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Статті в журналах з теми "Artesian Mound Springs"
Fensham, R. J., R. J. Fairfax, D. Pocknee, and J. Kelley. "Vegetation patterns in permanent spring wetlands in arid Australia." Australian Journal of Botany 52, no. 6 (2004): 719. http://dx.doi.org/10.1071/bt04043.
Повний текст джерелаSaruwatari, Kazuko, Yukihiro Mizuochi, Yasunori Mahara, Teruyoshi Hatano, Takuma Hasegawa, Hirohisa Kobayashi, Atsushi Ninomiya, et al. "The Great Artesian Basin and the Limestone Mound Springs, Australia." Journal of the Geological Society of Japan 110, no. 4 (2004): VII—VIII. http://dx.doi.org/10.5575/geosoc.110.4.vii_viii.
Повний текст джерелаNoble, JC, MA Habermehl, CD James, J. Landsberg, AC Langston, and SR Morton. "Biodiversity implications of water management in the Great Artesian Basin." Rangeland Journal 20, no. 2 (1998): 275. http://dx.doi.org/10.1071/rj9980275.
Повний текст джерелаHarris, CR. "Mound Springs: South Australian Conservation Initiatives." Rangeland Journal 14, no. 2 (1992): 157. http://dx.doi.org/10.1071/rj9920157.
Повний текст джерелаRutherford, Jasmine, Tania Ibrahimi, Tim Munday, Adrienne Markey, Andrea Viezzoli, Arianna Rapiti, and Rod Paterson. "An Assessment of Water Sources for Heritage Listed Organic Mound Springs in NW Australia Using Airborne Geophysical (Electromagnetics and Magnetics) and Satellite Remote Sensing Methods." Remote Sensing 13, no. 7 (March 28, 2021): 1288. http://dx.doi.org/10.3390/rs13071288.
Повний текст джерелаShand, P., A. J. Love, T. Gotch, M. D. Raven, J. Kirby, and K. Scheiderich. "Extreme Acidic Environments Associated with Carbonate Mound Springs in the Great Artesian Basin, South Australia." Procedia Earth and Planetary Science 7 (2013): 794–97. http://dx.doi.org/10.1016/j.proeps.2013.03.055.
Повний текст джерелаMudd, G. M. "Mound springs of the Great Artesian Basin in South Australia: a case study from Olympic Dam." Environmental Geology 39, no. 5 (March 14, 2000): 463–76. http://dx.doi.org/10.1007/s002540050452.
Повний текст джерелаKeppel, Mark N., Karl Karlstrom, Laura Crossey, Andrew J. Love, and Stacey Priestley. "Evidence for intra-plate seismicity from spring-carbonate mound springs in the Kati Thanda–Lake Eyre region, South Australia: implications for groundwater discharge from the Great Artesian Basin." Hydrogeology Journal 28, no. 1 (November 6, 2019): 297–311. http://dx.doi.org/10.1007/s10040-019-02049-1.
Повний текст джерелаInverarity, Kent, Michael Hatch, and Graham Heinson. "Electrical geophysics of carbonate mound spring complexes of the South- Western Great Artesian Basin." ASEG Extended Abstracts 2013, no. 1 (December 2013): 1–4. http://dx.doi.org/10.1071/aseg2013ab190.
Повний текст джерелаPrescott, J. R., and M. A. Habermehl. "Luminescence dating of spring mound deposits in the southwestern Great Artesian Basin, northern South Australia." Australian Journal of Earth Sciences 55, no. 2 (March 2008): 167–81. http://dx.doi.org/10.1080/08120090701689340.
Повний текст джерелаДисертації з теми "Artesian Mound Springs"
Stoate, K. M. "The mound springs of South Australia: their electromagnetic signature and fractal dimension." Thesis, 2011. http://hdl.handle.net/2440/97933.
Повний текст джерелаThe importance of groundwater to remote and regional Australia cannot be understated, due to the intermittent and unreliable rainfall in these areas, as well as the unreliability of other water sources. As such the major source of water is groundwater from the Great Artesian Basin (GAB). The natural discharge of the GAB is through mound springs, unique landforms comprised of precipitated carbonates that are primarily located along the south western edge of the GAB. Due to the cultural, economic and environmental significance of these features it is important to fully understand their underlying hydrogeological structure. Geophysical studies have the potential to provide non-invasive imaging of these specific aspects of the GAB. A number of different methods were used to collect data from the springs. For this particular study a set of shallow electromagnetic data was collected. These data were processed conventionally, however to provide additional information they were also processed to extract the fractal dimension information of the data. The fractal dimension is used here as an indicator of roughness or texture with a dataset, thus differentiating between a homogenous and heterogeneous earth. All of the data were compared, including conductivity, in-phase, fractal dimension and the regolith of the area. It was hoped that this would provide added depth to the understanding of the mound springs as well as trialling an alternate method of processing data. Although the data collected did show some correlations, especially in regards to the relationships between the conductivity and the EM signature of the mound springs, there was a lack of consistent correlation between the fractal dimension and the other data sets that did not allow for conclusions as to the usefulness of fractal dimension as a means of processing data. This may be due to the small survey size of the area, thus testing on larger areas may be worthwhile in the future.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Earth and Environmental Sciences, 2011
Lampe, R. J. "Monitoring groundwater flow using electrokinetics." Thesis, 2011. http://hdl.handle.net/2440/96682.
Повний текст джерелаVery little is known about the groundwater flow paths from the subsurface of the Great Artesian Basin to the surface basins throughout the Australian continent. The Wabma Kadarbu Mound Springs in northern South Australia lie at the south-west margin of the Great Artesian Basin and contain a number of springs that continually discharge groundwater over time. This work deals with the self potential (SP) method which was used along three intersecting lines in the area to help gain a better understanding of groundwater flow. The SP method responds to the electrokinetic phenomenon of streaming potential which can be applied to hydrogeological investigations to help evaluate the subsurface groundwater flow conditions. Because the SP data do not intrinsically yield a good indication of the depth of the sources generating groundwater flow, numerical models are developed to assess the SP distribution resulting from subsurface fluid flow. The self-potential associated with groundwater flow in an electrolytic environment is modelled by assuming a primary source as an electric double layer between the flowing groundwater and the porous media created by the flowing SP currents. This primary flow generates the secondary surface charge and double layers on the interfaces between media with different conductivities. The geometry of the sources is obtained from an image reconstruction technique which determines the spatial locations of SP sources. The modelling and image reconstructions help to obtain a better understanding of these flow paths and how they make their way to the surface can give a greater chance of collecting the groundwater to use to good effect. The results showed evidence for groundwater flow networks in the subsurface of the Wabma Kadarbu springs. The groundwater flow networks for all three lines had similar characteristics including having individual columns connected at depth and large widths for the columns. This research showed that SP can be used to help better understand groundwater flow patterns in the subsurface.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Earth and Environmental Sciences, 2011
Частини книг з теми "Artesian Mound Springs"
Ponder, W. F. "Mound Springs of the Great Artesian Basin." In Limnology in Australia, 403–20. Dordrecht: Springer Netherlands, 1986. http://dx.doi.org/10.1007/978-94-009-4820-4_25.
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