Gotowe bibliografie tematyczne / Groundwater South Australia Willunga Basin

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Gotowa bibliografia na temat „Groundwater South Australia Willunga Basin”

Autor: Grafiati

Data publikacji: 4 czerwca 2021

Data aktualizacji: 30 stycznia 2023

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Artykuły w czasopismach na temat "Groundwater South Australia Willunga Basin"

Knowles, Ian, Michael Teubner, Aimin Yan, Paul Rasser, and Jong Wook Lee. "Inverse groundwater modelling in the Willunga Basin, South Australia." Hydrogeology Journal 15, no. 6 (May 22, 2007): 1107–18. http://dx.doi.org/10.1007/s10040-007-0189-6.

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Majoran, Stefan. "Cytheropterine ostracoda in view ofthe palaeoecology of the Palaeogene Port Willunga Formation, South Australia, and the palaeobathymetrical evolution of the Tasman Basin." Geobios 30, no. 3 (January 1997): 421–35. http://dx.doi.org/10.1016/s0016-6995(97)80203-3.

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Ordens, Carlos M., Adrian D. Werner, Vincent E. A. Post, John L. Hutson, Craig T. Simmons, and Benjamin M. Irvine. "Groundwater recharge to a sedimentary aquifer in the topographically closed Uley South Basin, South Australia." Hydrogeology Journal 20, no. 1 (November 3, 2011): 61–72. http://dx.doi.org/10.1007/s10040-011-0794-2.

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Halihan, Todd, Andrew Love, Mark Keppel, Meghan K. M. Dailey, Volmer Berens, and Daniel Wohling. "Evidence for groundwater mixing at Freeling Spring Group, South Australia." Hydrogeology Journal 28, no. 1 (December 4, 2019): 313–23. http://dx.doi.org/10.1007/s10040-019-02069-x.

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AbstractWater sampling at springs that are a part of the Freeling Spring Group, South Australia, was used along with electrical resistivity imaging (ERI) data to evaluate the sources and pathways for groundwater to the springs and to find evidence of mixing between the Great Artesian Basin (GAB) aquifer system (Algebuckina Sandstone, Cadna-owie Formation and lateral equivalents) and waters from the adjacent mountain block basement (MB) aquifer. Five springs and a well were used to evaluate spring chemistry; multi-electrode resistivity data were collected along three orientations over the Freel

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Petrides, B., I. Cartwright, and T. R. Weaver. "The evolution of groundwater in the Tyrrell catchment, south-central Murray Basin, Victoria, Australia." Hydrogeology Journal 14, no. 8 (July 19, 2006): 1522–43. http://dx.doi.org/10.1007/s10040-006-0057-9.

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Ahmed, Alaa, Chathuri Ranasinghe-Arachchilage, Abdullah Alrajhi, and Guna Hewa. "Comparison of Multicriteria Decision-Making Techniques for Groundwater Recharge Potential Zonation: Case Study of the Willochra Basin, South Australia." Water 13, no. 4 (February 18, 2021): 525. http://dx.doi.org/10.3390/w13040525.

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In semi-arid regions, groundwater resources play a crucial role in all economic, environmental, and social processes. However, the occurrence, movement, and recharge of these hidden and valuable resources vary from place to place. Therefore, better management practices and mapping of groundwater recharge potential zones are needed for the sustainable groundwater resources. For an example, groundwater resources in Willochra Basin are vitally important for drinking, irrigation, and stock use. This study shows the significance of the application of three decision-making approaches, including mult

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Walker, Glen. "A Potential Approach of Reporting Risk to Baseflow from Increased Groundwater Extraction in the Murray-Darling Basin, South-Eastern Australia." Water 14, no. 13 (July 2, 2022): 2118. http://dx.doi.org/10.3390/w14132118.

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An approach of reporting long-term trends in groundwater extraction and baseflow impacts in the Murray-Darling Basin (MDB) in south-eastern Australia was developed and tested. The principal aim of the framework was to provide early warning of any potential adverse impacts from groundwater extraction on environmental releases of surface water for baseflow, support adaptive management of these impacts, and highlight those areas which may benefit from conjunctive water management. The analysis showed that there is no current decadal trend in the annual aggregate groundwater extraction volumes or

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Herczeg, A. L., S. S. Dogramaci, and F. W. J. Leaney. "Origin of dissolved salts in a large, semi-arid groundwater system: Murray Basin, Australia." Marine and Freshwater Research 52, no. 1 (2001): 41. http://dx.doi.org/10.1071/mf00040.

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Hypotheses to explain the source of the 1011 tons of salt in groundwaters of the Murray Basin, south-eastern Australia, are evaluated; these are (a) mixing with original sea water, (b) dissolution of salt deposits, (c) weathering of aquifer minerals and (d) acquisition of solutes via rainfall. The total salinity and chemistry of many groundwater samples are similar to sea-water composition. However, their stable isotopic compositions (δ18O= –6.5 ‰; δ2H = –35) are typical of mean winter rainfall, indicating that all the original sea water has been flushed out of the aquifer. Br/Cl mass ratios a

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Walker, Glen R., Avril C. Horne, Quan J. Wang, and Rob Rendell. "Assessing the Impact of Irrigation Efficiency Projects on Return Flows in the South-Eastern Murray–Darling Basin, Australia." Water 13, no. 10 (May 14, 2021): 1366. http://dx.doi.org/10.3390/w13101366.

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Improving irrigation efficiency (IE) is an approach used globally to help meet competing demands for water and facilitate reallocation of water between sectors. In the Murray–Darling Basin in Australia, the Australian government has invested heavily in IE projects to recover water for the environment. However, this approach has been seriously questioned, out of concerns that improved IE would reduce irrigation return flows to rivers and therefore offset water recovery. In this study, we use a water balance model to assess the impact of the IE projects on return flows and highlight sensitivitie

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Knowling, Matthew J., Adrian D. Werner, and Daan Herckenrath. "Quantifying climate and pumping contributions to aquifer depletion using a highly parameterised groundwater model: Uley South Basin (South Australia)." Journal of Hydrology 523 (April 2015): 515–30. http://dx.doi.org/10.1016/j.jhydrol.2015.01.081.

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Rozprawy doktorskie na temat "Groundwater South Australia Willunga Basin"

James-Smith, Julianne Marie. "Development of a water management model for the evaluation of streamflow for aquifer storage and recovery." Title page, contents and abstract only, 2002. http://web4.library.adelaide.edu.au/theses/09ENS/09ensj291.pdf.

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Addendum on back page. Includes bibliography. Groundwater levels within the Willunga Basin, South Australia, are declining due to excessive extraction of water for irrigation purposes. An alternative source of water is needed to supplement the declining levels to ensure the sustainability of the groundwater system. A model was developed to evaluate the potential for using aquifer storage and recovery in conjunction with the surface storage of streamflow as a possible alternative water source. The application of this model to the largest catchment in the Willinga basin shows that sufficient str

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Bush, Angela L. "Physical and chemical hydrogeology of the Otway Basin, southeast Australia." Connect to thesis, 2009. http://repository.unimelb.edu.au/10187/8523.

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The Otway Basin of southeast Australia is the subject of this thesis, which incorporates pre-existing geological, hydraulic and major element hydrogeological data with new isotope hydrogeochemical investigations. The region is an Upper Cretaceous–Tertiary basin, filled with siliciclastic and calcareous aquifers and aquitards and characterised by late volcanic activity, pervasive faulting and karstification. (For complete abstract open document.)

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Finlay, Alison Janet. "Carbonate geochemistry of the tertiary (late eocene to early oligocene) section at Maslin and Aldinga Bays, the Willunga embayment of the St. Vincent Basin, South Australia /." Title page, contents and abstract only, 1993. http://web4.library.adelaide.edu.au/theses/09SB/09sbf511.pdf.

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Thesis (B. Sc.(Hons.))--University of Adelaide, Dept. of Geology and Geophysics, 1994. National grid reference : Barker Street 1 54-13 (1:250 000). Includes bibliographical references (leaves 24-27).

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Rasser, Paul Edward. "Calibration of numerical models with application to groundwater flow in the Willunga Basin, South Australia." 2001. http://thesis.library.adelaide.edu.au/public/adt-SUA20030414.111541/index.html.

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Bibliography: 80-82. Electronic publication; full text available in PDF format; abstract in HTML format. The process of calibrating a numerical model is examined in this thesis with an application to the flow of groundwater in the Willunga Basin in South Australia. The calibration process involves estimating unknown parameters of the numerical model so that the output obtained from the model is comparable with data that is observed in the field. Three methods for calibrating numerical models are discussed, these being the steepest descent method, the nonlinear least squares method, and a new m

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Ellis, Timothy Willson. "Estimating groundwater recharge from alley farming systems in the southern Murray Basin Australia / Tim Ellis." 2001. http://hdl.handle.net/2440/22427.

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"June 2001" Bibliography: p. 165-183. xxviii, 250 p. : ill., plates (col.), maps (col.) ; 30 cm. Title page, contents and abstract only. The complete thesis in print form is available from the University Library. The aims of this study were to develop models for predicting groundwater recharge from alley farming systems in the Murray Basin and for designing alley farms that will result in a prescribed recharge reduction. --p. 158. Thesis (Ph.D.)--University of Adelaide, Dept. of Agronomy and Farming Systems, 2002

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Ellis, Timothy Willson. "Estimating groundwater recharge from alley farming systems in the southern Murray Basin Australia / Tim Ellis." Thesis, 2001. http://hdl.handle.net/2440/22427.

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"June 2001" Bibliography: p. 165-183. xxviii, 250 p. : ill., plates (col.), maps (col.) ; 30 cm. The aims of this study were to develop models for predicting groundwater recharge from alley farming systems in the Murray Basin and for designing alley farms that will result in a prescribed recharge reduction. --p. 158. Thesis (Ph.D.)--University of Adelaide, Dept. of Agronomy and Farming Systems, 2002

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Jasonsmith, Julia F. "Origins of salinity and salinisation processes in the Wybong Creek catchment, New South Wales, Australia." Phd thesis, 2010. http://hdl.handle.net/1885/49429.

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The Wybong Creek catchment is located in the upper Hunter Valley of New South Wales, Australia, and contains award winning beef and wine producing operations. Solute concentrations in Wybong Creek are often too high for irrigation use, however, with previous research showing that the saline and Na-Cl dominated water discharged from Wybong Creek decreases water quality in both the Goulburn and Hunter Rivers into which it flows. This study therefore aimed at identifying the source of solutes to the Wybong Creek catchment and the processes which cause salinisation of surface water, soil (regolith

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Części książek na temat "Groundwater South Australia Willunga Basin"

Morgan, Leanne K., Adrian D. Werner, Melinda J. Morris, and Michael D. Teubner. "Application of a Rapid-Assessment Method for Seawater Intrusion Vulnerability: Willunga Basin, South Australia." In Groundwater in the Coastal Zones of Asia-Pacific, 205–25. Dordrecht: Springer Netherlands, 2013. http://dx.doi.org/10.1007/978-94-007-5648-9_10.

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Werner, Adrian D., and Le Dung Dang. "Three-Dimensional Seawater Intrusion Modelling of Uley South Basin, South Australia." In Groundwater in the Coastal Zones of Asia-Pacific, 177–203. Dordrecht: Springer Netherlands, 2013. http://dx.doi.org/10.1007/978-94-007-5648-9_9.

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Guillaume, Joseph H. A., Alvar Closas, and Andrew McCallum. "Groundwater allocation in New South Wales, Australia." In Water Resources Allocation and Agriculture, 143–58. IWA Publishing, 2022. http://dx.doi.org/10.2166/9781789062786_0143.

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Abstract New South Wales has more than 100 years of history of water licensing and allocation. This chapter reflects on the approach to water allocation in the current groundwater sharing plans, including general principles and underlying reasoning for application elsewhere. Focus is on groundwater-specific issues for transition from open to regulated access, while embedded within broader water regulations and connections to surface water management. Water allocation is built around water sharing plans that determine extraction limits, with community consultation. Water rights are differentiated in terms of water sources and priority, separated from land ownership, and from time-varying water allocations, subject to available water determinations. Both water entitlements and allocations can be traded, with rules governing impact of trade. Water sharing plans are state-level instruments explicitly connected in applicable regions to the Commonwealth-level Murray-Darling Basin Plan and associated extraction limits. Compliance is based firstly on metering of water extractions. Future prospects are also discussed.

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Dodds, A. R., and Dragon Ivic. "31. Integrated Geophysical Methods Used for Groundwater Studies in the Murray Basin, South Australia." In Geotechnical and Environmental Geophysics, 303–10. Society of Exploration Geophysicists, 1990. http://dx.doi.org/10.1190/1.9781560802785.ch31.

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Streszczenia konferencji na temat "Groundwater South Australia Willunga Basin"

"Modelling groundwater dependent ecosystems in the Willunga Basin, South Australia." In 20th International Congress on Modelling and Simulation (MODSIM2013). Modelling and Simulation Society of Australia and New Zealand (MSSANZ), Inc., 2013. http://dx.doi.org/10.36334/modsim.2013.l16.hamilton.

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"Field estimates of groundwater discharge – Great Artesian Basin, South Australia." In 19th International Congress on Modelling and Simulation. Modelling and Simulation Society of Australia and New Zealand (MSSANZ), Inc., 2011. http://dx.doi.org/10.36334/modsim.2011.e8.costelloe.

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Davis, Aaron, Kevin Cahill, and Tim Munday. "A Surface NMR Study for Groundwater Resource Assessment in the Uley Basin, South Australia." In Symposium on the Application of Geophysics to Engineering and Environmental Problems 2012. Environment and Engineering Geophysical Society, 2012. http://dx.doi.org/10.4133/1.4721757.

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