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Journal articles on the topic 'Soils South Australia Lofty, Mount, Ranges, Region'

Author: Grafiati

Published: 4 June 2021

Last updated: 28 January 2023

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1

Fitzpatrick, R. W., J. W. Cox, B. Munday, and J. F. Bourne. "Development of soil-landscape and vegetation indicators for managing waterlogged and saline catchments." Australian Journal of Experimental Agriculture 43, no. 3 (2003): 245. http://dx.doi.org/10.1071/ea00198.

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The objectives of this study were to develop a systematic approach to identify important soil morphological and vegetation field indicators to better target land management in degraded landscapes in a specific region. The authors were able to link the soil-landscape features to the main soil and water processes operating within the landscape. This information was used to develop a set of field indicators (e.g. soil colour) within a user-friendly soil classification key that is linked to land use options to form the basis of a manual. It was shown that information written in this format helped

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2

Speight, Natasha, Daniel Colella, Wayne Boardman, David A. Taggart, Julie I. Haynes, and William G. Breed. "Seasonal variation in occurrence of oxalate nephrosis in South Australian koalas (Phascolarctos cinereus)." Australian Mammalogy 41, no. 1 (2019): 92. http://dx.doi.org/10.1071/am17038.

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Many koalas (Phascolarctos cinereus) in the Mount Lofty Ranges, South Australia, are affected by oxalate nephrosis, in which renal calcium oxalate deposition occurs. In other species, suboptimal water intake increases the risk of urinary calcium oxalate crystal formation. Koalas principally rely on eucalypt leaf moisture content to maintain hydration but the Mount Lofty Ranges region has hot, dry summers. This study investigates the association between temperature, rainfall and eucalypt leaf moisture and the occurrence of oxalate nephrosis in this population of koalas. Koalas from the Mount Lo

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3

Merry, RH, KG Tiller, and AF Richards. "Variability in characteristics of some acidic pasture soils in South Australia and implications for lime application." Soil Research 28, no. 1 (1990): 27. http://dx.doi.org/10.1071/sr9900027.

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The variability of soil pH (0.01 M CaCI2), aluminium and manganese (extractable in 0.01 M CaCl2), total carbon and some soil morphological factors have been investigated in the surface and subsoil at seven pasture sites in the southern Mount Lofty Ranges and Kangaroo Island, South Australia. The coefficients of variation of the factors measured were found to be of a similar order, except for soil pH which, being a logarithmic transformation, is much lower. Relationships between pH and soil aluminium, manganese and carbon are used to predict the effects of further acidification, especially with

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4

Varcoe, Jon, John A. van Leeuwen, David J. Chittleborough, James W. Cox, Ronald J. Smernik, and Anna Heitz. "Changes in water quality following gypsum application to catchment soils of the Mount Lofty Ranges, South Australia." Organic Geochemistry 41, no. 2 (February 2010): 116–23. http://dx.doi.org/10.1016/j.orggeochem.2009.09.010.

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5

Fritsch, E., and RW Fitzpatrick. "Colour plates - Interpretation of soil features produced by ancient and modern processes in degraded landscapes .1. A new method for constructing conceptual soil-water-landscape models." Soil Research 32, no. 5 (1994): 880. http://dx.doi.org/10.1071/sr9940880.

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A pedo-hydrological method which involves interpreting features in soils that result from both ancient and modern processes along toposequences in a subcatchment of the Mt Lofty Ranges, South Australia, is used to construct conceptual soil-water-landscape models. This method links soil-landscape features to soil-water processes with strong emphasis on: (i) soil water-flow systems and (ii) soil-forming and soil-change processes. The conceptual model illustrates the interactions between soil processes acting in soil water-flow systems. This model is able to predict future modes of soil-landscape

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6

Fritsch, E., and RW Fitzpatrick. "Interpretation of soil features produced by ancient and modern processes in degraded landscapes .1. A new method for constructing conceptual soil-water-landscape models." Soil Research 32, no. 5 (1994): 889. http://dx.doi.org/10.1071/sr9940889.

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A pedo-hydrological method which involves interpreting features in soils that result from both ancient and modern processes along toposequences in a subcatchment of the Mt Lofty Ranges, South Australia, is used to construct conceptual soil-water-landscape models. This method links soil-landscape features to soil-water processes with strong emphasis on: (i) soil water-flow systems and (ii) soil-forming and soil-change processes. The conceptual model illustrates the interactions between soil processes acting in soil water-flow systems. This model is able to predict future modes of soil-landscape

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7

Naidu, R., DR Williamson, RW Fitzpatrick, and IO Hollingsworth. "Effect of landuse on the composition of throughflow water immediately above clayey B horizons in the Warren Catchment, South Australia." Australian Journal of Experimental Agriculture 33, no. 2 (1993): 239. http://dx.doi.org/10.1071/ea9930239.

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The effect of landuse on composition of throughflow water immediately above the clayey B horizons in duplex soils (mostly natric and/or sodic) in the Mount Lofty Ranges, South Australia, was investigated using simple lysimeters. During July-November 1991, the pH of the first flow immediately after rainstorm under pines, native woodland, and pasture, respectively, was 5.7, 6.0, and 6.4. At each of the sites, average pH over 4 months during July-November was 5.8-5.9. Both the electrical conductivity (EC) and the amounts of total dissolved solids (TDS) were 2-3 times higher under pine than at oth

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8

Biddle, DL, DJ Chittleborough, and RW Fitzpatrick. "Field-based comparison of platinum and wax impregnated graphite redox electrodes." Soil Research 33, no. 3 (1995): 415. http://dx.doi.org/10.1071/sr9950415.

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An inert electrode was constructed using wax-impregnated graphite (WIG) as an alternative to Pt for permanent installation in the regolith. The performance of WIG electrodes has not previously been systematically evaluated by using data from field trials, although Pt and WIG measure similar Eh values in laboratory solutions. We compared the performance of the WIG electrode when installed adjacent to Pt redox electrodes in the A, B and C horizons of duplex soils in a X-eralf-Aqualf toposequence near Mount Crawford in the Mt Lofty Ranges, South Australia. Lower potentials, commonly in the order

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9

BAKER, G. H., V. J. BARRETT, R. GREY-GARDNER, and J. C. BUCKERFIELD. "The life history and abundance of the introduced earthworms Aporrectodea trapezoides and A. caliginosa (Annelida: Lumbricidae) in pasture soils in the Mount Lofty Ranges, South Australia." Austral Ecology 17, no. 2 (June 1992): 177–88. http://dx.doi.org/10.1111/j.1442-9993.1992.tb00796.x.

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10

Granger, AR, and DRC Traeger. "Effect of different rates and timing of soil applications of paclobutrazol on the growth of sweet cherries (Prunus avium L.)." Australian Journal of Experimental Agriculture 33, no. 2 (1993): 207. http://dx.doi.org/10.1071/ea9930207.

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The response of sweet cherry trees (butt circumference, canopy volume, yield) to different rates of the growth-inhibiting chemical paclobutrazol applied at various times during each year was studied on red podsolic soils in the Mount Lofty Ranges of South Australia Two experiments were conducted: one used a regression design with 16 rates of paclobutrazol; the other was a randomised block experiment with paclobutrazol treatments applied in spring, autumn, or half in autumn and half in spring. Butt circumference growth of the variety Sam grafted on Mahaleb rootstocks tended to reduce with incea

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11

Guan, H., A. J. Love, C. T. Simmons, O. Makhnin, and A. S. Kayaalp. "Factors influencing chloride deposition in a coastal hilly area and application to chloride deposition mapping." Hydrology and Earth System Sciences 14, no. 5 (May 26, 2010): 801–13. http://dx.doi.org/10.5194/hess-14-801-2010.

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Abstract. Chloride is commonly used as an environmental tracer for studying water flow and solute transport in the environment. It is especially useful for estimating groundwater recharge based on the commonly used chloride mass balance (CMB) method. Strong spatial variability in chloride deposition in coastal areas is one difficulty encountered in appropriately applying the method. A high-resolution bulk chloride deposition map in the coastal region is thus needed. The aim of this study is to construct a chloride deposition map in the Mount Lofty Ranges (MLR), a coastal hilly area of approxim

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12

Guan, H., A. J. Love, C. T. Simmons, and A. S. Kayaalp. "Factors influencing chloride deposition in a coastal hilly area and application to chloride deposition mapping." Hydrology and Earth System Sciences Discussions 6, no. 5 (September 16, 2009): 5851–80. http://dx.doi.org/10.5194/hessd-6-5851-2009.

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Abstract. Chloride is commonly used as an environmental tracer for studying water flow and solute transport in the environment. It is especially useful for estimating groundwater recharge based on the commonly used chloride mass balance (CMB) method. Strong spatial variability in chloride deposition in coastal areas is one difficulty encountered in appropriately applying the CMB approach. Furthermore, intensive vegetation clearance for agriculture, for example during the European settlement in many coastal areas of Australia, may have perturbed catchment chloride balance conditions for appropr

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13

Cox, JW, E. Fritsch, and RW Fitzpatrick. "Interpretation of soil features produced by ancient and modern processes in degraded landscapes. VII. Water duration." Soil Research 34, no. 6 (1996): 803. http://dx.doi.org/10.1071/sr9960803.

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Rising saline groundwater and fresh perched water have increased over 120 years (modern processes) in the Mediterranean region (>600 mm per annum) of the Mt Lofty Ranges, South Australia. This was caused by replacement of native vegetation with pastures which use less water. Relationships between morphological features (mainly soil colour) and field measurements (e.g. watertable duration, salinity, and sodicity) were studied to 3 m at 12 sites down a representative toposequence of red-yellow-grey duplex soils (Palexeralfs-Natraqualfs), which are common from crest to flat in these catchments

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14

Bresciani, Etienne, Roger H. Cranswick, Eddie W. Banks, Jordi Batlle-Aguilar, Peter G. Cook, and Okke Batelaan. "Using hydraulic head, chloride and electrical conductivity data to distinguish between mountain-front and mountain-block recharge to basin aquifers." Hydrology and Earth System Sciences 22, no. 2 (March 2, 2018): 1629–48. http://dx.doi.org/10.5194/hess-22-1629-2018.

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Abstract. Numerous basin aquifers in arid and semi-arid regions of the world derive a significant portion of their recharge from adjacent mountains. Such recharge can effectively occur through either stream infiltration in the mountain-front zone (mountain-front recharge, MFR) or subsurface flow from the mountain (mountain-block recharge, MBR). While a thorough understanding of recharge mechanisms is critical for conceptualizing and managing groundwater systems, distinguishing between MFR and MBR is difficult. We present an approach that uses hydraulic head, chloride and electrical conductivit

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15

Maier, NA, G. Barth, and M. Bennell. "Effect of nitrogen, potassium and phosphorus on the yield, growth and nutrient status of ixodia daisy (Ixodia achillaeioides ssp. alata)." Australian Journal of Experimental Agriculture 34, no. 5 (1994): 681. http://dx.doi.org/10.1071/ea9940681.

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The effect of annual applications of nitrogen (N), potassium (K) and phosphorus (P) on the yield, growth and nutrient status of Ixodia daisy (Ixodia achillaeioides ssp. alata) grown on a silty loam, was investigated in field experiments conducted during 1989-91 in the Mount Lofty Ranges, South Australia. The experimental design was a randomised block with 3 replications. The N and K treatments, at annual rates up to 200 kg N/ha and 150 kg K/ha, were applied as 2 equal side-dressings. The P treatments, at rates up to 200 kg/ha, were broadcast as 1 annual application. To assess plant nutrient st

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