Gotowe bibliografie tematyczne / Great Artesian Basin

Gotowa bibliografia na temat „Great Artesian Basin”

Autor: Grafiati
Data publikacji: 4 czerwca 2021
Data aktualizacji: 20 lutego 2023

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Artykuły w czasopismach na temat "Great Artesian Basin"

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Dafny, Elad. "The Great Artesian Basin: is it that great?" Hydrogeology Journal 24, nr 6 (14.07.2016): 1329–32. http://dx.doi.org/10.1007/s10040-016-1444-5.

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Mazor, Emanuel. "Stagnant aquifer concept Part 1. Large-scale artesian systems— Great Artesian Basin, Australia". Journal of Hydrology 173, nr 1-4 (grudzień 1995): 219–40. http://dx.doi.org/10.1016/0022-1694(95)02706-u.

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Fensham, R. J., R. J. Fairfax i P. R. Sharpe. "Spring wetlands in seasonally arid Queensland: floristics, environmental relations, classification and conservation values". Australian Journal of Botany 52, nr 5 (2004): 583. http://dx.doi.org/10.1071/bt03171.

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The vegetation and environmental setting of permanent spring wetlands are described from a survey of 269 spring complexes throughout seasonally arid Queensland. Wetlands associated with springs in the western and southern discharge areas of the Great Artesian Basin are floristically distinct from other spring wetlands. Ordination analysis suggests that the biogeographic regions and the broad geological substrates that support spring wetlands provide a meaningful representation of floristic range. An existing classificatory system that defines ‘regional ecosystems’ on the basis of the biogeographic region and broad geological substrate is adopted to define 15 spring-wetland types in seasonally arid Queensland. The conservation value of the springs is assessed by a scheme that weights plant species populations on the basis of their endemicity and isolation from other populations, demonstrating that both Great Artesian Basin and non-Great Artesian Basin springs have similar conservation values.
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Fensham, R. J., i R. J. Fairfax. "Spring wetlands of the Great Artesian Basin, Queensland, Australia". Wetlands Ecology and Management 11, nr 5 (październik 2003): 343–62. http://dx.doi.org/10.1023/b:wetl.0000005532.95598.e4.

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PONDER, W. F., W. H. ZHANG, A. HALLAN i M. E. SHEA. "New taxa of Tateidae (Caenogastropoda, Truncatelloidea) from springs associated with the Great Artesian Basin and Einasleigh Uplands, Queensland, with the description of two related taxa from eastern coastal drainages". Zootaxa 4583, nr 1 (10.04.2019): 1. http://dx.doi.org/10.11646/zootaxa.4583.1.1.

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Species from artesian springs associated with the Queensland Great Artesian Basin that were previously included in the tateid genus Jardinella are included in three new genera, namely Eulodrobia, with six species, five of them new and all from the Eulo Supergroup; Springvalia, with one species from the Springvale Supergroup; and Carnarvoncochlea with two previously-described species, from the Carnarvon Supergroup. The genus Edgbastonia is extended to include eight previously described species, in addition to the type species, and four new species-group taxa from the Barcaldine Supergroup springs; all but the type species are included in the new subgenus Barcaldinia. Three new species from non-artesian springs in north Queensland are included in Edgbastonia, one of them tentatively. Two additional related new genera, both with a single new species, are described from outside the Great Artesian Basin; Conondalia from southeast Queensland and Nundalia from north-eastern New South Wales. The genus Jardinella, previously used for all the Queensland spring tateids, is here restricted to three species found in coastal rivers and streams in northeast Queensland. A molecular phylogenetic analysis using COI and 16S mitochondrial genes in combination suggests that the Queensland Great Artesian Basin taxa may be more closely related to the tateid genera Austropyrgus, Pseudotricula, Posticobia and Potamopyrgus than to the South Australian GAB taxa, thus indicating the separate origins of these two desert spring faunas.
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Henderson, Robert A., i E. Donald McKenzie. "Idanoceras, a new heteromorph ammonite genus from the Late Albian of eastern Australia". Journal of Paleontology 76, nr 5 (wrzesień 2002): 906–9. http://dx.doi.org/10.1017/s0022336000037574.

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The late Albian marine fossil record from eastern Australia derives from the sedimentary succession of the Great Artesian Basin deposited in a vast epicontinental sea which then covered much of the continent (see Frakes et al., 1987). Ammonites of this age are common but their generic diversity is low. Heteromorph assemblages almost exclusively comprise the taxa Myloceras, Labeceras sensu stricto and Labeceras (Appurdiceras) of the Family Labeceratidae that were widely distributed in higher latitudes of the Southern Hemisphere during Late Albian time (see Aguirre Urreta and Riccardi, 1988; Klinger, 1989). Some 19 endemic species of these genera are recorded from the Great Artesian Basin in the present literature (Etheridge, 1892; Whitehouse, 1926; Reyment, 1964) and there are additional undescribed species (Henderson and McKenzie, unpublished data). The Australian Late Albian epicontinental sea was clearly a site of significant speciation for Labeceras and Myloceras and it has been argued that the Great Artesian Basin represents the evolutionary center for these genera (Henderson, 1990).
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Noble, JC, MA Habermehl, CD James, J. Landsberg, AC Langston i SR Morton. "Biodiversity implications of water management in the Great Artesian Basin." Rangeland Journal 20, nr 2 (1998): 275. http://dx.doi.org/10.1071/rj9980275.

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The Great Artesian Basin (GAB) underlies a vast, mainly arid, region where most of the indigenous biota are not dependent upon surface water. In contrast, an important minority is dependent on refuges such as mound springs and their associated wetlands. In some parts of the GAB, such as western New South Wales, many springs have either ceased to flow, or are now barely detectable, because the proliferation of artesian waterbores has reduced groundwater pressures. Because of the rarity of species endemic to mound springs, and the damage they have suffered since pastoral settlement, emphasis should be directed towards conservation and possible rejuvenation of these ecosystems. Provision of artificial sources of water allows more widespread grazing by livestock, larger native and feral herbivores, thereby posing threats to native plants and animals that do not use the water. Because of the proliferation of artificial waters and the grazing they allow, terrestrial grazing-sensitive species now appear to be confined to tiny patches in the landscape. Some nature reserves within the GAB retain numerous artificial sources of water. Most of these should be closed over time to reduce negative impacts on grazing-sensitive plants and animals, especially where these species are inadequately protected elsewhere. In those regions where the ratio of artificial to natural waters is still low, consideration should be given to balancing provision of water for livestock with conservation of biological diversity, by maintaining a patchwork of areas remote from water. In regions where the density of artificial waters is high, conservation of biodiversity on freehold and leasehold lands might be enhanced with a mix of approaches accommodating the needs of the biota and the aspirations of landholders, tailored according to land type and condition. Key words: Great Artesian Basin, biological diversity, mound springs, refuges, rare biota, grazing impact, conservation management, groundwater.
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Saruwatari, Kazuko, Yukihiro Mizuochi, Yasunori Mahara, Teruyoshi Hatano, Takuma Hasegawa, Hirohisa Kobayashi, Atsushi Ninomiya i in. "The Great Artesian Basin and the Limestone Mound Springs, Australia". Journal of the Geological Society of Japan 110, nr 4 (2004): VII—VIII. http://dx.doi.org/10.5575/geosoc.110.4.vii_viii.

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Ordens, Carlos Miraldo, Neil McIntyre, Jim R. Underschultz, Tim Ransley, Catherine Moore i Dirk Mallants. "Preface: Advances in hydrogeologic understanding of Australia’s Great Artesian Basin". Hydrogeology Journal 28, nr 1 (22.01.2020): 1–11. http://dx.doi.org/10.1007/s10040-019-02107-8.

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Herczeg, A. L., T. Torgersen, A. R. Chivas i M. A. Habermehl. "Geochemistry of ground waters from the Great Artesian Basin, Australia". Journal of Hydrology 126, nr 3-4 (wrzesień 1991): 225–45. http://dx.doi.org/10.1016/0022-1694(91)90158-e.

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Rozprawy doktorskie na temat "Great Artesian Basin"

1

Kanso, Sungwan, i n/a. "Molecular Studies of Bacterial Communities in the Great Artesian Basin Aquifers". Griffith University. School of Biomolecular and Biomedical Science, 2004. http://www4.gu.edu.au:8080/adt-root/public/adt-QGU20040219.140509.

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16S rRNA gene analysis has shown that bacterial diversity in the GAB bores studied was limited to the genera Hydrogenobacter in the phylum Aquificae, Thermus in the phylum Deinococcus-Thermus, Desulfotomaculum in the phylum Firmicutes, the alpha-, beta- and gamma-classes of the phylum Proteobacteria and the phylum Nitrospirae. There was no clone closely related to members of the delta-proteobacteria and epsilon-proteobacteria classes detected. The number of bacterial strains directly isolated from the Fairlea and the Cooinda bores were far less than the numbers of distinctive phylotypes detected by the 16S rRNA gene characterisation. In addition none of the bacterial strains directly isolated from the water samples were represented in the 16S rRNA gene clone libraries. Similar discrepancies between the bacterial populations obtained from the 16S rRNA gene analysis and those obtained from direct isolation have been reported in the literature (Dunbar et al., 1999; Kampfer et al., 1996; Suzuki et al., 1997; Ward et al., 1998; Ward et al., 1997). However, in general, the phyla with which the isolates were affiliated were the same as those phyla to which the clones belonged. The environmental changes introduced (by bringing the artesian water up to the surface and exposing it to four types of metal coupons made of carbon steels identified by codes ASTM-A53B, ASTM-A53, AS-1074 and AS-1396 and commonly used in bore casings) led to changes in the bacterial community structures. In general, the species which proliferated in the communities before and after the changes were different. The diversity of the bacterial species in the community decreased following the environmental changes. Clones dominating the clone libraries constructed from newly established bacterial communities also differed from the clones dominating the libraries constructed from the bacterial communities which had existed naturally in the bores. These trends toward change in the bacterial communities were observed at both the Fairlea and the Cooinda bore sites. All four metal types incubated in the Fairlea bore water lost between 3.4 and 4.7% of their original weight. In contrast none of the metals incubated in Cooinda bore water lost weight. Clone library A1 showed that the natural population of the Fairlea bore was dominated by clone A1-3, which represented a novel species related to the isolate boom-7m-04. But after metal incubation (and recording of the metal weight loss), the bacterial community was dominated by clone PKA34B, which has a 95% similarity in its 16S rRNA gene sequence with Desulfotomaculum putei. Desulfotomaculum species are known to cause metal corrosion due to their byproduct H2S. But the low level of phylogenetic relatedness found does not provide enough information to speculate on whether the species represented by clone PKA34B is a member of the genus Desulfotomaculum or not. However, the fact that clone PKA34B dominated the PKA clone library by 50% makes the species it represents a suspected candidate likely to be involved with the metal weight loss at the Fairlea bore. In contrast, clone library 4381 showed that the natural population of the Cooinda bore was dominated by clone 4381-15 representing a species distantly related to a hydrogen oxidiser Hydrogenophaga flava (95% similarity). The dominating clone of the new community formed after metal incubation was clone COO25, which has 99% similarity with Thermus species that have not been reported to be involved with metal corrosion to my knowledge. In this project detection, identification and comparative quantification by 16S rRNA gene-targeted PCR probing with probes 23B and 34B were successfully developed for a Leptothrix-like species and for a Desulfotomaculum-like species represented by clones PKA23B and PKA34B respectively. This method of probing permits a fast, sensitive and reproducible detection, identification and at least a comparative quantification of the bacteria in the environment without the need for culturing. Therefore it is extremely suitable for use in bacterial population monitoring. PCR probing with the 34B probe has a potential commercial use as a means of screening for bores with a potential high risk of corrosion due to this Desulfotomaculum-like species. Direct isolation of bacteria from the GAB water has resulted in the isolation of seven strains from the Fairlea bore and eight from the Cooinda bore. Among these isolates, three novel strains were studied in detail. Reports on the characterisation of strain FaiI4T (T=Type strain) from the Fairlea bore (Kanso & Patel, 2003) and strain CooI3BT from the Cooinda bore have been published (Kanso et al., 2002). The data generated during this project add to our current information and extend our knowledge about the bacterial communities of the GAB's sub-surface environment. This information will provide a basis for further ecological studies of the GAB. Studies on involvement of certain groups of bacteria with the corrosion of metals used in bore casings could provide a foundation for further studies to develop maintenance and managing strategies for the GAB bores.
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Kanso, Sungwan. "Molecular Studies of Bacterial Communities in the Great Artesian Basin Aquifers". Thesis, Griffith University, 2004. http://hdl.handle.net/10072/366613.

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16S rRNA gene analysis has shown that bacterial diversity in the GAB bores studied was limited to the genera Hydrogenobacter in the phylum Aquificae, Thermus in the phylum Deinococcus-Thermus, Desulfotomaculum in the phylum Firmicutes, the alpha-, beta- and gamma-classes of the phylum Proteobacteria and the phylum Nitrospirae. There was no clone closely related to members of the delta-proteobacteria and epsilon-proteobacteria classes detected. The number of bacterial strains directly isolated from the Fairlea and the Cooinda bores were far less than the numbers of distinctive phylotypes detected by the 16S rRNA gene characterisation. In addition none of the bacterial strains directly isolated from the water samples were represented in the 16S rRNA gene clone libraries. Similar discrepancies between the bacterial populations obtained from the 16S rRNA gene analysis and those obtained from direct isolation have been reported in the literature (Dunbar et al., 1999; Kampfer et al., 1996; Suzuki et al., 1997; Ward et al., 1998; Ward et al., 1997). However, in general, the phyla with which the isolates were affiliated were the same as those phyla to which the clones belonged. The environmental changes introduced (by bringing the artesian water up to the surface and exposing it to four types of metal coupons made of carbon steels identified by codes ASTM-A53B, ASTM-A53, AS-1074 and AS-1396 and commonly used in bore casings) led to changes in the bacterial community structures. In general, the species which proliferated in the communities before and after the changes were different. The diversity of the bacterial species in the community decreased following the environmental changes. Clones dominating the clone libraries constructed from newly established bacterial communities also differed from the clones dominating the libraries constructed from the bacterial communities which had existed naturally in the bores. These trends toward change in the bacterial communities were observed at both the Fairlea and the Cooinda bore sites. All four metal types incubated in the Fairlea bore water lost between 3.4 and 4.7% of their original weight. In contrast none of the metals incubated in Cooinda bore water lost weight. Clone library A1 showed that the natural population of the Fairlea bore was dominated by clone A1-3, which represented a novel species related to the isolate boom-7m-04. But after metal incubation (and recording of the metal weight loss), the bacterial community was dominated by clone PKA34B, which has a 95% similarity in its 16S rRNA gene sequence with Desulfotomaculum putei. Desulfotomaculum species are known to cause metal corrosion due to their byproduct H2S. But the low level of phylogenetic relatedness found does not provide enough information to speculate on whether the species represented by clone PKA34B is a member of the genus Desulfotomaculum or not. However, the fact that clone PKA34B dominated the PKA clone library by 50% makes the species it represents a suspected candidate likely to be involved with the metal weight loss at the Fairlea bore. In contrast, clone library 4381 showed that the natural population of the Cooinda bore was dominated by clone 4381-15 representing a species distantly related to a hydrogen oxidiser Hydrogenophaga flava (95% similarity). The dominating clone of the new community formed after metal incubation was clone COO25, which has 99% similarity with Thermus species that have not been reported to be involved with metal corrosion to my knowledge. In this project detection, identification and comparative quantification by 16S rRNA gene-targeted PCR probing with probes 23B and 34B were successfully developed for a Leptothrix-like species and for a Desulfotomaculum-like species represented by clones PKA23B and PKA34B respectively. This method of probing permits a fast, sensitive and reproducible detection, identification and at least a comparative quantification of the bacteria in the environment without the need for culturing. Therefore it is extremely suitable for use in bacterial population monitoring. PCR probing with the 34B probe has a potential commercial use as a means of screening for bores with a potential high risk of corrosion due to this Desulfotomaculum-like species. Direct isolation of bacteria from the GAB water has resulted in the isolation of seven strains from the Fairlea bore and eight from the Cooinda bore. Among these isolates, three novel strains were studied in detail. Reports on the characterisation of strain FaiI4T (T=Type strain) from the Fairlea bore (Kanso & Patel, 2003) and strain CooI3BT from the Cooinda bore have been published (Kanso et al., 2002). The data generated during this project add to our current information and extend our knowledge about the bacterial communities of the GAB's sub-surface environment. This information will provide a basis for further ecological studies of the GAB. Studies on involvement of certain groups of bacteria with the corrosion of metals used in bore casings could provide a foundation for further studies to develop maintenance and managing strategies for the GAB bores.
Thesis (PhD Doctorate)
Doctor of Philosophy (PhD)
School of Biomolecular and Biomedical Sciences
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3

Alonaizi, Thnayan. "Heavy Metal Bioremediation by Anaerobic-Thermophilic Bacteria from the Great Artesian Basin". Thesis, Griffith University, 2019. http://hdl.handle.net/10072/386067.

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Bioremediation is considered an effective environmental remedial strategy when compared with physical and chemical techniques. Microorganisms can remove and detoxify pollutants by transforming or degrading them. A large portion of these toxic pollutants are heavy metals that are present naturally or due to anthropogenic activities. Bacteria inhabiting areas that have high levels of heavy metals have adapted to resist and reduce these pollutants. In the current, study heavy metal transforming bacteria have been isolated, characterised and investigated for bioremediation and biodegradation capabilities. The Great Artesian Basin (GAB) in Australia is a unique thermal site that harbours diverse microbial communities. Anaerobic and facultative anaerobic, thermophilic and thermotolerant bacteria were isolated from groundwaters and run-off waters from the GAB region. A total of 6 bacteria were isolated and identified as belonging to Anoxybacillus, Thermobrachium, Caloramator, and Virgibacillus genera using the 16S rRNA. Heavy metal reduction capacity was tested on all of the isolates. Strain VY was best at reducing vanadium(V), up to 10mM. Strain COY reduced up to 8 mM of cobalt(III). Strain SEY showed the most significant reduction of selenium(III). Strain FEY had the highest extent of iron(III) reduction. Strains CRG and CRL could reduce chromium(VI) most efficiently. Additional tests were done to fortify the selection of an optimal candidate for heavy metal bioremediation. These tests included biosurfactant production, for which all strains exhibited at least a 32% reduction in surface tension after 24 hours. The second test was biofilm formation where strains SEY and CRG performed best forming a medium rated biofilm under aerobic conditions but a poor biofilm under anaerobic conditions. A third test was to measure the chemotactic ability of the strains and strain SEY demonstrated the ability to possess a chemical attraction towards iron(III). From the characterisation tests and regarding bioremediation potential, strain SEY, an Anoxybacillus sp., was the most promising. This isolate had improved vanadium(V) and iron(III) reduction rates of over 50% in co-cultivation symbiosis tests with strains CRL and FEY, respectively.
Thesis (Masters)
Master of Science (MSc)
School of Environment and Sc
Science, Environment, Engineering and Technology
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Aldosary, Huda A. KH. "Polycyclic Aromatic Hydrocarbon Degradation by Anaerobic Bacteria from the Great Artesian Basin". Thesis, Griffith University, 2020. http://hdl.handle.net/10072/393639.

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The Great Artesian Basin (GAB) is a vast subterranean thermal aquifer system underlying over 20% of the Australian continent. Substantial reserves of oil, gas and minerals exist within the GAB and combined with industrial activities can often contaminate the groundwaters. The current study investigated the bacterial ecology of bore waters that were in or close to oil deposits. Three sites were selected, two in the Quilpie/Eromanga region of Queensland (Naretha bore registered number 4022 and Adavale bore registered number 305), and the other in the Moomba oil field of South Australia (Moomba bore 9). A wide diversity of bacteria was detected across all of the samples collectively, including members of 32 bacterial phyla. There was greater diversity in the water samples from bores 4022 and 305 compared with Moomba 9, which was likely due to its closer association with oil. The most dominant bacterial taxa were similar in bores 4022 and 305, families Rhodobacteraceae, and Xanthomonadaceae and the order Bacillales. In contrast, the dominant taxa from Moomba 9 were the family Oxalobacteriaceae and the genus Agrococcus. Three different water samples were tested from bore 4022, from the source, 100 m and 250 m downstream in the runoff channel water. The bacterial diversity increased the further away the water flowed from the bore, due to the cooler water and contamination from the surrounding environment. A comprehensive anaerobic thermophilic enrichment program revealed that bacteria grew on a wide variety of organic substrates and a range of heavy metals as terminal electron acceptors. Isolation yielded 164 bacteria capable of using substrates from sugars and extracts through to polycyclic aromatic hydrocarbons (PAH) and reducing the metals iron(III), vanadium(V), cobalt(III) and manganese(IV). Seven pure iron(III) reducing polycyclic aromatic hydrocarbon (PAH) degrading bacteria, designated strains RN40AT, RN40BT, RN40CT, RN40DT, RN305AT, RN305BT and MBA9BT, were selected for further studies. The rates of degradation Polycyclic Aromatic Hydrocarbon Degradation by Anaerobic Bacteria from the Great Artesian Basin and PAH preference varied significantly between the isolates. Strain MBA9BT showed the highest extent (97.6%) of anthracene degradation while strain RN305BT was the lowest (9.7%). Again, strain MBA9BT also showed the highest extent (91.2%) of pyrene degradation and strain RN40DT showed the lowest (16.1%). Phenanthrene degradation was highest in strain RN40BT and the lowest in strain MBA9BT (2%). PAH degradation in all the isolates showed a direct dependence on Fe(III) reduction. A measurable decrease in the surface tension of the medium suggested the production of biosurfactants by all isolates when grown with PAHs as substrates. Genomic analysis of the isolates revealed subsystems of different pathways that are commonly found in metal acquisition, transport and utilisation as well as those for aromatic hydrocarbon degradation. Strain RN40DT had the highest number of genes involved in the metabolism of PAHs, though all of the isolates had genes for the metabolism of central aromatic intermediates, especially those related to catechol, salicylate and homogentisate degradation. The isolates had varying levels of genes involved in the metabolism and resistance to iron, copper, chromium, zinc, molybdenum, manganese and mercury. Strains RN40AT, RN305AT RN305BT, RN40BT and RN40DT contained the most genes for iron acquisition and metabolism including those for siderophores, hemin transporters and ferric ABC transport systems. The results in the current study have built upon our understanding of bacterial diversity in the GAB, particularly with insights into waters associated with oil deposits. Bacteria that degrade polycyclic aromatic hydrocarbons with the simultaneous reduction of Fe(III) under anaerobic conditions were isolated for the first time and may have significant potential in bioremediation of contaminated groundwaters.
Thesis (PhD Doctorate)
Doctor of Philosophy (PhD)
School of Environment and Sc
Science, Environment, Engineering and Technology
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Spanevello, Mark. "The Phylogeny of Prokaryotes Associated with Australia's Great Basin". Thesis, Griffith University, 2001. http://hdl.handle.net/10072/367766.

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The Great Artesian Basin of Australia is the largest freshwater artesian basin in the world. It underlies arid and semi-arid regions of Queensland, New south Wales, South Australia and the Northern territory, approximately 20% of the Australian continent. Temperatures of its' waters range from 30°C to over 100°C and over 5000 bores access its waters and empty into open drainage systems for agricultural irrigation and stock watering purposes. The Great Artesian Basin of Australia has great economic and agricultural importance, but prokaryotic communities persisting in the bore waters influence its' quality. To gain an understanding of these prokaryotic communities, a culture-independent study was conducted on microbial communities present in the outflow of the New Lorne bore (registered bore number 17263). Five distinct prokaryotic communities existing at different temperatures (88°C, 75°C, 66°C, 57°C, and 52°C) were selected and total genomic DNA was extracted. PCR-amplified 16S rRNA genes were subsequently cloned and a total of 64 clones from the 88°C community and 96 clones from the other communities were examined. Partial sequences identified phylotypes that were then fully sequenced and analysed phylogenetically. The analysis revealed identical phylotypes existing in adjacent communities, as well as an increase in the phylogenetic diversity as water temperature decreased. Sequences identified belonged to species spanning the full diversity of the Bacterial domain, including Hydrogenobacter, Thermus, Meiothermus, Chloroflexus, Cytophaga, Planctomycetes, Rhodothermus, Bacillus, Clostridium, Nitrospira, Verrucomicrobium, Acidobacterium, α-, β-, γ-, and δ-Proteobacteria. Clones recovered also grouped with taxa with no isolated representatives. Of the libraries, 24 phylotypes from 6 phyla had a similarity of 96% or more to cultured isolates and comprised 73% of all clones analysed. 34 phylotypes from 11 phyla had less than 96% similarity to cultured isolates, or were related to previously cloned 16S rRNA gene sequences, and comprised 27% of the clones analysed. This shows the prokaryotic ecology of the Great Artesian Basin environment includes a diverse range of many uncultured, novel species. Previous studies on isolates of Thermus and Meiothermus have revealed a relationship between the taxonomic groups and the geographical sites of isolation. A survey of 14 Thermus and 2 Meiothermus isolates and 16S rRNA gene clone data from the New Lorne bore extends the geographical diversity of these two genera. Thermus was isolated from all four mat samples and were most dominant in the red mat at 66°C. Meiothermus was only isolated from the red mat at 66°C. 16S rRNA gene sequence analysis revealed that 13 of the 14 Thermus isolates were closely related to T. igniterrae (100% similarity) and one isolate was closely related to Thermus strain SRI-96 (99.1% similarity). Both Meiothermus had 100% similarity with Meiothermus ruber. The 16S rRNA gene study of the environment showed that Thermus dominated the grey mat (75°C) followed by the red mat (66°C) and green mat (57°C), but was absent from the brown mat (52°C). Four Thermus phylotypes were identified with T. scotoductus the most dominant, followed by T. igniterrae, Thermus strain SRI-248, and T. oshimai. T. scotoductus dominated over T. igniterrae in the grey mat library, and, only marginally, in the red mat. Phylotypes belonging to the genus Meiothermus were identified in the red, green and brown mats, but not in the grey coloured mats with 2 distinct phylotypes related to M. ruber and M. cerberus. The M. ruber phylotype was dominant in the red mat and the M. cerberus phylotype was dominant in the brown mat with M. ruber only slightly dominant over M. cerberus in the green mat. Based on 16S rRNA gene sequence analysis, isolates and clones were most similar to those obtained from hot springs in Iceland, perhaps demonstrating a ecological similarity between the Great Artesian Basin of Australia and Iceland's thermal environments. Similarity of biodiversity was low between Thermus and Meiothermus species identified from the Great Artesian Basin and other well-studied thermal environments such as Yellowstone National Park, USA and New Zealand. From enrichment studies, a strictly aerobic, thermophilic, Gram-positive, spore-producing rod-shaped bacterium (2 - 10μm x 0.3μm), designated isolate C21T (T = type strain) was isolated from a sediment sample collected from the run-off channel of the New Lorne bore accessing the Great Artesian Basin of Australia. Isolate C21T grew optimally at 70°C (temperature range for growth between of 55°C and 80°C) and a pH of 8.5 (pH growth range between 6 and 10.5) with a generation time of 90 minutes. The isolate is strictly heterotrophic and grew on yeast extract and/or tryptone as sole carbon and energy source(s). The growth of isolate C21T was not improved with the addition of a variety of carbohydrates (sucrose, cellobiose, glucose, dextrin, amylopectin, chitin, xylan, carboxymethylcellulose, inositol, arabinose, mannose, fructose, gelatin, starch, amylose, galactose, dextrose, xylose, maltose, L-sorbose, and raffinose), organic acids (lactic acid, pyruvic acid, and benzoic acid), or casamino acids without either yeast extract or tryptone. The G+C content of the chromosomal DNA of isolate C21T was 71mol%. A phylogenetic analysis of the 16S rRNA gene of isolate C21T indicated that it was a member of the phylum Firmicutes clustering with Thermaerobacter marianensis (similarity of 98%). However, isolate C21T differed from T. marianensis in a number of key physiological and phenotypic properties and based on the evidence isolate C21T is designated Thermaerobacter subterranea sp. nov. (type strain C21T = ATCC BAA-137). To further understand the prokaryotic ecology of the Great Artesian Basin, the development of real-time PCR to detect and quantify environmental isolates of Caloramator was undertaken. Thermophilic isolates from the genus Caloramator within the phylum Firmicutes are readily isolated from drainage systems of the Great Artesian Basin of Australia. Adjacent hybridisation probes were designed to identify Caloramator strains. The real-time PCR was optimised by manipulating the PCR and the concentrations of the adjacent hybridisation probes. Real-time PCR enabled the detection of as little as 6fg of DNA in the 45 PCR cycles. The development of real-time PCR will provide the foundation of applying this technique to identify and monitor other, perhaps detrimental, members of prokaryotic communities in the environment. The information provided by the examination of these communities has improved our understanding of the culturable and non-culturable members of the prokaryotic communities of the Great Artesian Basin of Australia and provides the basis for further ecological studies of the Great Artesian Basin.
Thesis (PhD Doctorate)
Doctor of Philosophy (PhD)
School of Biomolecular and Biomedical Sciences
Science, Environment, Engineering and Technology
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Braz, Carmen. "Modelling the role of dynamic topography and eustasy in the evolution of the Great Artesian Basin". Thesis, The University of Sydney, 2022. https://hdl.handle.net/2123/29730.

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Widespread flooding of the Australian continent during the Early Cretaceous, referred to as the Eromanga Sea, deposited extensive shallow marine sediments throughout the Great Artesian Basin. This event had been considered ‘out of sync’ with eustatic sea level and was instead solely attributed to dynamic subsidence associated with Australia’s passage over eastern Gondwanan subducted material. However, mantle convection models previously used to explain this event have since been shown to overestimate dynamic topography amplitude by a factor of two compared to residual topography estimates. Previous models were also based on a Cretaceous eustatic sea level peak at ~90 Ma in conventional eustatic sea level curves; however, more recent estimates of global sea level from Ocean Basin Volume (OBV) suggest this peak may have occurred earlier at ~120 Ma. Our work links time-dependent erosion and deposition with dynamic topography and eustasy to test their contribution to basin development using the landscape evolution code pyBadlands. Our results show that the lower amplitude estimates of dynamic topography derived from pseudo-compressible mantle flow models better reflect the Cretaceous vertical motions of the Australian continent (~100 m) compared to their incompressible counterparts (~200-400 m). Additionally, our models include the Neogene north-eastward tilting of Australia, elusive in most previously-published geodynamic models. In conjunction with an OBV-derived sea level curve, our preferred landscape evolution model broadly matches the Cretaceous inundation patterns and first-order sedimentary sequences in the Great Artesian Basin. The results highlight that the Early Cretaceous inundation of the Australian continent is likely a combination of high global sea levels and the regional effects of dynamic subsidence. Our work provides a framework for a new generation of evolving paleogeographic models at continental scales, while also providing key insights into the viability of existing sea level curves and dynamic topography estimates for reproducing topographic and basin evolution.
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Jiang, Zhenjiao. "Analysis and modelling of the hydraulic conductivity in aquitards : application to the Galilee Basin and the Great Artesian Basin, Australia". Thesis, Queensland University of Technology, 2014. https://eprints.qut.edu.au/73181/1/Zhenjiao_Jiang_Thesis.pdf.

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In large sedimentary basins with layers of different rocks, the groundwater flow between aquifers depends on the hydraulic conductivity (K) of the separating low-permeable rocks, or aquitards. Three methods were developed to evaluate K in aquitards for areas with limited field data: • Coherence and harmonic analysis: estimates the regional-scale K based on water-level fluctuations in adjacent aquifers. • Cokriging and Bayes' rule: infers K from downhole geophysical logs. • Fluvial process model: reproduces the lithology architecture of sediment formations which can be converted to K. These proposed methods enable good estimates of K and better planning of further drillholes.
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Welsh, Wendy Denise, i wendywelsh@yahoo com au. "Groundwater balance modelling with Darcy's Law". The Australian National University. Faculty of Science, 2007. http://thesis.anu.edu.au./public/adt-ANU20070703.165654.

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The sustainability of groundwater resources is important for the environment, the economy and communities where surface water is scarce. It is a hidden resource, but additional information can be extracted by combining groundwater measurements and lithological information with groundwater flow equations in groundwater models. The models convert data and knowledge about the groundwater systems into information, such as relative inflow and outflow rates and water-level predictions that can be readily understood by groundwater managers. ¶ The development of models to effectively inform groundwater management policies is, however, a complex task that presents a fundamental scientific challenge. This thesis presents methods and results for water balances calculated using groundwater flow models. Groundwater flow modelling methods and approaches are discussed, and their capabilities and limitations are reviewed. Two groundwater systems are studied for the Great Artesian Basin (GAB) and for the irrigation area near Bowen, Queensland. Three approaches to water balance modelling are applied in comprehensive model-development frameworks that take into account model objectives, data and knowledge availability and sensitivity analysis techniques. The three models show numerical methods of increasing complexity. The Bowen study area is well-suited to the least-complex method because data collection has been a priority there. As a contrast, the GAB is a large, poorly-monitored basin for which more knowledge of the groundwater system can be gained from its simulation by the steady state and transient groundwater flow models. The Bowen impact assessment model calculates dynamic historical water balances. The GAB aquifer models are high-complexity representations of the groundwater system that include predicted responses of the system to changes in hydrological conditions. These are comprehensive and well-documented attempts to model these systems. They provide a platform for scenario investigation and future improvements. ¶ Darcy’s Law was used in a GIS (Geographic Information System) to calculate dynamic water balances for an aquifer near the Queensland town of Bowen. This is the first time this approach has been applied to generate a complete groundwater balance. Over the period 1989-1997 the model estimates average total inflows to be 87 % groundwater recharge by rainfall and irrigation return flow, 12 % river recharge and 1 % inflow across the study area boundary. Outflows are estimated to be 66 % evapotranspiration, 28 % water bore discharge, 4 % discharge to the ocean and 2 % groundwater loss to rivers. Analyses show that evapotranspiration is the most uncertain parameter value. The GIS method was found to be useful for calculating water balances more accurately than analytical methods, because of their simplifying assumptions, and less time consuming than the more complex numerical models developed for the GAB aquifer. ¶ For the GAB, a steady state numerical model was developed and tested and predictive scenarios were run. The purpose of this modelling was both to gain a better understanding of the water balance of the GAB and to provide a tool that could predict water level recoveries under different bore rehabilitation scenarios. The model complexity is greater than in any previous numerical groundwater model of the GAB. In particular, the model uses more data, extends over a larger area and uses a generally finer discretisation than previous models. For the nearest surface artesian aquifer in 1960 the model estimates total inflows to be 60 % groundwater recharge and 40 % diffuse vertical inter-aquifer leakage. The model estimates outflows to be 53 % diffuse vertical leakage, 43 % water bore discharge, 3 % spring discharge and 1 % discharge to the ocean. Analyses show that the model is most sensitive to changes in horizontal hydraulic conductivity and recharge. The model-predicted heads match field measurements with a Scaled RMS error of 0.8 %, which is well within the guideline error of 5 %. The predictive scenarios show net vertical leakage into the aquifer decreasing and net vertical leakage out of the aquifer increasing, as bore flows are reduced. These estimates of inflows and outflows complement other studies of the Basin and add to our understanding of its hydrodynamics. In this way the water balance helps provide a sound basis for the development of GAB groundwater management plans and policies. Through its water level recovery predictions, the model has also been used to support the GAB Sustainability Initiative. ¶ A transient numerical model of the GAB was also developed and tested, and predictive scenarios were run. This model builds on the steady state model, and is more complex, with a calibration period (1965-1999) that is longer than in any previous GAB model. During calibration the model observations were expressed and weighted so that the minimisation of the objective function reflected the relative importance of the model’s potential uses, these being respectively: to simulate the impact of changing bore flows, to more generally inform water management plans and to provide an estimate of the water balance. It was found that the 1960 steady state assumption was not correct. Discluding anthropogenic discharge, the model is most sensitive to recharge and hydraulic conductivity. The model-predicted heads match field measurements with a Scaled RMS error of 2.7 %, which is well within the guideline error of 5 %, but the increased data requirements of the transient model highlighted deficiencies in the data available for the modelling. In particular, the uneven spread of the groundwater measurements over both time and space, the questionable accuracy of measurements from both high temperature and pressure bores, and corroded bores, and the type of discharge measured (for example, maximum yield or flow-as-found), became evident during the calibration of the model. Insights and the value of this work indicates for the first time that at the start of 2005 outflows were estimated to exceed inflows by 266 GL/year, or 62 % of total inflows, and, assuming that inflows through the aquifer’s boundary will not be reduced due to climate change, it will be possible to recover some of the lost groundwater pressure if all stock and domestic bores are rehabilitated and new extractions are limited. In this case the modelling estimates that inflows could exceed outflows by up to 40 % of total outflows.
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Moya, Claudio Enrique. "Hydrostratigraphic and hydrochemical characterisation of aquifers, aquitards and coal seams in the Galilee and Eromanga basins, Central Queensland, Australia". Thesis, Queensland University of Technology, 2015. https://eprints.qut.edu.au/84153/14/84153%20Claudio%20Moya%20Thesis.pdf.

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Inter-aquifer mixing studies are usually made carrying out hydrochemical and isotopic techniques only. In this thesis these techniques have been integrated with three-dimensional geological modelling proving to be a better approach for inter—aquifer mixing assessment in regional areas, and also highlighting the influence of faulting in the understanding of groundwater and gas migration, which could not be possible using the two fist techniques alone. The results are of particular interest for coal seam gas basins and can even be used as exploration tools as areas of higher permeability and gas migration were identified.
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Ogg, Christopher David. "Thermophiles from Deep Subsurface Waters". Thesis, Griffith University, 2011. http://hdl.handle.net/10072/366568.

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Thermophiles dominate deep subsurface aquifers and represent the most ancient life on the planet. In this project, the culturable diversity of thermophiles that inhabit the world’s largest freshwater geothermal aquifer, Australia’s Great Artesian Basin (GAB), were explored using culture-dependent techniques. These studies largely focused on four unique microbial mat communities that exist in the runoff channel of the New Lorne Bore (registered number 17263) at temperatures between 52 – 72 °C and mostly targeted the cultivation of iron(III)- reducing bacteria due to their considerable influence on subsurface processes and likely involvement in the corrosion of GAB bores and pipelines. During this project a number of novel and modified screening methods were developed including high-throughput microenrichments of thermophiles using Biolog (Biolog Inc., U.S.A.) and U-bottom deep-well (1 ml) microtiter plates (Sarstedt, Germany) amended with seldom tested energy substrates and varied terminal electron acceptors (TEA) such as iron(III), sulphate, vanadium(V) and molybdenum(VI). Phylogenetic analyses of the isolates recovered in this project detected more than 15 novel phylotypes thereby extending the known culturable diversity of the GAB microflora. Complete phenotypic characterisations were performed on 9 GAB thermoanaerobic isolates, which resulted in the descriptions of 8 novel organisms including 4 novel genera: Thermotalea metallivorans (Ogg & Patel, 2009b), Fervidicola ferrireducens (Ogg & Patel, 2009c), Sporolituus thermophilus (Ogg & Patel, 2009d) and Fervidicella metallireducens (Ogg & Patel, 2010); and 4 novel species: Caloramator australicus (Ogg & Patel, 2009a), Caloramator mitchellensis (Ogg & Patel, 2011a), Thermovenabulum gondwanense (Ogg et al., 2010), and Desulfotomaculum varum (Ogg & Patel, 2011c); and amendments to the genus Caloramator (Ogg & Patel, 2011a) [given in Appendices 1 – 8]. Included in these characterisation studies was a modified method for determining an organisms mol % of G + C content of DNA using TempliPhi (Amersham Biosciences, U.K.) genome amplification kits to prepare the high molecular weight (HMW) genomic DNA prior to thermal denaturation. When the phenotypic data resulting from the strain characterisations was combined with the enrichment results, a complex model of the microbial oxidation of organic matter in the GAB at elevated temperatures (50 – 70 °C) was constructed.
Thesis (PhD Doctorate)
Doctor of Philosophy (PhD)
School of Biomolecular and Physical Sciences
Science, Environment, Engineering and Technology
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Książki na temat "Great Artesian Basin"

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Booth, Carol. Water down under: Understanding and managing Australia's Great Artesian Basin. [Australia]: Great Artesian Basin Coordinating Committee (GABCC), 2011.

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Części książek na temat "Great Artesian Basin"

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Ponder, W. F. "Mound Springs of the Great Artesian Basin". W 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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Murray, Tim. "Towards an Archaeology of Extensive Pastoralism in the Great Artesian Basin in Australia". W Historical Archaeology and Environment, 109–27. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-90857-1_6.

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Ogg, Christopher D., Mark D. Spanevello i Bharat K. C. Patel. "Exploring the Ecology of Thermophiles from Australia’s Great Artesian Basin During the Genomic Era". W Thermophilic Microbes in Environmental and Industrial Biotechnology, 61–97. Dordrecht: Springer Netherlands, 2013. http://dx.doi.org/10.1007/978-94-007-5899-5_2.

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Cosens, Barbara, i Angela H. Arthington. "Assessing Adaptive Water Governance for Lake Eyre Basin and Linked Portions of the Great Artesian Basin in Australia". W Practical Panarchy for Adaptive Water Governance, 131–47. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-72472-0_9.

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Ordens, Carlos Miraldo, Neil McIntyre, Jim Undershultz i Phil Hayes. "A Comprehensive, Up-To-Date Evidence Base to Inform Public, Planning and Policy for Australia’s Great Artesian Basin". W Advances in Geoethics and Groundwater Management : Theory and Practice for a Sustainable Development, 405–8. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-59320-9_85.

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Gasparon, Massimo, i Kenneth D. Collerson. "Trace elements and Sr isotopic composition of waters from the Great Artesian Basin of Australia: Implications for the formation of ore deposits and hydrocarbon resources". W Organic Matter and Mineralisation: Thermal Alteration, Hydrocarbon Generation and Role in Metallogenesis, 53–65. Dordrecht: Springer Netherlands, 2000. http://dx.doi.org/10.1007/978-94-015-9474-5_4.

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Habermehl, Rien A. "Groundwater governance in the Great Artesian Basin, Australia". W Advances in Groundwater Governance, 411–41. CRC Press, 2017. http://dx.doi.org/10.1201/9781315210025-21.

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Alley, William M., i Rosemarie Alley. "Not All Aquifers Are Created Equal". W High and Dry. Yale University Press, 2017. http://dx.doi.org/10.12987/yale/9780300220384.003.0005.

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This chapter examines how geology and climate create vastly different groundwater situations. Effective management of groundwater depends upon full consideration of these differences. The chapter begins with a distinction between confined and unconfined aquifers and a look at artesian wells, with a focus on Australia’s Great Artesian Basin. The characteristics of different rock types are illustrated by four basic aquifer rock types in sub-Saharan Africa. The chapter then turns to non-renewable aquifers in North Africa and Saudi Arabia. The fast-recharging Edwards Aquifer in Texas then provides a quite different story with its sensitivity to short-term climate variability and concerns about endangered species. The chapter concludes with a discussion of saltwater intrusion in coastal aquifers and the potential of brackish groundwater for water supply.
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Pandey, Sanjeev, Randall Cox i Steven Flook. "Cumulative Groundwater Impact Assessment and Management – An Example in Practice". W Groundwater [Working Title]. IntechOpen, 2021. http://dx.doi.org/10.5772/intechopen.95278.

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Production of coal seam gas (CSG), or coal bed methane, requires large-scale depressurisation of a target formation by extracting groundwater, which, in turn, has the potential to affect overlying and underlying aquifers. This leads to wide-ranging stakeholder concerns around the impacts on groundwater assets such as water supply bores, groundwater-dependent ecosystems and connected watercourses. Around 2010, the CSG industry in Queensland, Australia grew rapidly with the expansion of operations in the Surat and Bowen basins by multiple operators. This particularly raised concerns about the cumulative effects, because the target coal seams are part of the Great Artesian Basin – one of the world’s largest aquifers. To respond to this challenge, an innovative framework was developed to provide for an independent cumulative impact assessment and to set up arrangements for managing those impacts. This chapter describes the main thrust of that framework.
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"Verification of 4He and 36Cl dating of very old groundwater in the Great Artesian Basin, Australia". W Groundwater Response to Changing Climate, 109–22. CRC Press, 2010. http://dx.doi.org/10.1201/b10530-12.

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Streszczenia konferencji na temat "Great Artesian Basin"

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"Field estimates of groundwater discharge – Great Artesian Basin, South Australia". W 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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Underschultz*, Jim, i Sue Vink. "Emerging Complexity of the Great Artesian Basin Aquifer Systems in the Surat". W International Conference and Exhibition, Melbourne, Australia 13-16 September 2015. Society of Exploration Geophysicists and American Association of Petroleum Geologists, 2015. http://dx.doi.org/10.1190/ice2015-2205979.

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"Defining ecosystem processes of the Australian Great Artesian Basin springs from multi-sensor synergies". W 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.h15.white.

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White, Davina, i Megan Lewis. "Mapping the surface expression and vegetation communities of Australian Great Artesian Basin springs using hyperspectral analyses". W IGARSS 2013 - 2013 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2013. http://dx.doi.org/10.1109/igarss.2013.6721141.

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Pearce, Julie. "CO2 geological storage in the Surat Basin". W PESA Symposium Qld 2022. PESA, 2022. http://dx.doi.org/10.36404/depi2461.

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Carbon dioxide (CO2) storage is a vital part of the energy transition to low emissions. The Jurassic age Precipice Sandstone of the Surat Basin in Queensland, Australia, has been investigated as a suitable reservoir for CO2 storage. The overlying Evergreen Formation is a thick, interbedded mudstone and sandstone seal, and regarded a regional aquitard. Wells have been drilled for feasibility studies, initially in CTSCo’s Glenhaven region, near Wandoan, and recently in the southern Surat Basin near the town of Moonie. Since the Precipice Sandstone is also a Great Artesian Basin aquifer, the southern region with deeper groundwater unsuitable for stock use, and minimal to stagnant flow, is likely a more suitable site. The University of Queensland has undertaken research in both potential storage regions, and more broadly across the basin, including the separate Moonie oil field. This presentation will focus on core characterisation, experimental and modelled geochemical CO2-water-rock reactions and their impacts on water quality, porosity and permeability, and the effects of gas stream impurities SOx, NOx and O2. In addition, it may touch on field studies to assess existing hydrochemistry, water quality and native greenhouse gases in the Precipice Sandstone, and in the Hutton Sandstone that overlies the Evergreen Formation.
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Suckow, Axel, Matthias Raiber, Alec Deslandes, Christoph Gerber, Jorge Martinez, Guo-Min Yang, Wei Jiang i Karina Meredith. "Quantifying recharge to the Pilliga Sandstone aquifer, Great Artesian Basin Australia: learnings from combining 14C, 36Cl and 81Kr." W Goldschmidt2022. France: European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.10724.

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Raporty organizacyjne na temat "Great Artesian Basin"

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Knight, B., B. Mather, L. Moresi, N. Symington, N. Rollet, J. Vizy, T. Ransley, L. Wallace i B. Sundaram. Bayesian inferences on groundwater flow within the Great Artesian Basin. Geoscience Australia, 2022. http://dx.doi.org/10.11636/record.2022.030.

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Vizy, John, i Nadege Rollet. Great Artesian Basin geological and hydrogeological surfaces update: report and data package. Geoscience Australia, 2022. http://dx.doi.org/10.11636/record.2022.019.

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Wallace, L., i T. Ransley, red. Assessing the status of groundwater in the Great Artesian Basin – Summary report. Geoscience Australia, 2022. http://dx.doi.org/10.11636/record.2022.046.

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McPherson, A., N. Rollet, J. Vizy i P. Kilgour. Great Artesian Basin eastern recharge area assessment - northern Surat Basin airborne electromagnetic survey interpretation report. Geoscience Australia, 2022. http://dx.doi.org/10.11636/record.2022.017.

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Tan, K. P., N. Rollet, J. Vizy i P. Kilgour. Great Artesian Basin eastern recharge area assessment – Eastern Eromanga Basin airborne electromagnetic data interpretation report. Geoscience Australia, 2022. http://dx.doi.org/10.11636/record.2022.033.

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Norton, C. J., i N. Rollet. Regional stratigraphic correlation transects across the Great Artesian Basin: Eromanga and Surat basins focus study. Geoscience Australia, 2022. http://dx.doi.org/10.11636/record.2022.002.

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McCubbine, J. C., Z. Du, C. Ojha, M. C. Garthwaite i N. J. Brown. InSAR processing over the Great Artesian Basin and analysis over the western Eromanga Basin and northern Surat Basin. Geoscience Australia, 2022. http://dx.doi.org/10.11636/record.2022.029.

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Ransley, T. R., E. E. Slatter, P. Kilgour, B. M. Radke, A. McPherson, J. Lester, E. Lai, J. Vizy i P. Dixon-Jain. Water Balance for the Great Artesian Basin: Summary of data, methods and results. Geoscience Australia, 2022. http://dx.doi.org/10.11636/record.2022.047.

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McPherson, A., N. Rollet, J. Vizy, T. Ransley, P. Kilgour, E. Slatter, N. Symington, J. Wilford i L. Wallace. Improving hydrogeological conceptualisations of the Great Artesian Basin: Northern Surat Basin pilot study – methods and preliminary results. Geoscience Australia, 2022. http://dx.doi.org/10.11636/record.2022.006.

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Lai, E. C. S., B. Sundaram, R. Evans, T. R. Ransley i T. J. Evans. Summary of the Great Artesian Basin Research Priorities Workshop: 27-28 April 2016, Canberra. Geoscience Australia, 2016. http://dx.doi.org/10.11636/record.2016.023.

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