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Seasonal fluctuations of native available N and soil management implications

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Nitrogen Economy in Tropical Soils

Part of the book series: Developments in Plant and Soil Sciences ((DPSS,volume 69))

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Abstract

The concentration of native available N in tropical soils fluctuates considerably in response to seasonal changes in soil water potential. Such fluctuation reflects the net effect of inputs of N from mineralization, fertilizers and the atmosphere, and removal by plant uptake, immobilization, leaching and gaseous losses. The greatest concentrations normally occur during the transition between the dry and wet seasons. In East-Africa, up to 184 kg mineral N ha-1 has been measured in the 0–40 cm soil layer and in Trinidad, 143 kg ha-1 was found in the 0–10 cm layer. Release and accumulation of mineral N occur as a result of the influence of soil water potential on microbial activity. This is due to changes in microbial motility, solute diffusion, microbial survival and the release of protected organic matter. A quantitative understanding of these processes should increase the efficiency of use of this valuable N resource by crops. Current methods of forecasting mineralization under field conditions include measurement of the soil mineralization potential, the release of N from seasonal inputs of litter and model predictions. Litter quality is important. Its composition, in particular its nitrogen, lignin and soluble polyphenol content has a major impact on its N mineralization rate.

Crop uptake, gaseous and leaching losses decrease the concentration of soil mineral N during the wet season. These losses are important under moist tropical conditions. For example, at Port Harcourt and Ibadan in Nigeria, leaching losses were large in spite of NO -3 adsorption which decreased the depth of NO -3 leaching relative to through-flow. To minimise these losses, it is essential to synchronise plant nutrient demand with supply by mineralisation. This is particularly important at the start of the tropical rainy season when high rates of mineralisation often in excess of the relatively low levels of crop demand, are observed. Fertilizer recommendation, the time table for cropping and the farming system used therefore need to take into account the seasonal availability of N. The CERES model simulates crop growth and development and the N-cycle. As development and validation continue, such models should provide a strong basis for better soil, crop and fertilizer management practices. A better understanding of the processes should provide a strong basis for futher development of such models.

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Wong, M.T.F., Nortcliff, S. (1995). Seasonal fluctuations of native available N and soil management implications. In: Ahmad, N. (eds) Nitrogen Economy in Tropical Soils. Developments in Plant and Soil Sciences, vol 69. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-1706-4_2

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  • DOI: https://doi.org/10.1007/978-94-009-1706-4_2

  • Publisher Name: Springer, Dordrecht

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