br></div><div>In the first iteration of GeoInsight, selected products for energy, minerals, water, and complementary information from Geoscience Australia’s Data Discovery Portal and Data and Publications Catalogue were examined to (1) gauge the relevance of the information they contain for non-geoscientists and, (2) determine how best to deliver this information for effective use by non-technical audiences. </div><div><br></div><div>This Record documents the technical details of the methods used for summarising groundwater information for GeoInsight, including groundwater reliance, depth, salinity, and uses. This Record will be updated, including a change log, when the scope of information or methods for generating the data change.</div>
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<div>As part of the $225 million Exploring for the Future programme, Geoscience Australia have undertaken an investigation into the resource potential of the Officer-Musgrave-Birrindudu region. Part of this project focusses on characterising palaeovalley groundwater resources within the West Musgrave region of Australia. This GA Record is a technical report detailing the science undertaken as part of the Musgrave Palaeovalley groundwater project. The project aimed to improve understanding of the region's palaeovalley architecture, groundwater quality, and overall hydrogeology to support responsible water resource management. The most significant work undertaken included three-dimensional modelling of palaeovalley architecture, groundwater characterisation using hydrochemistry, groundwater model conceptualisation and a detailed review of local groundwater around remote communities in the region. This work will underpin responsible groundwater management into the future.</div>
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<div>Aboriginal and Torres Strait Islander peoples hold a wealth of traditional knowledge about their land and waters gathered and passed down from observations over thousands of years. Geoscience Australia (GA) is the national geoscience public sector organisation that advises on the geology, hydrogeology, and geography of Australia by applying science and technology to describe and understand the Earth. Respectful and successful two-way engagement with Indigenous peoples provides an opportunity to identify and share traditional understanding, complementing geoscientific studies and preserving traditional knowledge Through its Innovate Reconciliation Action Plan, GA is committed to building mutually beneficial relationships with Aboriginal and Torres Strait Islander peoples. Aligned with this vision, and as part of the Exploring for the Future Program, GA engaged a subject matter expert to undertake a scoping study. The aim of this study was to provide advice to strengthen the internal processes it uses to engage and undertake projects with Indigenous peoples. Drawing on two case studies (northeast NSW; eastern WA), a framework was developed to guide GA staff in the collection and recording of information and knowledge in a culturally appropriate manner. The project also delivered a road map to achieve better engagement and inclusion of Indigenous peoples in geoscience studies, to be tested and refined in future work programs. The road map is built on six key elements: (1) increasing Indigenous employment; (2) building partnerships; (3) respecting timeframes; (4) embedding Indigenous values and culture; (5) adhering to ethical practices and principles; and (6) embracing two-way knowledge sharing. Trust is crucial to building a partnership with Indigenous communities, binding the six elements of the road map. In the future GA hopes to share the outcomes with other organisations, from applying the framework and road map aimed at improving engagement with Indigenous peoples in groundwater activities and the geosciences more broadly. Presented at the 2022 Australasian Groundwater Conference (AGC)
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<div>Groundwater is critical to the survival of a range of ecosystems in Australia through provision of a direct source of water to plants with suitable root systems, and through discharge into surface water systems. Effectively managing groundwater dependent ecosystems (GDEs) alongside other water demands requires the ability to identify, characterise, and monitor vegetation condition. <em> </em><br> As part of the <a href="https://www.eftf.ga.gov.au/upper-darling-river-floodplain-groundwater-study">Exploring for the Future Upper Darling Floodplain</a> (UDF) groundwater project in western New South Wales, we present results from a study testing the suitability of two novel methods (a) recently available tasselled cap percentile products with national coverage through Digital Earth Australia, and (b) dry-conditions interferometric radar (InSAR) coherence images for mapping vegetation that is potentially groundwater dependent. <em> </em></div><div><em> </em></div><div>A combination of greenness and wetness 10th percentile tasselled cap products delineated terrestrial and aquatic GDEs with greater accuracy than existing regional ecosystem mapping, demonstrating the utility of these products for GDE identification. These results suggest the tasselled cap products can be used to support and refine the existing GDE mapping for this region, and further testing of their suitability and application for other regions is warranted. <em> </em></div><div><em> </em></div><div>The InSAR coherence images produced good agreement with the Bureau of Meteorology national GDE Atlas for areas of high probability of groundwater dependence. Although data availability and technical expertise currently lags behind optical imagery products, if research continues to show good performance in mapping potential GDEs and other applications, InSAR could become an important line of evidence within multi-dataset investigations. <em> </em></div><div><em> </em></div><div>Key next steps for improving the utility of these techniques are (a) comparison with vegetation condition data, and (b) further assessment of the likelihood of groundwater dependence through assessing relationships between vegetation condition and groundwater, surface water, and soil moisture availability.<em> </em></div><div> </div><div>This abstract was submitted/presented to the 2023 Australasian Groundwater / New Zealand Hydrological Society (AGC NZHS) Joint Conference (https://www.hydrologynz.org.nz/events-1/australasian-groundwater-nzhs-joint-conference)</div>
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<div>The Darling River is the primary water source for communities on the Upper Darling River Floodplain (UDF) in arid northwest New South Wales. A 70% reduction in mean annual flow down the Darling over the past 80 years, due to droughts and over-extraction, has resulted in critical water shortages and water quality issues for communities and ecosystems. Presently there is a limited understanding of the spatial extent and controls on the occurrence of lower salinity groundwater within the surrounding Darling Alluvium; a possible alternative water source that is also important to groundwater-dependent ecosystems.</div><div> </div><div>The UDF project, part of the Australian Government’s Exploring for the Future program is working in collaboration with State partners to collect and integrate new data with existing hydrogeological knowledge. The project aims to improve the hydrogeological understanding of the region to help inform water management decisions and increase water security. A key focus of the project is the Darling Alluvium (DA)—a closed regional groundwater system comprising unconsolidated Cenozoic sediments deposited primarily by the paleo and current Darling River systems and their tributaries. Connectivity with aquifers of varying quality, within the underlying Murray and Great Artesian Basins, is also being investigated. </div><div> </div><div>Integration of airborne electromagnetic (AEM), hydrometric and hydrochemical data with lithology logs and geological maps has revealed a broad trend in groundwater–surface water dynamics. In the upper reaches of the floodplain systems appear to be disconnected, while in the lower reaches losing stream conditions prevail. In the losing stream setting, resistive AEM signatures, at depths of up to 60 m below ground level and extending laterally for several hundred metres from the river, indicate a hydraulic gradient away from the river. Low salinity groundwater measured in shallow bores suggest the potential for a significant quality groundwater resource. Further investigations will improve confidence in the geometry of fresh water zones, recharge rates, connectivity with underlying saline aquifers and relationships with groundwater-dependent ecosystems. </div><div><br></div>This Abstract was submitted/presented to the 2022 Australasian Groundwater Conference 21-23 November (https://www.aig.org.au/events/australasian-groundwater-conference-2022/)