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Changes in exchangeable cations and micronutrients in soils and grains of long-term, low input cropping systems of subtropical Australia

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Publication date: 1 January 2017
Source:Geoderma, Volume 285
Author(s): Peter M. Kopittke, Ram C. Dalal, Neal W. Menzies
Demand for agricultural products is increasing, but there remains considerable uncertainty regarding many of the impacts of long-term cropping systems on soil properties. Using six soils from low input cropping systems of subtropical Australia, the effects of long-term cultivation (≤70y) on three macronutrient cations (Ca, Mg, and K) and three micronutrient cations (Cu, Zn, and Mn) was examined. For Ca, Mg, and K, exchangeable concentrations generally remained constant and were not influenced by the period of cultivation. As a result, concentrations of these nutrients in grain tissues of wheat (Triticum aestivum) also remained constant over time. However, concentrations of DTPA-extractable Cu, Zn, and Mn often (but not always) decreased significantly over time, with Cu decreasing 21%, Zn by 34%, and Mn by 46% (when averaged across soils where significant differences were found). In some soils, these decreases in DTPA-extractable micronutrients also resulted in concomitant decreases in grain tissue concentrations. These decreases in DTPA-extractable Cu, Zn, and Mn concentrations do not result only from the export of nutrients in grain tissues, but also, from an increase in soil pH caused by a cultivation-induced mixing of alkaline subsoil into the surface soil. The data presented here demonstrate the potential impact of long-term cropping on nutrient availability, and in particular, the need to consider changes in nutrient availability and its potential impact on plant and human nutrition.


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