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1

Baker, G. H., P. J. Carter, and V. J. Barrett. "Survival and biomass of exotic earthworms, Aporrectodea spp. (Lumbricidae), when introduced to pastures in south-eastern Australia." Australian Journal of Agricultural Research 50, no. 7 (1999): 1233. http://dx.doi.org/10.1071/ar98181.

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The earthworm fauna of pastures in south-eastern Australia is dominated by exotic lumbricid earthworms, in particular the endogeic species, Aporrectodea caliginosa and A. trapezoides. Anecic species such as A. longa are very rare. All 3 species were introduced within cages in 10 pastures on a range of soil types within the region. Five months later, A. longa had generally survived the best and A. trapezoides the worst. The survivals and weights of individual worms varied between sites for all 3 species. The survivals of A. caliginosa and A. longa, and to a lesser extent A. trapezoides, were po
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2

Luck, Joanne E., Rosa Crnov, Barbara Czerniakowski, Ian W. Smith, and Jane R. Moran. "Investigating the Presence of Biotic Agents Associated with Mundulla Yellows." Plant Disease 90, no. 4 (April 2006): 404–10. http://dx.doi.org/10.1094/pd-90-0404.

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The role of biotic agents in the dieback syndrome Mundulla Yellows (MY) was investigated by analysis of 40 Eucalyptus camaldulensis, E. leucoxylon, or E. cladocalyx trees and soil samples from South Australia and Victoria, Australia. No pathogenic fungi, bacteria, phytoplasmas, or insect pests or vectors were found to be associated with MY. However, nematode analysis identified Merlinius spp. to be associated with soil, but not roots, from symptomatic trees. Interveinal chlorosis symptoms were not transmissible by seed, mechanical inoculation, or grafting using plant material derived from symp
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3

Pickering, Bianca J., Jamie E. Burton, Trent D. Penman, Madeleine A. Grant, and Jane G. Cawson. "Long-Term Response of Fuel to Mechanical Mastication in South-Eastern Australia." Fire 5, no. 3 (June 3, 2022): 76. http://dx.doi.org/10.3390/fire5030076.

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Mechanical mastication is a fuel management strategy that modifies vegetation structure to reduce the impact of wildfire. Although past research has quantified immediate changes to fuel post-mastication, few studies consider longer-term fuel trajectories and climatic drivers of this change. Our study sought to quantify changes to fuel loads and structure over time following mastication and as a function of landscape aridity. Measurements were made at 63 sites in Victoria, Australia. All sites had been masticated within the previous 9 years to remove over-abundant shrubs and small trees. We use
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4

Crombie, DS, JT Tippett, and TC Hill. "Dawn Water Potential and Root Depth of Trees and Understorey Species in Southwestern Australia." Australian Journal of Botany 36, no. 6 (1988): 621. http://dx.doi.org/10.1071/bt9880621.

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Water relations of selected tree and understorey species in the jarrah forest of south-western Australia were studied during summer drought and the results related to root morphology. Seasonal patterns of predawn water potential (Ψp) differed between species according to root depth and between sites according to average annual rainfall. Dawn water potentials fell most rapidly and by the greatest amount in plants with the shallowest roots. Dawn water potentials of medium and deep rooted species were not consistently different. Separation of Ψp between sites of different annual rainfall was less
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5

Abdallah, Ahmed M., Hanuman S. Jat, Madhu Choudhary, Emad F. Abdelaty, Parbodh C. Sharma, and Mangi L. Jat. "Conservation Agriculture Effects on Soil Water Holding Capacity and Water-Saving Varied with Management Practices and Agroecological Conditions: A Review." Agronomy 11, no. 9 (August 24, 2021): 1681. http://dx.doi.org/10.3390/agronomy11091681.

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Improving soil water holding capacity (WHC) through conservation agriculture (CA)-practices, i.e., minimum mechanical soil disturbance, crop diversification, and soil mulch cover/crop residue retention, could buffer soil resilience against climate change. CA-practices could increase soil organic carbon (SOC) and alter pore size distribution (PSD); thus, they could improve soil WHC. This paper aims to review to what extent CA-practices can influence soil WHC and water-availability through SOC build-up and the change of the PSD. In general, the sequestered SOC due to the adoption of CA does not
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6

Jettner, R., S. P. Loss, L. D. Martin, and K. H. M. Siddique. "Responses of faba bean (Vicia faba L.) to sowing rate in south-western Australia II Canopy development, radiation absorption and dry matter partitioning." Australian Journal of Agricultural Research 49, no. 6 (1998): 999. http://dx.doi.org/10.1071/a98003.

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Sowing rate influences plant density, canopy development, radiation absorption, dry matter production and its partitioning, and seed yield. The canopy development, radiation interception, and dry matter partitioning of faba bean (cv. Fiord) were examined using 6 sowing rate treatments from 70 to 270 kg/ha in field experiments conducted over 3 years at Northam as part of a larger investigation of sowing rate responses in faba bean in south-western Australia. High sowing rates resulted in significantly earlier canopy closure, larger green area indexes, more radiation absorption, more dry matter
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7

Regan, K. L., K. H. M. Siddique, and L. D. Martin. "Response of kabuli chickpea (Cicer arietinum L.) to sowing rate in Mediterranean-type environments of south-western Australia." Australian Journal of Experimental Agriculture 43, no. 1 (2003): 87. http://dx.doi.org/10.1071/ea01200.

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The effect of sowing rate (60–320 kg/ha) on the growth and seed yield of kabuli chickpea (cv. Kaniva) was assessed at 11 sites for 4 seasons in the cropping regions of south-western Australia. The economic optimum plant density and yield potential were estimated using an asymptotic model fitted to the data and calculating the sowing rate above which the cost of additional seed was equivalent to the revenue that could be achieved from the extra seed yield produced, assuming a 10 and 50% opportunity cost. On average for all sites and seasons, plant densities ranged from 10 plants/m2 when sown at
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8

SINGH, B., and R. J. GILKES. "Properties of soil kaolinites from south-western Australia." Journal of Soil Science 43, no. 4 (December 1992): 645–67. http://dx.doi.org/10.1111/j.1365-2389.1992.tb00165.x.

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9

Aldaoud, R., W. Guppy, L. Callinan, S. F. Flett, K. A. Wratten, G. A. Murray, T. Cook, and A. McAllister. "Occurrence of Phytophthora clandestina in Trifolium subterraneum paddocks in Australia." Australian Journal of Experimental Agriculture 41, no. 2 (2001): 187. http://dx.doi.org/10.1071/ea00048.

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In 1995–96, a survey of soil samples from subterranean clover (Trifolium subterraneum L.) paddocks was conducted across Victoria, South Australia, New South Wales and Western Australia, to determine the distribution and the prevalence of races of Phytophthora clandestina (as determined by the development of root rot on differential cultivars), and the association of its occurrence with paddock variables. In all states, there was a weak but significant association between P. clandestina detected in soil samples and subsequent root rot susceptibility of differential cultivars grown in these soil
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10

St. Pierre, Tim G. "Mössbauer Spectra of Soil Kaolins from South-Western Australia." Clays and Clay Minerals 40, no. 3 (1992): 341–46. http://dx.doi.org/10.1346/ccmn.1992.0400315.

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11

Doran-Browne, Natalie A., John Ive, Phillip Graham, and Richard J. Eckard. "Carbon-neutral wool farming in south-eastern Australia." Animal Production Science 56, no. 3 (2016): 417. http://dx.doi.org/10.1071/an15541.

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Ruminant livestock production generates higher levels of greenhouse gas emissions (GHGE) compared with other types of farming. Therefore, it is desirable to reduce or offset those emissions where possible. Although mitigation options exist that reduce ruminant GHGE through the use of feed management, flock structure or breeding management, these options only reduce the existing emissions by up to 30% whereas planting trees and subsequent carbon sequestration in trees and soil has the potential for livestock emissions to be offset in their entirety. Trees can introduce additional co-benefits th
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12

Ward, S. C. "Soil development on rehabilitated bauxite mines in south-west Australia." Soil Research 38, no. 2 (2000): 453. http://dx.doi.org/10.1071/sr99032.

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Rehabilitation after bauxite mining in the jarrah forest aims to re-establish a self-sustaining forest. This implies that ecosystem processes will be re-established and soil nutrient stores will be similar to those of the unmined forest. This study determined the baseline levels of a number of soil properties in areas of jarrah forest typically cleared and mined for bauxite, and the effect of mining and rehabilitation processes on the vertical distribution of soil nitrogen. In addition, the changes in soil nitrogen, extractable phosphorus, extractable potassium, and pH that occurred up to 8.5
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13

Cock, GJ. "Moisture characteristics of irrigated Mallee soils in South Australia." Australian Journal of Experimental Agriculture 25, no. 1 (1985): 209. http://dx.doi.org/10.1071/ea9850209.

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The soil moisture characteristics of undisturbed samples of Mallee soils, taken from typical profiles of the Riverland district neat Berri in South Australia, were determined. Samples were grouped according to texture and bulk density and, for each group, the moisture storage between matric potentials was derived. Over the usual range of soil moisture tensions (-0 to 40kPa) these showed only small variation between soil groups since, while moisture storage at field capacity and at wilting point does vary with texture; 50 to 60 mm/m is available between field capacity (-7 kPa) and the re-irriga
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14

Radke, J. K., A. R. Dexter, and O. J. Devine. "Tillage Effects on Soil Temperature, Soil Water, and Wheat Growth in South Australia." Soil Science Society of America Journal 49, no. 6 (November 1985): 1542–47. http://dx.doi.org/10.2136/sssaj1985.03615995004900060042x.

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15

Gardner, WK, RG Fawcett, GR Steed, JE Pratley, DM Whitfield, Hvan Rees, and Rees H. Van. "Crop production on duplex soils in south-eastern Australia." Australian Journal of Experimental Agriculture 32, no. 7 (1992): 915. http://dx.doi.org/10.1071/ea9920915.

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The environment, duplex soil types and trends in crop production in South Australia, southern New South Wales, north-eastern and north-central Victoria, the southern Wimmera and the Victorian Western District are reviewed. In the latter 2 regions, pastoral industries dominate and crop production is curtailed by regular and severe soil waterlogging, except for limited areas of lower rainfall. Subsurface drainage can eliminate waterlogging, but is feasible only for the Western District where subsoils are sufficiently stable. The other regions all have a long history of soil degradation due to cr
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16

Harper, R. J., R. J. Gilkes, M. J. Hill, and D. J. Carter. "Wind erosion and soil carbon dynamics in south-western Australia." Aeolian Research 1, no. 3-4 (January 2010): 129–41. http://dx.doi.org/10.1016/j.aeolia.2009.10.003.

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17

FOULDS, W. "Nutrient concentrations of foliage and soil in South-western Australia." New Phytologist 125, no. 3 (November 1993): 529–46. http://dx.doi.org/10.1111/j.1469-8137.1993.tb03901.x.

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18

Naidu, R., RH Merry, GJ Churchman, MJ Wright, RS Murray, RW Fitzpatrick, and BA Zarcinas. "Sodicity in South Australia - a review." Soil Research 31, no. 6 (1993): 911. http://dx.doi.org/10.1071/sr9930911.

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The current knowledge of the nature and distribution of sodic soils in South Australia is reviewed. The agriculturally developed area of South Australia lies south of latitude 32-degrees-S. and is mainly used for low intensity grazing and dry land cereal/sheep production. A high proportion of the State, including much of the high rainfall area, has soils which are sodic (>6% ESP) through a significant proportion of the profile but information on the precise nature of sodicity in these soils is limited. Where exchangeable cation data axe available, the analytical techniques used often did no
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19

Webb, Ashley A., Georgina L. Kelly, and Warwick J. Dougherty. "Soil governance in the agricultural landscapes of New South Wales, Australia." International Journal of Rural Law and Policy, no. 1 (March 29, 2015): 1–16. http://dx.doi.org/10.5130/ijrlp.i1.2015.4169.

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Soil is a valuable natural resource. In the state of New South Wales, Australia, the governance of soil has evolved since Federation in 1901. Following rapid agricultural development, and in the face of widespread soil degradation, the establishment of the Soil Conservation Service marked a turning point in the management of soil. Throughout the 20th century, advances in knowledge were translated into evolving governance frameworks that were largely reactionary but saw progressive reforms such as water pollution legislation and case studies of catchment-scale land and vegetation management. In
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20

Angus, J. F., A. F. van Herwaarden, D. P. Heenan, R. A. Fischer, and G. N. Howe. "The source of mineral nitrogen for cereals in south-eastern Australia." Australian Journal of Agricultural Research 49, no. 3 (1998): 511. http://dx.doi.org/10.1071/a97125.

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The relative importance of soil mineral nitrogen (N) available at the time of sowing ormineralised during the growing season was investigated for 6 crops of dryland wheat. The soil mineral N in the root-zone was sampled at sowing and maturity and the rate of net mineralisation in the top 10 cm was estimated by sequential sampling throughout the growing season, using an in situ method. Mineralisation during crop growth was modelled in relation to total soil N, ambient temperature, andsoil water content. Mineral N accumulated before sowing varied by a factor of 3 between the sites (from 67 to 19
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21

Yang, Xihua, Jonathan Gray, Greg Chapman, Qinggaozi Zhu, Mitch Tulau, and Sally McInnes-Clarke. "Digital mapping of soil erodibility for water erosion in New South Wales, Australia." Soil Research 56, no. 2 (2018): 158. http://dx.doi.org/10.1071/sr17058.

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Soil erodibility represents the soil’s response to rainfall and run-off erosivity and is related to soil properties such as organic matter content, texture, structure, permeability and aggregate stability. Soil erodibility is an important factor in soil erosion modelling, such as the Revised Universal Soil Loss Equation (RUSLE), in which it is represented by the soil erodibility factor (K-factor). However, determination of soil erodibility at larger spatial scales is often problematic because of the lack of spatial data on soil properties and field measurements for model validation. Recently,
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22

Unkovich, Murray, Therese McBeath, Rick Llewellyn, James Hall, Vadakattu VSR Gupta, and Lynne M. Macdonald. "Challenges and opportunities for grain farming on sandy soils of semi-arid south and south-eastern Australia." Soil Research 58, no. 4 (2020): 323. http://dx.doi.org/10.1071/sr19161.

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Sandy soils make up a substantial fraction of cropping land in low rainfall (<450 mm p.a.) south and south-eastern Australia. In this paper we review the possible soil constraints to increased production on these soils in this region. Many of these soils have a very low (<3%) clay content and suffer from severe water repellency, making crop establishment and weed control problematic. Crops which do emerge are faced with uneven soil wetting and poor access to nutrients, with crop nutrition constraints exacerbated by low fertility (soil organic matter < 1%) and low cation ex
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23

Hopmans, P., N. Collett, and R. Bickford. "Effects of fire retardant on heathland soils in south-eastern Australia." Soil Research 45, no. 8 (2007): 607. http://dx.doi.org/10.1071/sr07040.

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A study was undertaken to assess the effects of fire retardant application, unmodified by heat of fire, on soil properties in 2 fire-prone heathland communities at Marlo and the Grampians in south-eastern Australia. Fire retardant (Phos-Chek D75-R at 0.144 g/L) was applied at rates of 0.5, 1.0, and 1.5 L/m2 and compared with control treatments of nil and 1.0 L/m2 of water. Monitoring of surface soils showed that pH at both sites decreased while soil salinity increased immediately after application followed by a rapid decline to pre-treatment values within 12 months. The impact of retardant on
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24

Hopmans, Peter. "Stem deformity inPinus radiata plantations in south-eastern Australia:." Plant and Soil 122, no. 1 (February 1990): 97–104. http://dx.doi.org/10.1007/bf02851915.

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25

Hopmans, Peter, Matt Kitching, and George Croatto. "Stem deformity inPinus radiata plantations in south-eastern Australia." Plant and Soil 175, no. 1 (August 1995): 31–44. http://dx.doi.org/10.1007/bf02413008.

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26

Fisher, JM, and TW Hancock. "Population dynamics of Heterodera avenae Woll. in South Australia." Australian Journal of Agricultural Research 42, no. 1 (1991): 53. http://dx.doi.org/10.1071/ar9910053.

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Population changes of the cereal cyst nematode (Heterodera avenae Woll.) under various rotational regimes in the field were examined. A density of 5 eggs/g soils caused a loss of about 10% in yield of wheat cv. Bayonet under the experimental conditions. Maximum multiplication rate at low initial densities was about l0x, but this rapidly decreased as initial density increased. Equilibrium levels ranged from 15 eggs/g soil up to 40 eggs/g under different conditions. The resistant wheat, Aus 10894, maintained an equilibrium level of about 1 egg/g soil-a level low enough to avoid damage in a follo
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27

Barrett-Lennard, Edward G., Geoffrey C. Anderson, Karen W. Holmes, and Aidan Sinnott. "High soil sodicity and alkalinity cause transient salinity in south-western Australia." Soil Research 54, no. 4 (2016): 407. http://dx.doi.org/10.1071/sr15052.

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Transient salinity associated with increased dispersion of clays is arguably one of the most economically important soil constraints in Australia because it occurs on land that is regularly cropped. However, this issue is rarely studied. This paper examines the occurrence of transient salinity on agricultural land in the south-west of Western Australia and the factors causing it. We analysed four soil datasets from the region, collected at scales varying from the entire south-west to a single paddock. A variety of soil parameters were correlated with increased electrical conductivity (EC1:5).
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28

Wang, T. H., Y. T. Tchan, A. M. M. Zeman, and I. R. Kennedy. "Presence of sodium dependent azotobacter in Australia (New South Wales)." Soil Biology and Biochemistry 25, no. 5 (May 1993): 637–39. http://dx.doi.org/10.1016/0038-0717(93)90205-p.

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29

Nash, David, Craig Butler, Justine Cody, Michael St J. Warne, Mike J. McLaughlin, Dianne Heemsbergen, Kris Broos, et al. "Effects of Biosolids Application on Pasture and Grape Vines in South-Eastern Australia." Applied and Environmental Soil Science 2011 (2011): 1–11. http://dx.doi.org/10.1155/2011/342916.

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Biosolids were applied to a pasture and a vineyard in south-eastern Australia. At both sites, soil Cd, Cu, and Zn concentrations linearly increased with biosolids application rates although not to the extent of exceeding soil quality guidelines. Biosolids marginally increased soil C and N concentrations at the pasture site but significantly increased P concentrations. With lower overall soil fertility at the vineyard, biosolids increased C, N, and P concentrations. At neither site did biosolids application affect soil microbial endpoints. Biosolids increased pasture production compared to the
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30

Benyon, Richard G., S. Theiveyanathan, and Tanya M. Doody. "Impacts of tree plantations on groundwater in south-eastern Australia." Australian Journal of Botany 54, no. 2 (2006): 181. http://dx.doi.org/10.1071/bt05046.

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In some regions dependent on groundwater, such as the lower south-east of South Australia in the Green Triangle, deep-rooted, woody vegetation might have undesirable hydrological impacts by competing for finite, good-quality groundwater resources. In other regions, such as the Riverina in south-central New South Wales, where rising watertables and associated salinisation is threatening the viability of agriculture, woody vegetation might have beneficial hydrological impacts. In response to a growing need to better understand the impacts of tree plantations on groundwater, annual evapotranspira
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31

Grimes, K. G. "The South-East Karst Province of South Australia." Environmental Geology 23, no. 2 (March 1994): 134–48. http://dx.doi.org/10.1007/bf00766987.

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32

McFarlane, JD, GJ Judson, and J. Gouzos. "Copper deficiency in ruminants in the South East of South Australia." Australian Journal of Experimental Agriculture 30, no. 2 (1990): 187. http://dx.doi.org/10.1071/ea9900187.

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Pasture development in the South East of South Australia has depended upon trace element enriched fertiliser applications. Despite the wide usage of copper-enriched fertilisers, copper deficiency is still evident in livestock at pasture, particularly cattle. Serum collected from cows and heifers during the systematic sampling program of the Brucellosis and Tuberculosis Eradication Scheme was analysed for copper. Of the 3611 pooled herd samples analysed, approximately 9% had low serum copper concentrations (<7 �mol/L). Distribution of those herds identified to be at risk of copper deficiency
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33

Reuter, DJ, CB Dyson, DE Elliott, DC Lewis, and CL Rudd. "An appraisal of soil phosphorus testing data for crops and pastures in South Australia." Australian Journal of Experimental Agriculture 35, no. 7 (1995): 979. http://dx.doi.org/10.1071/ea9950979.

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Data from more than 580 field experiments conducted in South Australia over the past 30 years have been re-examined to estimate extractable soil phosphorus (P) levels related to 90% maximum yield (C90) for 7 crop species (wheat, barley, oilseed rape, sunflower, field peas, faba beans, potato) and 3 types of legume-based pasture (subterranean clover, strawberry clover, annual medics). Data from both single-year and longer term experiments were evaluated. The C90 value for each species was derived from the relationship between proportional yield responsiveness to applied P fertiliser rates (dete
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34

Baker, G. H., P. J. Carter, and V. J. Barrett. "Influence of earthworms, Aporrectodea spp. (Lumbricidae), on lime burial in pasture soils in south-eastern Australia." Soil Research 37, no. 5 (1999): 831. http://dx.doi.org/10.1071/sr98106.

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The relative abilities of 3 exotic lumbricid earthworms, the endogeic Aporrectodea caliginosa and A. trapezoides and the anecic A. longa, to bury surface-applied lime and help ameliorate soil acidity were measured in cages in 7 pasture soils in south-eastern Australia. All 3 species buried lime, mostly within the top 5 cm of the soil profile, but A. longa buried it deeper than A. caliginosa and A. trapezoides. A. longa significantly increased soil pH at 15–20 cm depth at some sites within 5 months (winter–spring, the earthworm ‘season’ in the Mediterranean climate of south-eastern Australia).
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35

Coventry, D. R., W. J. Slattery, V. F. Burnett, and G. W. Ganning. "Longevity of wheat yield response to lime in south-eastern Australia." Australian Journal of Experimental Agriculture 37, no. 5 (1997): 571. http://dx.doi.org/10.1071/ea96146.

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Summary. A long-term experiment in north-eastern Victoria has been regularly monitored for wheat yield responses to a range of lime and fertiliser treatments, and the soil sampled for acidity attributes. Substantial grain yield increases have been consistently obtained over a period of 12 years with a single lime application. Lime applied at 2.5 t/ha in 1980 was still providing yield increases of 24% with an acid-tolerant wheat (Matong, 1992 season) and 79% with an acid-sensitive wheat (Oxley, 1993 season) relative to no lime treatment. The 2 wheat cultivars responded differently to phosphorus
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36

Gray, Jonathan, Senani Karunaratne, Thomas Bishop, Brian Wilson, and Manoharan Veeragathipillai. "Driving factors of soil organic carbon fractions over New South Wales, Australia." Geoderma 353 (November 2019): 213–26. http://dx.doi.org/10.1016/j.geoderma.2019.06.032.

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37

Bakker, Derk, Grey Poulish, and Stephen Davies. "Water repellence and productivity of lateritic gravelly podosols in South West Australia." Geoderma Regional 17 (June 2019): e00223. http://dx.doi.org/10.1016/j.geodrs.2019.e00223.

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38

Standish, Rachel J., and Richard J. Hobbs. "Restoration of OCBILs in south-western Australia: Response to Hopper." Plant and Soil 330, no. 1-2 (October 9, 2009): 15–18. http://dx.doi.org/10.1007/s11104-009-0182-z.

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39

Lau, I., and M. Verrall. "Acid sulphate soil mapping with hyperspectral imagery at South Yunderup, Western Australia." ASEG Extended Abstracts 2009, no. 1 (2009): 1. http://dx.doi.org/10.1071/aseg2009ab100.

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40

Brooker, Peter I. "Modelling spatial variability using soil profiles in the Riverland of South Australia." Environment International 27, no. 2-3 (September 2001): 121–26. http://dx.doi.org/10.1016/s0160-4120(01)00071-x.

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41

Tighe, Matthew, Nick Reid, Brian Wilson, and Sue V. Briggs. "Invasive native scrub and soil condition in semi-arid south-eastern Australia." Agriculture, Ecosystems & Environment 132, no. 3-4 (August 2009): 212–22. http://dx.doi.org/10.1016/j.agee.2009.04.001.

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42

Muyen, Zahida, Graham A. Moore, and Roger J. Wrigley. "Soil salinity and sodicity effects of wastewater irrigation in South East Australia." Agricultural Water Management 99, no. 1 (November 2011): 33–41. http://dx.doi.org/10.1016/j.agwat.2011.07.021.

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43

Venn, Susanna E., and John W. Morgan. "Soil seedbank composition and dynamics across alpine summits in south-eastern Australia." Australian Journal of Botany 58, no. 5 (2010): 349. http://dx.doi.org/10.1071/bt10058.

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Alpine soil seedbanks are generally regarded as small and unimportant to regeneration. Here, we investigate for the first time the composition of the readily germinable soil seedbank across alpine summits in south-eastern Australia. We aimed to compare the species in the seedbank with the standing vegetation, show seasonal variations in seedbank composition and identify regeneration strategies of alpine seedbank species. By using standard glasshouse and cold-stratification germination techniques, the germinable soil seedbank across the study region was found to comprise 39 species from 25 fami
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44

Shi, Xian-Zhong, Mehrooz Aspandiar, and David Oldmeadow. "Reflectance spectral characterization of acid sulphate soil in South Yunderup, Western Australia." International Journal of Remote Sensing 35, no. 10 (April 24, 2014): 3537–55. http://dx.doi.org/10.1080/01431161.2014.907938.

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Maliki, Ali Al, David Bruce, and Gary Owens. "Spatial distribution of Pb in urban soil from Port Pirie, South Australia." Environmental Technology & Innovation 4 (October 2015): 123–36. http://dx.doi.org/10.1016/j.eti.2015.05.002.

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46

Jankowski, Nathan R., Zenobia Jacobs, and Paul Goldberg. "Optical dating and soil micromorphology at MacCauley's Beach, New South Wales, Australia." Earth Surface Processes and Landforms 40, no. 2 (August 5, 2014): 229–42. http://dx.doi.org/10.1002/esp.3622.

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Singh, B., and RJ Gilkes. "Phosphorus sorption in relation to soil properties for the major soil types of South-Western Australia." Soil Research 29, no. 5 (1991): 603. http://dx.doi.org/10.1071/sr9910603.

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The P sorption characteristics of 97 soils that are representative of the agricultural areas of Western Australia were described using Langmuir and Freundlich equations. The Langmuir P maximum (xm) ranged from 11 to 2132 �g g-1 soil and the Freundlich k coefficient ranged from 1 to 1681. Clay content, DCB Fe and Al, oxalate Fe and AL, and pyrophosphate Al were positively related to xm and k. By using stepwise regression analysis, the combination of DCB and oxalate-soluble A1 predicted more than 75% Of the variation in the P sorption coefficients. Reactive Al compounds may thus be responsible f
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Rabbi, S. M. Fazle, Matthew Tighe, Annette Cowie, Brian R. Wilson, Graeme Schwenke, Malem Mcleod, Warwick Badgery, and Jeff Baldock. "The relationships between land uses, soil management practices, and soil carbon fractions in South Eastern Australia." Agriculture, Ecosystems & Environment 197 (December 2014): 41–52. http://dx.doi.org/10.1016/j.agee.2014.06.020.

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Odgers, Nathan P., Karen W. Holmes, Ted Griffin, and Craig Liddicoat. "Derivation of soil-attribute estimations from legacy soil maps." Soil Research 53, no. 8 (2015): 881. http://dx.doi.org/10.1071/sr14274.

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It is increasingly necessary to apply quantitative techniques to legacy soil polygon maps given that legacy soil maps may be the only source of soil information over large areas. Spatial disaggregation provides a means of extracting information from legacy soil maps and enables us to downscale the original information to produce new soil class maps at finer levels of detail. This is a useful outcome in its own right; however, the disaggregated soil-class coverage can also be used to make digital maps of soil properties with associated estimates of uncertainty. In this work, we take the spatial
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Tighe, M., N. Reid, B. R. Wilson, and M. T. McHenry. "High soil acidity under native shrub encroachment in the Cobar Pediplain, south-eastern Australia." Rangeland Journal 40, no. 5 (2018): 451. http://dx.doi.org/10.1071/rj17124.

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This study investigated the chemical characteristics of shallow (0–30 cm) soil profiles under shrubs in areas of dense encroachment and compared them with shallow soil profiles under nearby large trees. Consistent patterns of high soil acidity were found under shrubs, as well as lower litter alkalinity, lower relative concentrations of calcium (Ca2+), lower effective cation exchange capacity, and higher aluminium (Al3+) and sodium (Na+) in the soil profile compared with under trees. Soil pH (CaCl2) was strongly correlated with the Ca content of surface litter. These findings suggest that shrub
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