Готові списки джерел за темами / Newcastle and Northern New South Wales

Добірка наукової літератури з теми "Newcastle and Northern New South Wales"

Автор: Grafiati
Опубліковано: 10 грудня 2022
Оновлено: 28 січня 2023

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Статті в журналах з теми "Newcastle and Northern New South Wales"

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Gardner, M. G., and R. D. Ward. "Population structure of the Australian gummy shark (Mustelus antarcticus GÜnther) inferred from allozymes, mitochondrial DNA and vertebrae counts." Marine and Freshwater Research 49, no. 7 (1998): 733. http://dx.doi.org/10.1071/mf98009.

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The gummy shark (Mustelus antarcticus) is the main target of southern Australian shark fisheries. Its stock structure was investigated through allozymes (up to 28 loci), mitochondrial DNA (up to 10 restriction enzymes) and vertebrae counts. The average heterozygosity per allozyme locus (0.099) and degree of polymorphism (0.255) was high for sharks. Composite mitochondrial DNA haplotype diversity (0.534) and mean nucleotide sequence diversity (0.16%) were also moderately high. Three of the seven polymorphic allozyme loci (CK-A*, LDH-1*, PEP*) and the mtDNA haplotypes showed significant spatial differentiation. Two genetic stocks were identified: one along the southern coast of Australia from Bunbury in Western Australia to Eden in New South Wales and one off northern New South Wales (in the region of Newcastle to Clarence River). There was some evidence for a third stock off Townsville, Queensland. The northern occurrences extend the known geographical range of this species. Vertebrae counts from Eden northwards increased, supporting the conclusion of population heterogeneity off eastern Australia.
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2

Adams, Peter. "A review of Dendrobium kingianum Bidwill ex Lindl. (Orchidaceae) with morphological and molecularphylogenetic analyses." Telopea 24 (May 19, 2021): 203–32. http://dx.doi.org/10.7751/telopea14806.

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Populations of Dendrobium kingianum Bidwill ex Lindl. from near Newcastle, New South Wales to southern and central west Queensland and encompassing all regions of the distribution were studied using field observations, morphometric analysis and nrITS sequences. A total of 281 individuals were used to construct regional descriptions of D. kingianum and 139 individuals were measured for 19 morphological characters, and similarities and differences among specimens summarised using multivariate statistical methods. Patterns of morphological variation within D. kingianum are consistent with a single variable species that expresses clinal variation, with short-growing plants in the south and taller plants in the northern part of the distribution. The nrITS gene tree suggests two subgroups within D. kingianum subsp. kingianum, one comprising northern, the other southern individuals, which may overlap in the vicinity of Dorrigo, New South Wales. The disjunct D. kingianum subsp. carnarvonense Peter B. Adams in central west Queensland, which can be distinguished by a predominately subterranean habit and a narrower labellum midlobe, was resolved sister to D. moorei F.Muell., which renders D. kingianum paraphyletic in the nrITS gene tree, but this position was not supported. Regional descriptions documenting clinal variation are provided. All previously described varieties, including D. kingianum var. pulcherrimum Rupp, are colour and growth forms of D. kingianum subsp. kingianum.
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3

MELCHERS, R. E., and A. W. PAGE. "THE NEWCASTLE (NEW SOUTH WALES) EARTHQUAKE." Proceedings of the Institution of Civil Engineers - Structures and Buildings 94, no. 2 (May 1992): 143–56. http://dx.doi.org/10.1680/istbu.1992.18783.

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4

Fryer, J. G. "THE NEWCASTLE, NEW SOUTH WALES EARTHQUAKE." Photogrammetric Record 13, no. 76 (August 26, 2006): 609–10. http://dx.doi.org/10.1111/j.1477-9730.1990.tb00721.x.

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5

Hartig, Kate V., and Kevin M. Dunn. "Roadside Memorials: Interpreting New Deathscapes in Newcastle, New South Wales." Australian Geographical Studies 36, no. 1 (March 1998): 5–20. http://dx.doi.org/10.1111/1467-8470.00036.

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6

English, Helen Jane, Sarah Monk, and Jane W. Davidson. "Music and world-building in Newcastle, New South Wales, Australia." International Journal of Community Music 11, no. 3 (December 1, 2018): 245–64. http://dx.doi.org/10.1386/ijcm.11.3.245_1.

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7

Christie, David, Lyndall Spencer, and Ambikaipakan Senthilselvan. "Air quality and respiratory disease in Newcastle, New South Wales." Medical Journal of Australia 156, no. 12 (June 1992): 841–44. http://dx.doi.org/10.5694/j.1326-5377.1992.tb136996.x.

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8

Hanapi, Nur Amalina, and Khairul Asyraf Mohd Rodzi. "LIGHTING DESIGN FRAMEWORK; RECOMMENDATION STUDY FOR NEWCASTLE MOSQUE, NEW SOUTH WALES." Journal of Islamic Architecture 7, no. 1 (June 28, 2022): 111–19. http://dx.doi.org/10.18860/jia.v7i1.13093.

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This research explores the analysis method of the current situation and injects direct design proposal analysis to the mosque from the existing condition. The exploration of lighting fundamentally and significantly impacts holistic and ritual performance in any religious building. However, regarding the conversion of typology to the mosque, there were a few research that focus on the existing condition in lighting design performance for Newcastle Mosque. Therefore, this study explores approximately four designs of three-dimensional recommendations as a methodology which include passive and active design implications used recorded as part of the discussion. The result shows that the proposed design helped in repairing the conditions of the mosque through the implementation of the skylight, curtain, designated window, and sunbreak for the best rectification recommendation. Furthermore, the result of the study suggests such minimum glare and effective lighting distribution contribute to the amount reduction of energy consumption, improve the quality of reading, and properly enlighten the religious congregational activities and other exercises carried out to optimum brightness of the mosque.
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9

Monfries, Melissa M., and Norman F. Kafer. "Department of Education, The University of Newcastle, New South Wales, Australia 2308." Journal of Psychology 128, no. 4 (July 1994): 447–54. http://dx.doi.org/10.1080/00223980.1994.9712751.

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10

Oxley, Les. "INTERNATIONAL CONGRESS ON MODELLING AND SIMULATION, NEWCASTLE, NEW SOUTH WALES, AUSTRALIA 1995." Journal of Economic Surveys 10, no. 2 (June 1996): 225–31. http://dx.doi.org/10.1111/j.1467-6419.1996.tb00011.x.

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Дисертації з теми "Newcastle and Northern New South Wales"

1

Samuel, Jos Martinus. "Effects of multi-scale rainfall variability on flood frequency : a comparative study of catchments in Perth, Newcastle and Darwin, Australia." University of Western Australia. School of Environmental Systems Engineering, 2008. http://theses.library.uwa.edu.au/adt-WU2009.0066.

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Issues arising from climate change and long-term natural climate variability have become the focus of much recent research. In this study, we specifically explore the impacts of long-term climate variability and climate changes upon flood frequencies. The analyses of the flood frequencies are carried out in a comparative manner in catchments located in semiarid-temperate and tropical landscapes in Australia, namely Perth, Newcastle and Darwin, using a process-based derived flood frequency approach. The derived flood frequency analyses are carried out using deterministic rainfall-runoff models that capture the intrinsic water balance variability in the study catchments, and driven by temporal rainfall event sequences that are generated by a stochastic rainfall model that incorporates temporal variabilities over a multiplicity of time scales, ranging from within-event, between-event to seasonal, multi-annual and multi-decadal time scales. Six climate scenarios are considered for Newcastle, that combine the ENSO (El Niño Southern Oscillation) and IPO (Inter-decadal Pacific Oscillation) modes of variability, and six different climate scenarios are considered for Perth and Darwin that combine these different ENSO modes and step changes in climate (upwards or downwards) that occurred in 1970 in both regions, which were identified through statistical analysis. The results of the analyses showed that La Niña years cause higher annual maximum floods compared to El Niño and Neutral years in all three catchments. The impact of ENSO on annual maximum floods in the Newcastle catchment is enhanced when the IPO is negative and for Perth, the impact of ENSO weakens in the post-1970 period, while it strengthens in Darwin in the same period. In addition, the results of sensitivity and scenario analyses with the derived flood frequency model explored the change of dominant runoff generation processes contributing to floods in each of the study catchments. These analyses highlighted a switch from subsurface stormflow to saturation excess runoff with a change of return period, which was much more pronounced in Perth and Darwin, and not so in Newcastle. In Perth and Darwin this switch was caused by the interactions between the out-of-phase seasonal variabilities of rainfall and potential evaporation, whereas the seasonality was much weaker in Newcastle. On the other hand, the combination of higher rainfall intensities and shallower soil depths led to saturation excess runoff being the dominant mechanism in Newcastle across the full range of return periods. Consequently, within-storm rainfall intensity patterns were important in Newcastle in all major flood producing events (all return periods), where they were only important in Perth and Darwin for floods of high return periods, which occur during wet months in wet years, when saturation excess runoff was the dominant mechanism. Additionally, due to the possibility of a change of process from subsurface stormflow to saturation excess when conditions suited this switch, the estimates of flood frequency are highly uncertain especially at high return periods (in Darwin and Perth) and much less in Newcastle (when no process change was involved).
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2

Henkel, Cathy. "Development of audiovisual industries in the Northern Rivers Region of NSW." Thesis, Queensland University of Technology, 2002.

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The proposition that this thesis investigates is that the Northern Rivers region of NSW, the area from Grafton to Tweed Heads, is growing as a lifestyle and learning region with the potential for audiovisual industry activity to develop as a series of networked industry clusters. The cluster model is explored as an alternative approach to industry development that offers new opportunities for enterprise building and new options for government intervention in the cultural industries in the region. The concept of creative industries is also applied to scope new collaboration and economic development options for the cultural industries, creative arts, media and communications sectors and a new agenda for collective action amongst industry players in the region. The thesis confirms that audiovisual and creative industries' activity in the Northern Rivers region has reached a significant level in terms of representation in the workforce and economic and social benefit to the region. The research identified a total of 1,621 people involved in audiovisual industries in the region, representing a growth of 214% since 1996. The total number of people involved in creative industries in the region in 2000 was conservatively estimated to be 3,500, which is 4.1 % of the local work force, a significant figure for a non-metropolitan region. The thesis questioned the usefulness of Australian Bureau of Statistics (ABS) data in providing an accurate picture of creative industries, and the research may be considered a pioneering work in its method of collecting data on creative industry cluster developments in Australia. The thesis concludes that the Northern Rivers region has an active, significant and growing audiovisual industry within the creative milieu of a lively and growing creative industries' sector, and has the potential to develop as a series of networked creative industries' clusters. However, considerable barriers and difficulties exist at both the local and national levels for these industries, and specific measures need to be taken urgently to support this developing sector and to provide the infrastructure and mechanisms needed to ensure that the current growth is sustainable.
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3

Purdy, David John. "Volcanic stratigraphy and origin of the Wallangarra Volcanics, Wandsworth volcanic group, northern NSW, Australia." Thesis, Queensland University of Technology, 2003.

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4

Othman, Rushdy School of Biological Earth &amp Environmental Sciences UNSW. "Petroleum geology of the Gunnedah-Bowen-Surat Basins, Northern New South Wales : stratigraphy, organic petrology and organic geochemistry." Awarded by:University of New South Wales. School of Biological, Earth and Environmental Sciences, 2003. http://handle.unsw.edu.au/1959.4/20537.

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The three-dimensional thermal maturity pattern has been investigated and the hydrocarbon generation potential assessed for the Permian and Triassic sequences of the southern Bowen and northern Gunnedah Basins and the lower part of the overlying Jurassic Cretaceous Surat Basin sequence in northern New South Wales. An oil-source rock correlation also has been investigated in the Gunnedah Basin. Vitrinite reflectance measurements were conducted on 256 samples from 28 boreholes. A total of 50 of these samples were subjected to Rock-Eval pyrolysis analysis, and 28 samples extracted for additional organic geochemical studies (GCMS). A re-evaluation of the stratigraphy in the southern Bowen Basin and a stratigraphic correlation between that area and the northern Gunnedah Basin was also included in the study. An overpressured shaly interval has been identified as a marker bed within the lower parts of the Triassic Moolayember and Napperby Formations, in the Bowen and Gunnedah Basins respectively. Suppressed vitrinite reflectance in the Permian sequence was used as another marker for mapping the stratigraphic sequence in the southern Bowen Basin. The Permian sequence in the Bowen Basin thins to the south, and probably pinches out over the Moree High and also to the west. The coal-bearing Kianga Formation is present in the north and northeastern parts of the study area. A disconformity surface between Digby and Napperby Formations in the Gunnedah Basin is probably time-equivalent to deposition of the Clematis Group and Showgrounds Sandstone in the Bowen Basin. The Clematis Group is absent in the study area, and the Moolayember Formation considered equivalent to the Napperby Formation. Although in many cases core samples were not available, handpicking of coal or shaly materials from cuttings samples where geophysical log signatures identify these materials helped in reducing contamination from caved debris. Histogram plots of reflectance also helped where the target and caved debris were of similar lithology. Vertical profiles of the vitrinite reflectance identified suppressed intervals in the study area due to marine influence (Back Creek Group and Maules Creek Formation) and liptinite rich source organic matter (Goonbri Formation). The suppression occurs due to the perhydrous character of the preserved organic matter. High reflectance values were noted within intrusion-affected intervals, and two types of igneous intrusion profiles were identified; these are simple and complex profiles. An isoreflectance map for the non-suppressed interval at the base of the Triassic sequence in the southern Bowen Basin shows that the organic matter is mature more towards the east close to the Goondiwindi Fault, and also towards the west where the Triassic sequence directly overlies the basement. High values also occur over the Gil Gil Ridge in the middle, to the south over the Moree High, and to the north where the sequence is thicker. The reflectance gradient in the suppressed intervals is higher than in the overlying non-suppressed sequences, especially when the rank has resulted from burial depth. Tmax from Rock-Eval pyrolysis was found to be lower in the perhydrous intervals, and was high in mature and igneous intrusion-affected intervals. Based on the source potential parameters, the Permian Back Creek Group is a better source than the Kianga Formation, while the Goonbri Formation is better than the Maules Creek Formation. The Triassic Napperby Formation has a fair capacity to generate oil, and is considered a better source rock than the equivalent Moolayember Formation. The Jurassic Walloon Coal Measures is a better source than Evergreen Formation, and has the best source rock characteristics, but is immature. The Rock-Eval S1 value shows better correlation with extracted hydrocarbon compounds (saturated and aromatics) than the total extractable organic matter. This suggests that solvent extraction has a greater ability to extract NSO compounds than temperature distillation over the Rock-Eval S1 interval. Terrestrial organic matter is the main source input for the sequences studied. This has been identified from organic petrology and from the n-alkane distributions and the relatively high C29 steranes and low sterane/hopane ratios. The absence of marine biomarker signatures in the Permian marine influenced sequence, could be attributed to their dilution by overwhelming amounts of non-marine organic matter. A mainly oxic to suboxic depositional environment is inferred from trace amounts of 25-NH, BNH and TNH. This is further supported by relatively high pr/ph ratios. Although C29/C30 is generally regarded as an environmental indicator, high values were noted in intrusion-affected samples. The 22S and 20S ratios were inverted ????reaches pseudo-equilibrium???? in such rapidly heated, high maturity samples. The ratio of C24 tetracyclic terpane to C21-C26 tricyclic terpanes decreases, instead of increasing, within the Napperby Formation close to a major igneous intrusive body. The 22S ratio, which is faster in reaction than the other terpane and sterane maturity parameters, shows that the Permian sequence lies within the oil generation stage in the Bowen Basin, except for a Kianga Formation sample. The Triassic sequence is marginally mature, and the Jurassic sequence is considered immature. In the Gunnedah Basin, the Permian sequence in Bellata-1 and Bohena-1, and the Triassic sequence in Coonarah-1A, lie within the oil generation range. In the intrusion-affected high maturity samples, the ratio is reaches pseudo-equilibrium. This and other terpane and sterane maturity parameters are not lowered (suppressed) in the perhydrous intervals. The ???????? sterane ratio, however, is slowest in reaction to maturity, and variations in low maturity samples are mainly due to facies changes. Diasterane/sterane ratios, in the current study, increase with increasing TOC content up to 5% TOC, but decrease in rocks with higher TOC contents including coals. Highly mature samples, as expected, in both cases are anomalous with high ratios. Calculated vitrinite reflectance based on the method of Radke and Welte (1983), as well as MPI 1 and MPI 2, shows the best comparison to observed values. These aromatic maturity parameters are lowered within the reflectance-suppressed intervals. Oil stains in the Jurassic Pilliga Sandstone in the Bellata-1 well have been identified as being indigenous and not due to contamination. The vitrinite reflectance calculated to the oil stain suggests that the source rock should be within a late mature zone. Such high maturity levels are only recognised within intrusion-affected intervals. A close similarity between the oil stain sample and the intruded interval of the Napperby Formation is evident from the thermal maturity and biomarker content. Hydrocarbon generation and expulsion from the lower part of the Napperby Formation as a result of igneous intrusion effects is suggested as the source of the oil in this particular occurrence. Terpane and sterane maturity parameters increase with increasing burial depth in the intervals with suppressed (perhydrous) vitrinite reflectance. The generation maturity parameters also increase through intervals with perhydrous vitrinite, which suggests that hydrocarbons continue to be generated and the actual amount is increasing even though traditional rank ????????????stress???????????? maturity parameters are lowered. Accordingly, the Permian sequences in the lower part of the Bowen Basin are at least within the peak oil generation zone, and probably within late oil generation in the north and northeast of the study area. To generate significant amounts of hydrocarbon, however, the thickness of the shaly and coaly intervals in the Permian sequence is probably a critical parameter. In the Gunnedah Basin, a significant amount of hydrocarbon generation is probably only possible as a result of igneous intrusions.
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5

Liu, Qian. "An ethnopharmacological study of medicinal plants of the Kamilaroi and Muruwari aboriginal communities in northern New South Wales." Electronic version, 2006. http://hdl.handle.net/1959.14/416.

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6

Ritchie, Samuel Gordon Gardiner. "'[T]he sound of the bell amidst the wilds' : evangelical perceptions of northern Aotearoa/New Zealand Māori and the aboriginal peoples of Port Phillip, Australia, c.1820s-1840s : a thesis submitted to the Victoria University of Wellington in fulfilment of the requirements for the degree of Master of Arts History /." ResearchArchive@Victoria e-Thesis, 2009. http://researcharchive.vuw.ac.nz/handle/10063/928.

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7

Johnson, Wendi Leigh. "Policy innovation and policy transfer in Australia : a retirement village case study." Thesis, Queensland University of Technology, 1998.

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8

Noble, Rodney Ian. "Peak labour organisation in the Hunter Valley of New South Wales 1869-1990." Thesis, 2002. http://hdl.handle.net/1959.13/1418193.

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Masters Research - Master of Arts (Economics)
This research thesis traces the development of peak union organisation in the Hunter Valley from its beginnings in 1869 through to 1980, with a postscript covering the more recent years. The study is placed in a political and economic context with the early developments culminating in the formation of the Newcastle Trades Hall Council (NTHC) in 1926. The following chapters trace in some detail the fortunes of that organisation from then on. Although it is a chronological study, it addresses the various themes to emerge from the literature as important to peak union organisations and their historical development. These themes are discussed in the first chapter and they encompass the relationship of the NTHC to the broader labour movement within which it was operating, the degree to which authority and independence were able to be exercised and the critical inter-relationship with community. As well, it also looks at where such a peak union council was placed in respect of the competing ideologies 'socialism' and 'laborism' and the associated struggles to win the hearts and minds of the region's working class. In order to achieve this, the study takes into account the totality of the regional organisation including its industrial, cultural, community, and political involvement. Although it is primarily the history of a peak union organisation, in the process of understanding it, important aspects of the political and cultural life of the working class in the region comes to the surface and allows us a small insight into the social history of the labour movement and of the Hunter Valley's working class as a whole.
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9

Watson, Ian. "Class analysis and environmental politics : timber workers and conservationists in Northern New South Wales 1960-1986." Phd thesis, 1986. http://hdl.handle.net/1885/131957.

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In this thesis I explore the conflicts which have arise between middle class' conservationists and working class timber communities. I examine the New South Wales rainforest controversy as a case study and seek to place the animosity and hostility which arose there within the context of class analysis. At the same time, I integrate other important dimensions of social life, particularly rural ideologies and ideologies of masculinity, into an overall analysis of class power. I show that important cultural divisions underlaid the political conflict, particularly differing conceptions of nature and history, and that these had their roots in different labour processes. After introducing my theoretical framework, I provide an economic context for my cultural analysis by examining the restructuring of the north coast hardwood timber industry during the 1960s and 1970s. This is followed by two chapters which analyse the labour process in the timber industry. Here I explore both class struggles on the shop-floor and cultural productions which arise within the workplace and in rural communities. The subsequent chapters focus more closely on environmental politics. I analyse the New South Wales rainforest campaign by offering a critique of 'pluralist' political strategies and I then locate this campaign within a wider context by briefly overviewing the anti -uranium and green bans campaigns of the 1970s. One of my major conclusions is that environmental politics is flawed by the neglect by activists of the class effects of their political activities. Assessments of political campaigns solely in terms of ecological goals are seriously deficient because they fail to register how conservationists' actions facilitate capitalist strategies of industry restructuring and thereby further entrench capitalist class power. Theoretically, my thesis is based on principles of 'realist' methodology and I use concepts drawn from labour process theory, class analysis, and the theory of ideology. The thesis is heavily weighted toward oral history material, gathered during field work interviews on the north coast of New South Wales. I analyse this material using 'popular memory' theory and other studies of working class culture. In so doing, the thesis provides timber workers with a voice in a debate which has largely been dominated by 'middle class' conservationists. Politically, the thesis is an intervention into current debates about new social movements and their relationship to the left. I argue that an effective alliance between socialists and environmentalists entails a rejection of wilderness politics in favour of urban environmental issues. I conclude that 'pluralist' political strategies of lobbying for state- conferred concessions should be rejected in favour of strategies which develop alternative economic programmes at local and regional levels.
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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) and groundwater. Surface water was sampled at ten sites along Wybong Creek over three years, while groundwater was sampled from most of the bores and piezometers occurring in the Wybong Creek valley. Surface and groundwater in the upper catchment were dominated by Na-Mg-HCO3. Ratios of 87Sr/86Sr and cation/HCO3 indicated these facies were due to silicate weathering of the Liverpool Ranges, with localised groundwater bodies recharging in the Liverpool Ranges and discharging in the upper Wybong Creek valley. Wybong Creek became saline, and Na-Mg-Cl dominated in the mid-catchment area, with salinity doubling between the 55 and 60 km sample sites on some dates. Changes in surface water chemistry occurred independently of surface water input from tributaries, with abrupt salinity increases within a pool between these sites attributed to groundwater input via fractures beneath the Creek. One of two salt scalds in the Wybong Creek catchment also occurs adjacent to this stretch of river. A field site was established at the mid-catchment locality of Manobalai, therefore, in order to constrain the relationship between surface water, regolith and groundwater salinity. Ten piezometers were established at Manobalai, including three piezometer nests. Most regolith at Manobalai was found to be non-saline, including that within the salt scald, with the most saline and Na-Cl dominated regolith samples occurring in some of the most moist and coarse sandy/gravel layers. Groundwater sampled from piezometers installed in the holes drilled for regolith samples had salinities up to 20 times higher than the regolith on a per weight basis, and were similarly dominated by Na-Cl. A lack of carbonate and sulfate minerals within the soils and no indication of Ca-Mg/HCO3- SO4 dominated facies within alluvial soil solutions indicated groundwater did not evolve from rainwater to Na-Cl dominated facies while infiltrating the regolith. Groundwater samples from Manobalai were instead found to be amongst the most fresh and the most saline within the Wybong Creek catchment, and changed salinity abruptly down-gradient along a transect. Groundwater flow occurred through fractures in the Narrabeen Group sandstones and conglomerates, with vertical groundwater flow via fractures causing abrupt changes in salinity. Ratios of Na/Cl, Cl/Br and 87Sr/86Sr indicated saline groundwater at Manobalai and in the lower catchment was influenced by a marine endmember and halite dissolution. A poor relationship between salinity and d18O indicated this marine endmember was not evapoconcentrated rainwater. The occurrence of saline surface and groundwater in the Wybong Creek catchment was instead attributed to discharge from the regional groundwater system occurring in the Wittingham Coal Measures, with the abrupt increases in salinity at Manobalai indicating mixing between local, intermediate and/or regional groundwater systems. Salinity is likely to function similarly to this in the rest of the Hunter Valley also. The occurrence of salinity in both the Hunter River and Wybong Creek catchments is a naturally occurring phenomenon with salinity mitigation difficult due to the regional extent of the saline groundwater systems. Living with salt strategies are therefore recommended, such as limiting irrigation using both saline and fresh water and continuing with restrictions on saline discharge from coal mines.
This work was supported by ARC Linkage grant number LP05060743. Scholarship funding was provided by The Australian National University Faculty of Science and Research School of Earth Sciences, with project funding and support also provided by Hunter Central Rivers Catchment Management Authority and the New South Wales Office of Water.
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Книги з теми "Newcastle and Northern New South Wales"

1

Parsons, Margaret. Burials in Wallsend Cemetery, New South Wales, 1896-2008. Lambton, NSW: Newcastle Family History Society, 2009.

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2

Austin, Peter. A reference dictionary of Gamilaraay, northern New South Wales. Bundoora, Vic: La Trobe University, Dept. of Linguistics, 1992.

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3

Hinchman, Lewis P. Hiking tropical Australia: Queensland and northern New South Wales. Potsdam, NY: Grass Tree Press, 1999.

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4

Austin, Peter. A reference dictionary of Gamilaraay, northern New South Wales. Bundoora, Vic., Australia: La Trobe University, Dept. of Linguistics, 1993.

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5

Gordon, Moira. Redundancy, employment and occupational status: Ex-steel industry employees, Newcastle, New South Wales. [Newcastle], N.S.W., Australia: Dept. of Economics and Institute of Industrial Economics, University of Newcastle, 1986.

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6

David, Copsey, ed. Australia: Queensland, New South Wales, Victoria, Tasmania, South Australia, Western Australia, Northern Territory. New York: Gallery Books, 1987.

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7

Hoffman, Eric. Adventuring in Australia: New South Wales, Northern Territory, Queensland, South Australia, Tasmania, victoria, Western Australia. 2nd ed. San Francisco: Sierra Club Books, 1999.

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8

Hackett, Frances. Trailing clouds of glory: An informal chronicle of northern New South Wales, 1930-46. South Yarra, Melbourne, Vic: Hyland House, 1990.

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9

Hackett, Frances. Trailing clouds of glory: An informal chronicle of northern New South Wales, 1930-46. South Yarra, Melbourne, Vic: Hyland House, 1990.

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10

Australasian, Institute of Mining and Metallurgy (1995 Newcastle N. S. W. ). The AusIMM Annual Conference 1995: Adding value to our resources, our future, 23-26 March 1995, Newcastle, New South Wales. Carlton, Vic: Australasian Institute of Mining and Metallurgy, 1995.

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Більше джерел

Частини книг з теми "Newcastle and Northern New South Wales"

1

Wessell, Adele. "Unsettling the History of Macadamia Nuts in Northern New South Wales." In Food and Identity in a Globalising World, 109–26. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-030-96268-5_6.

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2

Knowles, Ross, and Michael Mahony. "Endangered frog invokes a Fauna Impact Statement in northern New South Wales." In Herpetology in Australia, 304. P.O. Box 20, Mosman NSW 2088, Australia: Royal Zoological Society of New South Wales, 1993. http://dx.doi.org/10.7882/rzsnsw.1993.045.

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3

Clancy, Greg P. "Vertebrate Fauna and its management on an urban block in northern New South Wales." In A Zoological Revolution, 155–62. P.O. Box 20, Mosman NSW 2088, Australia: Royal Zoological Society of New South Wales, 2002. http://dx.doi.org/10.7882/fs.2002.013.

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4

Mee, Kathleen, Pauline McGuirk, Jill Sweeney, and Kristian Ruming. "First We Had to Make It Livable: The Affordances of Livability in Suburban Newcastle, New South Wales, Australia." In Community Livability, 165–80. Second Edition. | New York : Routledge, 2020. | “First edition published by Routledge 2012”–T.p. verso.: Routledge, 2019. http://dx.doi.org/10.4324/9781315111636-14.

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5

Esdaile, Jeff. "The Development and Operation of No-till Farming in Northern New South Wales (NSW), Australia." In Rainfed Farming Systems, 1103–21. Dordrecht: Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-1-4020-9132-2_45.

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6

Alimardanian, Mahnaz. "Burnt Woman of the Mission: Gender and Horror in an Aboriginal Settlement in Northern New South Wales." In Monster Anthropology in Australasia and Beyond, 93–108. New York: Palgrave Macmillan US, 2014. http://dx.doi.org/10.1057/9781137448651_6.

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7

Tarvey, Lance. "First nesting records for the Leatherback Turtle Dermochelys coriacea in northern New South Wales Australia, and field management of nest sites." In Herpetology in Australia, 233–38. P.O. Box 20, Mosman NSW 2088, Australia: Royal Zoological Society of New South Wales, 1993. http://dx.doi.org/10.7882/rzsnsw.1993.036.

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8

Tasker, Elizabeth M., and Christopher R. Dickman. "Small mammal community composition in relation to cattle grazing and associated burning in eucalypt forests of the Northern Tablelands of New South Wales." In Conservation of Australia's Forest Fauna, 721–40. P.O. Box 20, Mosman NSW 2088: Royal Zoological Society of New South Wales, 2004. http://dx.doi.org/10.7882/fs.2004.043.

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9

Gratchev, Ivan, Sinnappoo Ravindran, Dong Hyun Kim, Chen Cui, and Qianhao Tang. "Mechanisms of Shallow Rainfall-Induced Landslides from Australia: Insights into Field and Laboratory Investigations." In Progress in Landslide Research and Technology, Volume 1 Issue 1, 2022, 113–22. Cham: Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-16898-7_7.

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Анотація:
AbstractThis paper presents and discusses the mechanisms of rainfall-induced shallow landslides that commonly occur in South East Queensland (SEQ) and northern New South Wales (NSW), Australia. The major factors causing the formation of landslide mass such as geology, weathering, and rainfall patterns were discussed. Results from field surveys and laboratory testing of rock/soil material from landslide masses were presented, and relationships between the material strength and landslide occurrence were drawn. It was found that most of shallow slides were related to sandstone deposits. Those failures occurred on natural slopes and road cuts with the inclination of the failure plane being in the range of 35–45°. For natural slopes where the landslide mass mostly consisted of coarse-grained soil, the relationship between the soil strength and water content was established. In addition, the relationship between rainfall patterns such as intensity and duration, and the landslide occurrence was presented. Based on the data from field work and laboratory results including a series of flume tests, the mechanism of shallow landslides triggered by rainfall events was identified and discussed.
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10

"Newcastle, New South Wales: win–win solutions for climate protection?" In Cities and Climate Change, 163–80. Routledge, 2003. http://dx.doi.org/10.4324/9780203219256-16.

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Тези доповідей конференцій з теми "Newcastle and Northern New South Wales"

1

"Impacts of a two degree increase in temperature on pasture growth in the Northern Tablelands of New South Wales." 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.b1.powell.

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Звіти організацій з теми "Newcastle and Northern New South Wales"

1

Savings Bank of New South Wales - Newcastle - Depositors Ledgers - Accounts 1521-2265 - 1869-1880. Reserve Bank of Australia, March 2021. http://dx.doi.org/10.47688/rba_archives_2006/21850.

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2

Savings Bank of New South Wales - Newcastle - Depositors Ledgers - Accounts 2266-3459 - 1871-1880. Reserve Bank of Australia, March 2021. http://dx.doi.org/10.47688/rba_archives_2006/21852.

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3

Savings Bank of New South Wales - Newcastle - Depositors Ledgers - Accounts 1-519 (Indexed) - 1858-1871. Reserve Bank of Australia, March 2021. http://dx.doi.org/10.47688/rba_archives_2006/21847.

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4

Government Savings Bank of New South Wales - Martin Place, Sydney - Depositors Ledgers - Accounts - Newcastle - Parramatta Street - 1876 - 1881. Reserve Bank of Australia, March 2021. http://dx.doi.org/10.47688/rba_archives_2006/22517.

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5

Savings Bank of New South Wales - Sydney (Head Office) - Ledgers - No. 13 Accounts - 301-400 - Newcastle Depositors - 1862. Reserve Bank of Australia, March 2021. http://dx.doi.org/10.47688/rba_archives_2006/21538.

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6

Savings Bank of New South Wales - Sydney (Head Office) - Ledgers - No. 4 Accounts - 1853-3341 - Newcastle Depositors - 1870-1875. Reserve Bank of Australia, March 2021. http://dx.doi.org/10.47688/rba_archives_2006/21547.

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7

Savings Bank of New South Wales - Sydney (Head Office) - Ledgers - No. 2 Accounts - 634-1250 - Newcastle Depositors - 1864-1875. Reserve Bank of Australia, March 2021. http://dx.doi.org/10.47688/rba_archives_2006/21545.

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8

Secretary's Department - Lectures - Governor - University of New South Wales - "Development of Northern Australia" - 1961. Reserve Bank of Australia, September 2022. http://dx.doi.org/10.47688/rba_archives_2006/06202.

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9

Savings Bank of New South Wales - Sydney (Head Office) - Ledgers - No. 1 Accounts - 4-633 - Newcastle Depositors (incl. Continuation) - 1863-1875. Reserve Bank of Australia, March 2021. http://dx.doi.org/10.47688/rba_archives_2006/21541.

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10

Savings Bank of New South Wales - Sydney (Head Office) - Ledgers - Accounts 1-309 Wollongong Depositors (1856-1862) 1-300 Newcastle Depositors (1858-1862) 1-135 Sofala Depositors (1856-1862). Reserve Bank of Australia, March 2021. http://dx.doi.org/10.47688/rba_archives_2006/21576.

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