Soil health and nutrient management

Permanent URI for this collectionhttp://elibrary2.sugarresearch.com.au/handle/11079/13842

Research outcomes: Soil health is improved with a resulting positive impact on the environment and yield growth. Improved reputation and relationship between industry and environmental groups.

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1991 - 199932000 - 20031

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Author: search.filters.author.Kingston, GHas files: Yes

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    Final report SRDC Project CLW009 Improving yield and ccs in sugarcane through the application of silicon based amendments
    (2003) Berthelsen, S; Noble, AD; Kingston, G; Hurney, A; Rudd, A; Garside, A
    Under high leaching environments common to the wet tropics, soils undergo significant weathering, which, when combined with accelerated chemical and physical degradation due to soil perturbation and crop removal, results in increased soil acidification and dissolution of the alumino-silicate clay minerals (de-silication). The consequences are both a loss of plant available Si through leaching and a decline in cation exchange capacity and hence an inability to retain essential plant nutrients. The current project has highlighted that large areas of cane-growing soils in North Queensland have sub-optimal levels of plant-available Si. Based on the current soil test, some 85% of soils that were evaluated in the six mill areas on the wet tropical coast have sub-optimal to marginal levels of available Si. Hence the implications of silicon deficiency for substantial areas under sugarcane production, and therefore the benefit of prophylactic applications of silicate materials may have a significant impact of productivity. One of the primary objectives of this study was to quantify responses in cane yield and ccs to Si application. To address this objective, three field trials were established in Bundaberg, Innisfail and Mossman, using a range of application rates of calcium silicate slag. At Innisfail, over the 2 years of the trial, a rate of 9t/ha Ca-silicate gave a 32% increase in total cane yield (189 t/ha) when compared to the control treatment (128 t/ha). At Mossman, a rate of 12 t/ha gave a 35% total yield increase (161 t/ha) compared to the control (105 t/ha) over the same period. At Bundaberg, over a crop cycle of 3 years, the 12 t/ha rate of Ca-silicate resulted in a 23 % increase (278 t/ha) compared to the control (213 t/ha). The results clearly indicate that Si should be treated as an integral part of any fertilizer strategy associated with cane production on these soils.
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    Consequences of future management options for the Bremerhaven drainage system.
    (1991) Kingston, G
    The following questions were referred to BSES by the Woongoolba Flood Mitigation Advisory Committee: (1) The possible short and long-term effect on all classes of land of lowering the watertable in the Bremerhaven System. (2) The possible effect of the continued use of a designated part of the system for water exchange for the existing prawn farm. These questions will be answered in relation to data acquired in the area of the Bremerhaven System during the Rocky Point Watertable Study from September 1982 to July 1984, and on the basis of sill height determinations at Bremerhaven on 28\8\91 and 19\9\91.
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    Final Report SRDC Project BS98S Factors Affecting the Residual Value of Lime
    (1996) Kingston, G; Aitken, RL
    Project was initiated to determine the relative significance of soil acidity and soil calcium status for predicting response of sugarcane to lime in southern Queensland, where recommendations developed for tropical soils had not been tested previously. Understand the influence of soil properties on the residual value of lime. Study the negative interaction between cane yield response to lime and ccs. Develop and extend improved management guidelines for the necessity and frequency of lime applications.
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    Development of criteria for draining shallow watertables in the Isis irrigation area
    (1993) Kingston, G
    This project was proposed to the Sugar Research Council because qualitative data suggested a significant problem with waterlogging and salinity in hydromorphic sedimentary soils in the Bundaberg to Maryborough region. Also there were no quantitative data to indicate elevation of watertables in areas of hazard, nor were there any criteria to determine an approach to management of shallow watertables in the region.