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Increasing co-limitation of water and nitrogen drives genetic yield gain in Australian wheat

机译:澳大利亚小麦的水和氮气的共同限制越来越泛滥

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The interactions between nitrogen (N) and water are manifold, and the concept of co-limitation provides a quantitative framework for integration. This paper tested the hypothesis that selection for yield increased water-N co-limitation in wheat adapted to winter rainfall environments of Australia. To test this hypothesis, we measured evapotranspiration, N uptake and yield in a historic collection of varieties released between 1958 and 2007 (exp. 1) and between 1969 and 2015 (exp. 2). Crops were grown under 5 (exp. 1) or 4 (exp. 2) environmental conditions resulting from the combination of sites, seasons, and supply of N and water. Genetic gain of yield, i.e. the slope of the regression between yield and year of release was 14-24 kg ha(-1) y(-1) or 0.36-0.52% y(-1). This yield gain was associated with a linear increase in water-N co-limitation, in turn associated with an increase in N uptake per mm of evapotranspiration at a rate of 0.0019 kg N mm(-1) y(-1). Our findings highlight the critical role of nitrogen for the adaptation of wheat to low rainfall environments, and the scope for further yield improvement based on traits that integrate resources.
机译:氮气(n)和水之间的相互作用是歧管,并限制的概念提供了用于集成的定量框架。本文检测了对澳大利亚冬季降雨环境的小麦产量增加的水平合并的假设。为了测试这一假设,我们在1958年至2007年(Exp.1)之间的历史悠久的品种历史悠久的品种收藏品种中测量了蒸散,N的吸收和产量,并在1969年至2015年间(Exp.2)。作物在5(exp.1)或4(exp.2)的环境条件下成长为5(exp.1)或4个(exp.2)N和水供应所产生的环境条件。产率的遗传增益,即产量和释放年份之间的回归的斜率为14-24kg ha(-1)y(-1)或0.36-0.52%y(-1)。该屈服增益与水 - n合并的线性增加有关,又与每毫米蒸腾的N次蒸腾的速率增加相关,以0.0019kg n mm(-1)y(-1)。我们的研究结果突出了氮气对小麦对低降雨环境的适应的关键作用,以及基于整合资源的特征的进一步收益率改善的范围。

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