Arsenic (As) in groundwater systems is a problem in many parts of the world owing to ever-increasing extraction of groundwater resources to meet the needs of growing populations. Surprisingly, the occurrence of elevated As concentrations in coastal sandy aquifers has only recently been published as a result of this research. Sandy aquifers are commonly used as a clean and reliable source of water for domestic, agricultural and industrial needs due to their high recharge rates and the filtering capacity of sands. Water quality monitoring in Australian sandy aquifers is usually limited to a small suite of major elements and salinity measurements to determine the quality of groundwater and to identify any potential problems from seawater intrusion as a result of over extraction. Minor and trace elements, particularly toxic elements, have largely been ignored in regular monitoring programs. Prompted by an emerging pattern of human health problems in a community reliant on groundwater, hydrogeochemical investigations of the Stuarts Point coastal sand aquifer, on the North Coast of New South Wales, Australia, identified elevated As concentrations of up to 337 ????g/L in the catchment's Pleistocene barrier sands. These concentrations are well in excess of the World Health Organisation and the Australian National Health and Medical Research Council water quality criteria of 10 and 7 ????g/L respectively. From research into the Stuarts Point geology, geochemistry, geomorphology, hydrogeology and hydrogeochemistry, and with the assistance of environmental isotopes, the spatial distribution, occurrence and mobilisation processes of As were determined. The presence and distribution of elevated As concentrations in the regional coastal aquifer system are sporadic and involve a series of complex hydrogeochemical processes. No single hydrogeochemical process can describe the release of As from solid phase to groundwater system on the regional scale. Processes of competitive exchange with PO43- and HCO3-, reductive dissolution of Fe oxyhydroxides and arsenical pyrite oxidation, though not forming dominant correlations, are still evident and influence As chemistry at this scale. Detailed investigations of the hydrogeochemistry on the vertical scale have identified two main processes as causing As to be released and mobilised. The first process is associated with the oxidation of arsenical pyrite in Acid Sulphate Soils and metal hydrolysis reactions which mobilise As in the acidic environment. In the absence of dissolved oxygen (DO), NO3- acts as the oxyanion facilitating arsenical pyrite oxidation and releasing As into solution. The second process that mobilises As from the sediments is the liberation of As from metal-oxyhydroxides in the carbon-rich environment, where HCO3- originates from the dissolution of shell material in the Pleistocene barrier sands. The marine influenced depositional history and geomorphology of the aquifer provide opportunities for As to become incorporated into the aquifers matrix in a variety of mineral forms, which is an occurrence not considered to be unique to the Stuarts Point catchment. The findings presented here are amongst the first detailed studies of naturally occurring As in an Australian groundwater system as well as in the Pleistocene coastal sand aquifer environment. The understanding of As accumulation and mobilisation identified as a result of this research emphasises the need for potential As occurrences in similar groundwater systems in other coastal environments in Australia, and globally, to be considered.

Spicers Creek catchment is located approximately 400 km west of Sydney in the Central West region of New South Wales, Australia. Dryland salinity has been recognised as a major environmental issue impacting soil and water resources in the Central West region of NSW for over 70 years. Due to the geological complexity of the catchment and the presence of high salt loads contained within the soils, groundwater and surface waters, the Spicers Creek catchment was identified as a large contributor of salinity to the Macquarie River catchment. Over fifty-two dryland salinity occurrences have been identified in the Spicers Creek catchment and it appears that dryland salinity is controlled by the presence of geological structures and permeability contrasts in the shallow aquifer system. Combinations of climatic, geological and agricultural factors are escalating salinity problems in the catchment. The main aim of this thesis was to identify the factors affecting salinisation processes in the Spicers Creek catchment. These include the role of geological structures, the source(s) of salts to the groundwater system and the geochemical processes influencing seepage zone development. To achieve these aims a multidisciplinary approach was untaken to understand the soils, geology, hydrogeology and hydrogeochemistry of the catchment. Investigative techniques employed in this project include the use of geophysics, soil chemistry, soil spectroscopy, hydrogeochemistry and environmental isotopes. Evaluation of high-resolution airborne magnetics data showed a major north-east to south-west trending shear zone. This structure dissects the catchment and several other minor faults were observed to be splays off this major structure. These structures were found to be conducive to groundwater flow and are influencing the groundwater chemistry in the fractured aquifer system. Two distinctive groundwater chemical types were identified in the catchment; the saline Na(Mg)-Cl-rich groundwaters associated with the fractured Oakdale Formation and the Na-HCO3-rich groundwaters associated with the intermediate groundwater system. The groundwater chemistry of other deep groundwaters in the catchment appears to be due to mixing between these end-member groundwaters within the fractured bedrock system. The spatial distribution of electrical conductivity, Cl-, Sr2+ and 87Sr/86Sr isotopic ratios showed the correlation between saline groundwaters and the location of faults. Elevated salinities were associated with the location of two crosscutting fault zones. The spatial distribution of HCO3-, K+, Li+ and ?????3CDIC highlighted the extent of Na-HCO3-rich groundwaters in the catchment and showed that these groundwaters are mixing further east than previously envisaged. These findings show that Na(Mg)-Cl-rich groundwaters are geochemically distinctive and have evolved due to extensive water-rock interaction processes within the fracture zones of the Oakdale Formation. These saline groundwaters contain elevated concentrations of trace elements such as As, V and Se, which pose a potential risk for water resources in the area. 87Sr/86Sr isotopic ratios indicated that the source of salinity to the Na(Mg)-Cl-rich groundwaters was not purely from marine or aerosol input. Salt is most likely contributed from various allochthonous and autochthonous sources. This research found that the main mechanism controlling the formation of dryland salinity seepage zones in the Spicers Creek catchment is due to the presence of geological structures. These groundwater seepage zones act as mixing zones for rainfall recharge and deeper groundwaters. The main sources of salt to the seepage zones are from deeper Na(Mg)-Cl-rich groundwaters and rainfall accession. The major importance of this research highlights the need for an integrated approach for the use of various geoscientific techniques in dryland salinity research within geologically complex environments.

Doctor of Philosophy(PhD) / This thesis concentrates on the role of Welsh noblewomen in the history of Wales in the thirteenth century. Their absence from this history until quite recently is discussed, and several outstanding Welsh noblewomen have been studied in detail. The women studied include the mothers, wives and daughters of the native Welsh rulers of Gwynedd as well as noblewomen from northern Powys, Cydewain, Ceredigion, and so on. One chapter of the work is devoted to the Welsh Laws of Women which, although somewhat archaic by the thirteenth century, were still in use in some parts of Wales and help provide background. Another chapter investigates the evidence for women in the extant literature and poetry of the period. The thesis explores the themes of women’s access to power through the family and also the ability of Welsh noblewomen to take action in their own and their family members’ interests, in the public sphere, when they felt it was necessary. While the later years of the thirteenth century witnessed the final defeat of the Welsh by the Anglo-Normans after more than two hundred years, earlier in the century, Welsh leaders had been able to unite under the leadership of the rulers of Gwynedd and achieve a measure of independence from their oppressors. Welsh noblewomen played an important part in this recovery of Welsh power and their participation in this aspect of Welsh medieval history is also explored. It is clear from the evidence collected that most of the noblewomen studied owned land, in spite of the prohibition against women owning land under native Welsh law. Welsh noblewomen supported their fathers, husbands and sons, and they also took direct action themselves when the need arose.

Master of Visual Arts / This paper grows out of my ongoing practice of photographing the Darling River in western NSW. My interest in imaging the landscape and representing the contemporary divisions within it led me to investigate previous colonial conflicts, which occurred as white explorers in the 1830’s and squatters in the 1850’s took over the Aboriginal tribal lands on the Darling. In this paper I investigate the images created by explorers, artists and photographers, which were the beginnings of a Eurocentric vision for this land. These images were created in the context of a colonial history which forms the ideological backdrop to historical events and representations of this land. This research has involved me in an investigation across three different disciplines; Australian history, Australian visual art, and environmental aspects of human interactions with the land. The postcolonial histories which inform my work are themselves re-evaluations of earlier histories. This recent history has revealed, amid the images of European ‘settlement’ and ‘progress’, views of frontier violence and Aboriginal resistance to colonisation that were excluded from earlier histories. The fan-like shape of the Darling River, which for millennia has bought water to this dry land, is the motif that focuses my investigation. I discuss the relatively recent degradation of the river, which is the focus of contemporary conflicts between graziers, Aboriginal people, environmentalists and irrigators. Because large-scale irrigation now has the capacity to divert the flows of entire rivers for the irrigation of cash crops, the insecurities of earlier generations over the ‘unpredictable’ floods and their perception of lack of control over water - has been entirely reversed. ‘Control’ of water is now held by irrigators and the river down stream from the pumps is kept at a constant low, becoming a chain of stagnant waterholes during summer. Like many rivers in industrialised countries, the Darling no longer flows to its ocean. The physical characteristics of rangeland grazing are an important background to my paper. Although the introduction of sheep and cattle has altered and degraded this landscape, unlike ploughed country to the east this land retains much of its native vegetation and an Aboriginal history embedded across its surface. This paper is an investigation of the changing representations of the Australian landscape, and central to my paper (and a result of growing up in this area) is my recognition, at an early age, of cultural difference in the context of this landscape. I became aware of contradictions in how Aboriginal people were treated by the ‘white’ community and I glimpsed the distinct cultural viewpoints held by Aboriginal people. A connection to country continues to be expressed in art produced by Aboriginal people in the Wilcannia area, including work by Badger Bates and Waddy Harris. The Wilcannia Mob, a schoolboy rap-group received national press coverage, winning a Deadly Award in 2002 for their acclaimed song ‘Down River’. While a discussion of these artworks is not part of the discussion of my paper, it is a context for my research. In broad terms this paper is an investigation of different worldviews, different views of land and landscape by graziers, Aboriginal people, environmentalists and irrigators. These views carry with them different cultural understandings and different representations of the land - different and sometimes opposing views of its past and its future. It seems in 2005 that, just as artists, historians, filmmakers, etc. are beginning to come to terms with Australian colonial history, as the El Nino seasons and the importance of ‘environmental flows’ in the Murray Darling Basin are increasingly understood, that technological changes and the global effects of population densities are creating other changes (greenhouse gasses, ozone depletion, climate changes) that once again appear to be unpredictable and beyond our control. While this environmental discussion is outside the scope of the current paper it is a context for my investigation of this landscape.

Doctor of Philosophy / The impact of the variability in timber properties has been a challenge for companies involved in drying timber, which have to handle these variations and at the same time meet the requirements stated in the Australian/New Zealand Standard for the assessment of dried timber quality (2001). The definition of quality considered in this study is to both minimize the dispersion of the final moisture contents in dried timber boards, and to reduce cracking/checking. Anecdotal evidence also suggests that the timber properties of plantation timber appear to be more variable compared with the properties of old growth or regrowth timber. Therefore, this thesis focuses on measuring the amount of variability of timber properties by conducting drying experiments using timber boards taken from different locations within a single tree and between trees, for regrowth and plantation blackbutt timber (Eucalyptus pilularis Sm.). The quantified variabilities were then used to develop optimized timber drying schedules that are intended to dry regrowth and plantation blackbutt boards as quickly as possible (highest productivity) without cracking (quality loss) in the presence of large biological variability. Blackbutt (Eucalyptus pilularis Sm.) was the chosen species for this thesis because of its abundance in New South Wales. It is considered to be one of the most important eucalypts for planting in NSW. It has superior growth and high survival rates compared with other eucalyptus species, and the timber is marketable. Lastly, conventional kiln drying was considered in this thesis compared with other drying methods such as air drying and solar kilns due to (arguably) better control of the drying conditions and faster throughput in conventional drying. The higher costs of conventional kiln drying are compensated, relative to open—air drying, by the reduction in stock level and faster turnaround of green to dried timber. Firstly, an overview of previous work on the development and evaluation of different drying schedules was given. Previous work either developed optimized drying schedules to minimize the dispersion of the final moisture contents, or reduced cracking/checking. No schedule has been developed to satisfy both aspects of quality. In addition, only one report has taken into consideration biological variability in the development of an optimized drying schedule, but this approach has not been tested experimentally. In addition, the information on the variability of biological parameters was very limited, was assumed to be normally distributed, and the parameters were assumed to be uncorrelated with one another. There is little information about the variability in timber properties with respect to drying, including how strongly they are correlated. This thesis has particularly addressed this aspect of the problem. Drying experiments using conventional kiln drying were conducted. The properties of two regrowth blackbutt logs (36 boards) and two plantation blackbutt logs (24 boards), have been measured and analysed for the within—tree variation of timber properties. In a separate set of experiments, two boards were taken from each log, from a total of 12 regrowth logs and 10 plantation logs, to study the between—tree variability of the timber properties of blackbutt timber. The timber properties measured consisted of the basic density, the initial moisture content, the diffusion coefficient, the failure strain, the failure stress, the modulus of elasticity and the shrinkage. The amount of cracking or checking and the dispersion of final moisture contents were assessed. 90% of the regrowth timber and 90% of the plantation timber fell in the Class C quality for surface checking, regrowth timber fell in Class B for end checking, while the end checks in the plantation timber fell in Class C for quality. Regrowth timber therefore appeared here to have slightly better quality than plantation material when dried with the same drying schedule, as here, in agreement with anecdotal suggestions that plantation material is more difficult to dry well. 95% of both the regrowth and the plantation timber fell in Class E quality for internal checking. Overall, along with the assessment that both regrowth and plantation timber was Class C quality for the variation of final moisture contents, these regrowth timber boards and the plantation timber boards fell in the lower quality classes for the criteria of checking and target moisture content for appearance products. Quality Classes A and B are higher quality categories, for appearance—grade products. The dispersion of the final moisture contents was greater with the plantation blackbutt timber (0.24 within; 0.36 between) than with the regrowth blackbutt timber (0.19 within; 0.15 between) for both within—tree and between—trees variability, respectively. In general, the diffusion coefficients for the timber in this thesis ranged between 1.14×10—10 and 6.77×10—10 m2s—1. There was a significant difference between the diffusion coefficients of the plantation and regrowth blackbutt timber for the within—tree test at a 0.05 significance level. The variation in the diffusion coefficients within a single plantation blackbutt log was higher than the variation in the diffusion coefficients within a regrowth blackbutt log. In addition, there was also a significant difference between the diffusion coefficients of regrowth and plantation blackbutt timber at a 0.05 significance level for between—trees variability. The initial moisture contents, the diffusion coefficient, and shrinkage decreased from pith to bark and the basic density and the modulus of elasticity (MOE) increased in the same direction, within a tree, for both regrowth and plantation blackbutt. The results of the analysis of variance (ANOVA) showed that radial and circumferential effects were significant sources of the within—tree variations for the diffusion coefficient, the initial moisture content, the basic density, the failure strain, the failure stress, the modulus of elasticity and shrinkage. A similar result was found for the ANOVA between trees. The ANOVA results also indicated that the smaller—sized samples used for the analysis (i.e. sub—samples of eight boards for the within—tree test of regrowth blackbutt, sub—samples of four boards for the between—trees test of regrowth blackbutt, sub—samples of six boards for the within—tree test of plantation blackbutt, and sub—samples of six boards for the between—trees test of plantation timber) were sufficient to measure the key effects adequately for the variabilities of the physical, transport, and mechanical properties, provided that all combinations of sub—samples were considered. There was no significant difference between the ANOVA results for these smaller sized samples (less than 1% change), considering all combinations, and the ANOVA results for the ‘full’ board cases. Though the sample sizes were unusually small to represent population statistics by most standards, all combinations of the sub-sets were assessed and an averaged picture of the situation with smaller sample sizes was given. Moreover, MOEs (both green and kiln—dried states) of plantation blackbutt were lower compared with the MOE of regrowth blackbutt. It is possible that the MOE was correlated with the basic density, and the basic density of regrowth blackbutt was higher than the basic density of plantation blackbutt. The shrinkage in the tangential direction was approximately twice the amount of radial shrinkage. The ranges of the measured radial shrinkage values were 0.024 – 0.094 mm mm-1 for regrowth blackbutt and 0.037 – 0.125 mm mm-1 for plantation blackbutt. The higher shrinkage values for plantation blackbutt timber show that plantation material is less stable dimensionally, and this situation is possibly due to the high juvenile wood content and low basic density. These differential (tangential:radial) shrinkage values ranged from 1.12 – 2.93 for regrowth blackbutt and 1.09 – 2.92 for plantation blackbutt. Tests were conducted to determine the degree of statistical normality for the distribution of each property (physical, transport, and mechanical). The results of the normality tests showed that most timber properties for regrowth and plantation blackbutt timber were distributed normally on a linear scale based on the W test, both within and between—trees. On the other hand, some timber properties showed a better fit with the three—parameter lognormal distribution, such as the diffusion coefficient and the green failure strain for within—tree variability of regrowth timber. The means and standard deviations of these distributions were further analysed by applying significance tests at a 0.05 level. For regrowth blackbutt, the data for the initial moisture content, the basic density, the diffusion coefficient, and shrinkage showed no significant differences, comparing the cases within and between—trees. The mechanical behaviour, however, was significantly different between each group and suggested that the two regrowth trees used for the within—tree test were stiffer than the 12 trees used for the between—trees test. It was possible that the mechanical properties were dependent on the geographic location where the tree was felled, and the heartwood content of each log. On the other hand, since all the plantation logs used for the within and between—trees tests were taken from one location, the mechanical properties were not significantly different within the plantation sample. The silviculture and the age of all the plantation trees were the same, which might have contributed to the small variation of the timber properties between the within—tree and between—trees cases for plantation material. Lastly, a significance test was conducted to compare the properties of regrowth and plantation blackbutt timber. Most timber properties (except for the initial moisture content) were significantly different between regrowth and plantation blackbutt. Plantation blackbutt timber had a lower basic density, higher diffusion coefficient and shrinkage, and the modulus of elasticity (both in its green and dried states) was lower compared with regrowth blackbutt timber. In addition to geographic location, heartwood/juvenile content, maturity (age), and differences in microfibril angle may have affected these timber properties in plantation blackbutt timber. For all the experiments, the possibility that there is a correlation between high initial moisture contents, higher diffusion coefficients, low basic densities, and low green modulus of elasticity’s (MOE) was assessed using principal components analysis (PCA). A principal components analysis was performed on the four parameters: the basic density, the initial moisture content, the diffusion coefficient, and the green MOE. The results of the PCA showed that the principal component for the within—tree and between—trees test accounted for 93% and 94% (for regrowth), and 92% and 90% (for plantation), respectively, of the total amount of variation within these parameters, giving some support for the mentioned correlation between the parameters. The strong correlation between the diffusion coefficient and the basic density, D; the diffusion coefficient and the initial moisture content, Xi; and the diffusion coefficient, D, and the modulus of elasticity, EG were represented by empirical equations. The F significance test was conducted to determine if the equations from the within—tree and between—trees tests, and the regrowth blackbutt and plantation blackbutt tests, were significantly different. The difference between the equations for the within—tree and between—trees variability of plantation blackbutt timber (Factual= 1.35  Fexpected= 2.13) was the only result that showed no significant difference. A possible reason for this finding is that the boards from the within—tree and between—tree variability tests, hence the trees, were all felled from one location. On the other hand, the other tests compared boards that were taken from trees felled from different locations, including the regrowth blackbutt within trees, compared with between trees. The results of the significance tests imply that boards taken from one location, whether they are within—tree and between—tree samples, have probably come from the same overall population. Hence using any of the correlations (within—tree or between—trees for plantation blackbutt) would be suitable to estimate the diffusion coefficient of other plantation blackbutt samples at the same location. Overall, these empirical equations can be used to estimate important drying properties of other regrowth and plantation blackbutt samples, such as the diffusion coefficient, using easily measured properties, like the initial moisture content or the basic density, as long as the boards are taken from the same age group (i.e. regrowth or plantation) and the same location. Thereafter, the blackbutt timber boards may be segregated based on the range of diffusion coefficients as estimated from the densities or the initial moisture contents. Hence a suitable drying schedule should be chosen for each segregated group. Collapse was not significant for blackbutt samples studied in this thesis, and possibly this timber species in general, but it may be significant for other eucalyptus species such as collapse—prone Eucalyptus regnans F. Muell (mountain ash) This potential limitation means that care is needed in applying the relationships found in this thesis to collapse—prone species. The same drying model was used to assess the effects of different drying schedules (i.e. increasing and decreasing the dry—bulb and wet—bulb temperatures of the original drying schedule by 5oC and 10oC) and of the potential correlations between the diffusion coefficient, the green MOE, the shrinkage coefficient (calculated from the tangential shrinkage), and the initial moisture content on the variability of final moisture contents, when the average moisture content within a stack of timber reached 15%. In addition, the maximum strain attained by the timber boards was also predicted. The results show that for regrowth blackbutt timber and accounting for within—tree variability, there was no relationship between the length of the drying schedule and the dispersion of final moisture contents. As the temperatures increased, the dispersion of the final moisture contents showed no consistent trend. The absence of a clear trend may be due to the different locations where the logs used for the within—tree test of regrowth variability were taken. On the other hand, the between—tree variability sensitivity tests for both regrowth and plantation blackbutt timber and the within—tree variability sensitivity test for plantation blackbutt timber show a relationship between the length of the drying schedule and the dispersion of final moisture contents. The dispersion of the final moisture contents decreased as temperatures increased. Generally, the ‘+10oC’ drying schedule gave the shortest time for the stack of timber to reach the target average moisture content, and its conditions produced the smallest dispersion of final moisture contents. It was also observed, however, for all sensitivity tests, that as the temperature of the drying schedule increased, the average predicted values decreased for the maximum strains reached. This is a very unusual result, because normally the strains and stresses would be expected to increase with increasing temperature. A possible reason for this is that within a piece of timber, as the temperatures increase, the diffusion coefficient will increase because the internal average temperature increases, so the internal resistance to mass transfer decreases, which leads to the moisture content gradient decreasing, even though the drying rate may slightly increase. This decreases both the drying time and the maximum strain reached as the temperature increases. There are limitations, however, associated when using high temperatures in kiln drying such as collapse and timber discolouration. The optimization technique created by Pordage (2006) was improved by using a large number of measurements to quantify the variability in the properties of blackbutt timber. The first simulation accounted for the between—tree variability of the biological parameters in regrowth blackbutt, and the second simulation accounted for both the within and between—tree variability of the timber properties in plantation blackbutt. Since location was observed as a main source of variability, the timber properties used for each simulation were taken from the logs that were felled from the same location. The mean and the standard deviations of the initial moisture content, the reference diffusion coefficient, and the shrinkage coefficient of regrowth and plantation blackbutt timber boards measured in the actual drying experiments, along with the covariance between these properties represented by a covariance matrix, were used for each simulation. The total drying time of the optimized drying schedule of plantation blackbutt timber was longer (an additional 168 hours, i.e. 472 hours) compared with the total drying time of the optimized drying schedule of regrowth blackbutt timber (304 hours). Due to the greater variability present in plantation blackbutt, slower drying is required. Moreover, the total drying times from the ‘regrowth blackbutt’ optimization and the ‘plantation blackbutt’ optimization (which both accounted for variability) were shorter compared with the total drying time of the original drying schedule for 28 mm—thick mixed—sawn blackbutt boards, i.e. 504 hours. On the other hand, the total drying times of the optimized drying schedules of regrowth and plantation blackbutt timber were greater than the total drying time (152 hours) predicted by Pordage’s (2006) optimized drying schedule accounting for the variability of Eucalyptus paniculata (grey ironbark). He had limited information on the variability of the parameters of grey ironbark and thus used an estimate from another eucalyptus species, Eucalyptus obliqua (messmate), whereas in this thesis, the variabilities for regrowth and plantation blackbutt used for the optimization technique were measured and part of the scope for this study. Overall, this is a typical application of the data obtained in this thesis to the optimization of drying schedules.

The research outlined in this thesis explores the issue of the effective principal through the perceptions of a sample of senior primary aged school students. The study originated due to a concern that too much of the current literature concerning effective schools and effective principals relies on the views of significant adults. Given that students are the focus of the school's and principal's energy it is difficult to understand why their views have not been sought more frequently. This study was initiated and conducted in an effort to determine what is was that students expected of the effective principal. The research is based on content analysis of the written responses from a sample of one hundred and ninety five senior primary aged school students aged between ten and twelve years from an education district in an education region of the New South Wales Public School System and in addition one to one interviews with a group of thirty students. The analysis resulted in the development of two sets of descriptors. One set of descriptors outline the fourteen most significant Behaviour Descriptors of the effective principal as perceived by the senior primary aged students surveyed while the other set outlines the eleven most significant Quality Descriptors of the effective principal. These two sets of descriptors of the effective principal have much support in the effective schools research. One area notably different however is the emphasis given by the students to the need for the principal to develop positive, warm and caring relationships with each student in the school. Although students were realistic in their understanding of what this implied they were adamant and consistent in their desire for such a relationship in order that the principal be deemed effective. The results of the study provide specific, clear, unambiguous descriptions of behaviours and qualities expected of the effective principal by the students surveyed. The descriptors are presented in a manner useful to practitioners.

This field study is the result of observations of stress and disquiet among educational administrators. Two survey instruments, one to a population of A.C.E.A. members in five states and two territories of Australia, and a refined survey to administrators in two Metropolitan West Inspectorates in N.S.W. were employed. An attempt was made to look at perceived deficits, in areas considered necessary skills for educational administrators, over variables of state, sex, age, level of institution, government/nongovernment systems, status, tenure and educational administration qualifications. From the outset it was realized that the nature of the study would have to be essentially to generate directions of future specific research since there was little Australian research in the areas being surveyed. This became more obvious as data was collected and possible causes for stress, perceived deficits, and the related poor morale multiplied with each set of comments received. The only conclusion that could be unequivocal was that the areas of administrator morale, training, selection, support, style and role perception are urgently in need of in-depth research as are the effects on educational institutions of policy processes, socio-political factors and community expectations. Even with a wider literature search it becomes obvious that there is a need for researchers to rethink theory in terms of social realities and human and socio-political possibilities rather than continue building theories which have little or no effect on the education received by an Australian student in the 1980's. It is equally evident that the solution for the obvious administrator malaise and powerlessness expressed by respondents is in their own hands via a quest for excellence in education, relevance to society and socio-political understanding.

This work is a case-study in curriculum development in secondary school science education, especially senior science, in New South Wales during the decade 1962-1972. The situation became exceptionally complex and grew out of the reorganisation of the secondary school curriculum recommended by the so-called Wyndham Committee in 1957. A completely new concept of science was offered to students of the State when biology was given increased status beside the physical sciences - physics and chemistry. This combination of material was examined in a very special way and Science (in this broad sense) was also tied administratively to mathematics. In 1966 a complicated syllabus was presented to students and teachers with negligible advance preparation of teachers, no period of familiarisation and no in-service support. Almost no explanation of the rationale behind such a novel and untried scheme was offered. The response of teachers and students was initially one of stunned silence. Very quickly this developed into hostility to the content, to its serious overloading and to the restriction of practical work. Teachers, parents and some members of the Universities expressed grave misgivings not only about the suitability of the course as a preparation for tertiary studies, but also about the completely unsatisfactory nature of the texts offered, about the examination method adopted, and about the restrictions on the personal aspirations of students for some degree of specialisation in their senior studies. The Universities became very interested in the discussions then appearing in the newspapers. Academics took sides either attacking or defending the concepts underlying the course; their points of view being based largely on the performance of the students at university level. The campaign for change began with a band of very vocal teachers working through the Teachers' Federation. These were supported by academics in promoting a series of public meetings. Parallel to this a campaign spearheaded by Professor Alexander of Sydney University was initiated in the Press. The defence of the new courses was taken up by Professors Messel and Butler of the same University. To maintain the impetus for the change in curriculum, the Secondary Schools Science Association was formed by persons interested and very involved in the curriculum. Intricately woven into the pattern of discontent with and strenuous defence of the Wyndham courses, among teachers there was a groundswell of positive aspirations towards the understanding of and clarification of the aims of science teaching in New South Wales. This resulted in the preparation of a document which contained guidelines for both teaching and curriculum development: it was subsequently adopted by the Board of Senior School Studies. This same Board was, by then, very much aware of the discontent with the new courses and various modifications of them were considered. Attempts to accommodate teacher, student and university aspirations resulted in firstly the appointment of Curriculum Development Officers to assist the Science Syllabus Committee and, parallel to this, a willingness to permit trial of science courses which had been developed for use in the United States of America and in other states of Australia. Once the decision was made in December, 1969 to permit the trialling of other courses, a Committee was set up to evaluate these courses as well as the existing Wyndham courses. This Committee reported favourably on the new courses and after some false starts the Board of Senior School Studies not only extended the trials of the new courses, but in 1975 the old Wyndham courses were abolished and superseded. Complications arising from the personalities involved, from people with vested interests in certain educational theories, from the authors of the specially published texts, from the Publishing Houses which were to provide the new texts became very tangled indeed. Similar difficulties were encountered by the Curriculum Development Officers who later directed the adoption of the new courses to a conclusion satisfactory to the Science Syllabus Committee and the Board of Senior School Studies.

The Monaro Volcanic Province (MVP) is an Oligocene-Eocene intraplate basaltic lava field situated in the Southern Highlands of New South Wales between the towns of Cooma and Bombala. The lava pile of the MVP consists of basal sub-alkali rocks (olivine tholeiite, transitional basalt) capped by a number of thick ankaramite lavas, above which lie less numerous alkali rocks including alkali olivine basalt, nepheline basanite and olivine nephelinite. Intercalated with the lava flows are massive and matrix-supported alkali and ankaramitic hyaloclastites, alkali pillow basalts, rare tuffs, bauxitic weathering profiles, lacustrine sediments and reworked late Cretaceous to early Tertiary river gravels. The lava pile is intruded through by numerous volcanic plugs and dykes and rare maars. Volcanic centres are principally concentrated in two NW-SE trending zones parallel to major crustal-scale fractures in the Palaeozoic basement. Centres almost always lie over the intersections of two or more conjugate strike-slip or transverse fractures. The stratigraphy, whole-rock geochemistry and Sr and Nd isotopic signatures of rocks from the MVP indicate magma-genesis initially from an asthenospheric source with EM1 characteristics, gradually becoming more lithospheric with DM source characteristics. The long-lived nature of the MVP rules out a mantle plume-type source for magmas. Instead, a diapiric source is envisaged. The MVP mantle xenolith suite appears to have equilibrated at slightly higher temperatures for given pressures than the Newer Volcanics Province suite suggesting the palaeogeotherm for the MVP was slightly hotter than the "South East Australian" geotherm. Large amounts of amphibole (pargasitic hornblende, pargasite, ferroan pargasite and kaersutite) occuring within the more silica-undersaturated rocks of the MVP, and rarely within Iherzolitic xenoliths, are interpreted to have formed as selvages on mantle veins in contact with peridotite beneath the MVP. Amphiboles were later sampled by magmas rising through the same conduits and were brought to the surface. MVP ankaramite lavas feature < 2cm clinopyroxene porphyrocrysts, the cores of which are shown to have crystallised at ca. 18 kb pressure or ca. 54 km depth. This defines the base of the local crust within the MVP region. Data from the MVP support a landscape evolution model based on the isostatic rise of the Southern Highlands due to voluminous magmatic underplating since the Cretaceous. Data further support limited denudation since the Early Tertiary based on a pulsatory but high palaeogeotherm.

A study of the nature of entrepreneurial activity and its use in furthering our understanding of small business establishment. An ethnographic study is presented of the business perspectives of a group of business entrepreneurs in the Riverina region of N.S.W. and a conceptual framework is developed for consideration of various qualitative issues involved in establishing a small business.