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Irrigation practices may affect denitrification more than nitrogen mineralization in warm climatic conditions

机译:在温暖的气候条件下,灌溉实践对反硝化的影响大于对氮矿化的影响

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Predicting the impact of irrigation practices on soil N mineralization and N balance is an important issue to optimize N fertilization and reduce the N losses towards the environment. The effect of summer irrigation on N dynamics was investigated in two arable fields in Southern France. Net N mineralization was assessed by combining frequent measurements of water and mineral N contents in soil and the use of a calculation model (LIXIM). It was first calculated assuming that denitrification was negligible. This hypothesis led to inconsistent results, apparent net N mineralized being smaller under irrigated than non-irrigated conditions and net mineralization kinetics being erratic. The occurrence of denitrification was confirmed by the use of 15NO3 tracing in an experiment carried out in summer, including three irrigated treatments. The average 15N recovery varied from 45% to 85% and was smallest in the most frequently irrigated treatment. Over the 8-week experiment, the N losses varied from 30 to 38 kg ha?1 in the irrigated treatments. They were satisfactorily simulated by a simple denitrification model (NEMIS). Combining the LIXIM model and the simulated or calculated denitrification allowed to predict satisfactorily the evolution of soil mineral N accounting for the effects of temperature and moisture. The net N mineralized for 8 weeks varied from 34 kg N ha?1 in the un-irrigated to 46 kg N ha?1 in the irrigated treatments. The drying–rewetting cycles did not induce a flush of N mineralization. Our results suggest that denitrification has to be accounted for in irrigated systems, particularly in warm conditions and when the topsoil contains high nitrate contents.
机译:预测灌溉措施对土壤氮矿化和氮平衡的影响是优化氮肥施用和减少氮向环境损失的重要问题。在法国南部的两个耕地中研究了夏季灌溉对氮素动态的影响。通过结合经常测量土壤中水和矿物质N含量并使用计算模型(LIXIM)来评估净氮矿化。首先假设脱氮量可以忽略不计。该假设导致结果不一致,灌溉条件下的表观净氮矿化比非灌溉条件下的要小,并且净矿化动力学不稳定。夏季进行的一项实验(包括三种灌溉处理)通过使用15 NO3 示踪证实了反硝化的发生。 15 N的平均回收率从45%到85%不等,在最频繁的灌溉处理中最小。在为期8周的实验中,灌溉处理的氮素损失从30到38 kg ha?1 不等。通过简单的反硝化模型(NEMIS)令人满意地模拟了它们。结合LIXIM模型和模拟或计算的反硝化作用,可以令人满意地预测考虑温度和湿度影响的土壤矿质氮的演变。连续8周的矿化净氮量从未灌溉的34 kg N ha?1 到灌溉处理的46 kg N ha?1 。干燥-再湿循环没有引起氮矿化。我们的结果表明,在灌溉系统中必须考虑反硝化作用,特别是在温暖的条件下以及表土中硝酸盐含量高的情况下。

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