School of Agriculture, Food and Ecosystem Sciences - Theses
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ItemSalinity control, water reform and structural adjustment : the Tragowel Plains Irrigation District(University of Melbourne, 1999)
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ItemNo Preview AvailableEpidemiology of mint rust and variation in the Pathogen, Puccinia menthae Pers(University of Melbourne, 1998)
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ItemNo Preview AvailableGenetics of resistance to Heterodera avenae in Triticum tauschii and its transfer to bread wheat (Triticum aestivum)(University of Melbourne, 1995)
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ItemNo Preview AvailableSurvey of the sheep industry in the Western District of Victoria(University of Melbourne, School of Agriculture, 1952?)
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ItemNo Preview AvailableThe role of diffused carbohydrates in the infection of stone fruit by Sclerotinia fructicola (Wint.) rehm(University of Melbourne, 1970)
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ItemSunraysia : a social survey of a dried fruits area(University of Melbourne, 1948)
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ItemNo Preview AvailableObservations on fomes pomaceus (pers.) big. & guill. infecting plum trees ; An investigation of sooty moulds with particular reference to their taxonomy and their growth in culture(University of Melbourne, 1974)I. The Taxonomy of "Sooty Mould "-Fungi. 1. Existing schemes of classification are discussed. 2. A classification is offered in which, the inaccuracies of other taxonomic schemas, are corrected. 3. "Sooty Moulds� are arranged, according to the macroscopic appearance of their growth, into four groups. 4. Diagnostic features are given for five families of ��sooty mould"-genera. 5. The families Capnodiaceae v. Hohn. and Chaetothyriaceae Th. are emended. A key to the identification of the genera Included in each of these families Is given. 6. Chaetothyrium Citri (Arn.) nov. comb. is recorded for the first time in Australia. 7. A new species, Phycopsis australiensis is described. II. An Instigation of the Cultural Behaviour of some "Sooty Mould" Fungi with reference to Climatic Conditions. 1. Eight species which, were isolated from epiphytic moulds, are included in this study. 2. A preliminary survey is made of the nutritional recuirementa of these species. 3. The methods used for recording measurements of colony-size and for calculating the rate of growth are described. 4. Measurement is made of the growth occurring at the following temperatures: 10�C., 15�C., 18�C., 20�C. and 25�C. The optimum growth temperatures determined for seven "sooty mould" endemics lie between 15�C and 20�C. 5. The methods which were adopted for growing these fungi under conditions of controlled atmospheric humidity are described. 6. The humidity growth-rate relations determined here are similar to those of fungi from quite unrelated habitats. 7. The geographic distribution of epiphytic "sooty moulds" is discussed in relation to the temperature and humidity requirements of the species examined here. The temperature-growth relations of the Capnodiaceae species do not confirm the assumption that high temperatures are favourable, rather It would appear that growth is active during the winter months. 8. It la suggested that the deciduous nature of the flora in cool temperate regions is responsible for the almost entire absence of the Capnodiaceae in these regions.
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ItemNo Preview AvailableSelected papers(University of Melbourne, 1972)These selected papers are submitted for examination for the degree of Doctor of Agricultural Science bearing in mind the need to demonstrate that they should constitute - (i) "Substantial published contributions to science applied to some branch of agriculture"; (ii) "Evidence of research and ability satisfactory to the examiners". To this end the papers have been grouped in the following manner. Group I - Papers which collectively provide evidence of the evolution and development of principles and methods for studying land to provide the ecological information needed to determine its capability for various kinds of land-use and so enable better decisions to achieve conservation of natural resources. 1. Soil, land-use and erosion survey around Dookie, Victoria. CSIRO Bull. No. 243, 1949. 2. Soils of the Macquarie Region N.:. . CSIRO Soil Publication No. 4, 1955. 3. Principles and methods of ecological surveys for land-use purposes. Papers for Australian Soils Conference, 1957. 4. Reconnaissance survey of the ecology and land-use in the catchment of the Glenmaggie Reservoir. Soil Conservation Authority Tech. Pubn. No. 1, 1960. 5. A study of the land in north-western Victoria. Soil. Cons. Auth. Tech. Pubn. No. 2, 1963. 6. A study of the land in south-western Victoria. Soil Cons. Auth. Tech. Pubn. No. 3, 1964. 7. The role of humans in land evaluation. CSIRO-UNESCO Symposium on Land Evaluation, Canberra, 1968. Group II - Papers that report results of original research as evidence of contributions to scientific knowledge and its significance as the basis for work by others. 8. The use of the hydrometer for the mechanical analysis of soils. Journ. CSIR Vol. 17, 1944. 9. Tunnelling erosion in north-eastern Victoria. Journ. CSIR Vol. 19, 1946. 10. Studies in the variation of soil reaction - I Field variations at Barooga N.S.W Aust. Journ. Agric. Res. Vol. 2, 1951. 11. Cyclic salt as a dominant factor in the genesis of soils in south-eastern Australia. Aust. Journ. Agric. Res. Vol. 5, 19514. 12. The effect of subterranean clover an Wimmera rye grass in controlling surface run-off from four-acre catchments near Bacchus Marsh, Victoria. Aust. Journ. Exp. Agric. & An. Husb. Vol. 2, 1962. Group III - Papers which indicate the application of a conceptual philosophy of conservation based on ecological principles to tae solution of problems of land-use, soil conservation and agriculture. 13. The Westgate Planning Project. Soil Cons. Auth. Pubn. 1953. 14. Conservation problems on solodic soils in Victoria. Journ. Soil & Water Cons. (USA), Vol. 11, 1956. 15. Land management problems following disturbance of the hydrologic balance of environments in Victoria. Proc. 7th Tech. Meeting IUCN, Athens. 1958. 16. Soil salinity in non-irrigated arable and pastoral land as the result of unbalance of the hydrologic cycle. Proc. UNESCO-Arid hone Symposium on Salinity Problems, Teheran, 1958. 17. The ecology and prevention of soil erosion. Chapter XXX - Biogeography and ecology in Australia. Publishers Junk - The Hague, 1959. 18. The water balance and land-use. Proc. Aust. Acad. Sci. Nat. Symposium on Water Resources, Use & Management. Melb. Univ. Press, 1963. 19. The rehabilitation of degraded land for agricultural and pastoral production. ANZAAS, Canberra, 1964. 20. The correlation of failure of earthen dams with environmental features - Colloquium on Failure of Small Earth. Dams - CSIRO, , 1964. 21. Agrometeorology in relation to the control of soil erosion - United Nations .O. Regional Seminar on Agrorneteorology. Melb., 1966. 22. Dryland farming - principles of applying conservation methods in Australia. T roc. Int. Lech. Dryland Farmg. Conf. - Deere Co. and. F.A.C., oline USA, 1969. Group IV - Papers which collectively demonstrate the extension of the conceptual philosophy of conservation as applied to soil conservation and agricultural problems to those related to tie conservation of all natural resources and its application as a basis for influencing social, political, legal and administrative activities in relation to them. 23. The Victorian High plains - The environment and its use. Proc. Roy. Soc. Vict. Vol. 75, 1962. 24. Soil conservation - ho is responsible? - from Coil conservation in the Pacific - Tenth Pacific Science Congress Series, University of Hawaii Press, 1963. 25. Conservation and the community. Journ. Soil & Water Cons. (USA) Vol. 20, 1965, 26. Nature reserves and National larks in relation to the conservation of man's environment. Aust. Journ. Sci. Vol. 30 196', 27. The conflict between conservation and exploitation of natural resources - Paper to ANZAAS Regional Symposium on The planning and management of Australia's natural resources. Univ. New England, 1967. 28. Soil conservation in Iran - Consultant report to F.A.O., 1967. 29. Resources of East Gippsland - Summary of Symposium - Proc. Roy. Soc. Vict. Vol. 82, 1969. 30. Soil Conservation Law in Australia - Soil. Cons. Authority Pubn., 1970. 31. Criteria for resolving conflict about land-use - Aust. Cons. Found. Seminar on Conservation & Wining, Syd. 1971. 32. Management of conservation reserves - ANZAAS Symposium, Brisbane, 1971.
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ItemNo Preview AvailableNitrogen dynamics after application of biosolids to a Pinus radiata plantation(University of Melbourne, 1999)The application of biosolids (sewage sludge) to forests has the potential to increase plantation productivity. Environmental damage may result from pollution of nutrients, heavy metals or pathogens contained in biosolids, leaching of nitrogen (N) to groundwater is of particular concern. This thesis examines the rate of release of N from biosolids, its subsequent fate, and those factors controlling storage and loss of N. Integral to the release of N is the decomposition of biosolids, which is examined through the loss of mass, organic matter and carbon. The potential for increased productivity and environmental risk is assessed through comprehensive N budgeting in the ecosystem. The objectives were addressed through a series of field and laboratory experiments. To compare N dynamics, biosolids were obtained from three sewage treatment plants with contrasting processes (one aerobically- and two anaerobically-digested). The core work was carried out in a major field trial, where biosolids were applied to the forest floor of a 22 year-old Pinus radiata D. Don plantation. The experimental rate of application supplied between 965 and 1425 kg ha-1 of N. More than 85% of the NH4+-N applied in biosolids was volatilised in the first three weeks after application. Subsequent rates of volatilisation were small. The magnitude and temporal patterns were confirmed in a separate study. Volatilisation losses reported in the literature are generally much less, highlighting the variability of losses due to differing biosolids chemistry and environmental conditions at application. About 35% of the organic N was released from anaerobically-digested biosolids in the first year after application, and 54% from the aerobically-digested biosolids. These rates are considerably higher than those used in guidelines of the NSW Environment Protection Authority. There were no significant increases in total N in soil after application, but natural variability in soil precluded detection of increases of the order of 100 kg ha-1. Amounts of NH4+-N in soil increased immediately after application, the size and longevity of increases differing among biosolids. One year after application only very small amounts of inorganic N remained in soil. Throughout the trial, concentrations of NO3--N in soil solution at 60 cm in soil remained consistently below drinking water standards under the anaerobically-digested biosolids and consistently exceeded drinking water standards under the aerobically-digested biosolids. Loss of N in drainage below 60 cm depth in soil in the first year after application was about 20 kg ha-1 under anaerobically-digested biosolids and about 100 kg ha-1 under aerobically-digested biosolids. A controlled incubation study demonstrated that patterns of N mineralisation in the field could not be predicted from laboratory incubations. However relative rates of N mineralisation correlated with amounts of N leached in drainage. Application of biosolids significantly increased tree growth (20 - 34% in basal area) by the second growing season after application. Such a response is likely to be maintained for several years. Rates of volatilisation and mineralisation need to be considered when determining rates of application to ensure that the capacity of soil and plants to store N is not exceeded. Application of anaerobically-digested biosolids at 30 dt ha-1 can increase plantation productivity with minimal risk of groundwater contamination by N. Repeat applications at the same rate concomitant with plantation thinning operations should improve productivity and soil fertility with minimal risk of groundwater contamination.
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ItemNo Preview AvailableNitrogen dynamics after application of biosolids to a Pinus radiata plantation(University of Melbourne, 1999)The application of biosolids (sewage sludge) to forests has the potential to increase plantation productivity. Environmental damage may result from pollution of nutrients, heavy metals or pathogens contained in biosolids, leaching of nitrogen (N) to groundwater is of particular concern. This thesis examines the rate of release of N from biosolids, its subsequent fate, and those factors controlling storage and loss of N. Integral to the release of N is the decomposition of biosolids, which is examined through the loss of mass, organic matter and carbon. The potential for increased productivity and environmental risk is assessed through comprehensive N budgeting in the ecosystem. The objectives were addressed through a series of field and laboratory experiments. To compare N dynamics, biosolids were obtained from three sewage treatment plants with contrasting processes (one aerobically- and two anaerobically-digested). The core work was carried out in a major field trial, where biosolids were applied to the forest floor of a 22 year-old Pinus radiata D. Don plantation. The experimental rate of application supplied between 965 and 1425 kg ha-1 of N. More than 85% of the NH4+-N applied in biosolids was volatilised in the first three weeks after application. Subsequent rates of volatilisation were small. The magnitude and temporal patterns were confirmed in a separate study. Volatilisation losses reported in the literature are generally much less, highlighting the variability of losses due to differing biosolids chemistry and environmental conditions at application. About 35% of the organic N was released from anaerobically-digested biosolids in the first year after application, and 54% from the aerobically-digested biosolids. These rates are considerably higher than those used in guidelines of the NSW Environment Protection Authority. There were no significant increases in total N in soil after application, but natural variability in soil precluded detection of increases of the order of 100 kg ha-1. Amounts of NH4+-N in soil increased immediately after application, the size and longevity of increases differing among biosolids. One year after application only very small amounts of inorganic N remained in soil. Throughout the trial, concentrations of NO3--N in soil solution at 60 cm in soil remained consistently below drinking water standards under the anaerobically-digested biosolids and consistently exceeded drinking water standards under the aerobically-digested biosolids. Loss of N in drainage below 60 cm depth in soil in the first year after application was about 20 kg ha-1 under anaerobically-digested biosolids and about 100 kg ha-1 under aerobically-digested biosolids. A controlled incubation study demonstrated that patterns of N mineralisation in the field could not be predicted from laboratory incubations. However relative rates of N mineralisation correlated with amounts of N leached in drainage. Application of biosolids significantly increased tree growth (20 - 34% in basal area) by the second growing season after application. Such a response is likely to be maintained for several years. Rates of volatilisation and mineralisation need to be considered when determining rates of application to ensure that the capacity of soil and plants to store N is not exceeded. Application of anaerobically-digested biosolids at 30 dt ha-1 can increase plantation productivity with minimal risk of groundwater contamination by N. Repeat applications at the same rate concomitant with plantation thinning operations should improve productivity and soil fertility with minimal risk of groundwater contamination.