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MODELLING THE EFFECTS OF CLIMATIC CHANGE AND GENETIC MODIFICATION ON NITROGEN USE BY WHEAT

机译:模拟气候变化和遗传修饰对小麦氮利用的影响

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This paper considers how and the extent to which climate change and the balance of nitrogen between crops and soils may interact and how the ability to modify genetically specific crop attributes might affect the overall nitrogen balance of the crop-soil system. The possible effects of each change have been assessed using the AFRCWHEAT2 crop model for wheat. Model output pointed to a decrease in harvest index as a result of coincidental increases in CO2 level and temperature, and the importance of considering not only changes to average but also to the variability of environmental driving variables is illustrated. When mean temperatures were raised the model predicted that more nitrate would be left in the soil at the end of the season but that raising CO2 level could counter this effect. Doubling the variability of temperature had a more complicated effect on the soil N balance with the mean amount of residual soil nitrate predicted to be at about the same level as for the baseline and with only a comparatively small change in its coefficient of variation. These results are interpreted in terms of a bell-shaped response of mineralisation rate to temperature. Raising the value of the maximum N concentration (N-max) in the shoots increased the amount of NO3-N extracted from the soil. However, the overall effects were not simply proportional to the increase in N-max because the crop could also become limited by the supply of N from the soil.
机译:本文考虑了气候变化以及农作物与土壤之间的氮平衡之间如何相互作用以及在何种程度上相互作用,以及遗传上特定的作物属性的改变能力如何影响作物-土壤系统的整体氮平衡。已经使用AFRCWHEAT2小麦作物模型评估了每种变化的可能影响。模型输出指出由于二氧化碳水平和温度的同时增加而导致收获指数的下降,并说明了不仅要考虑平均值的变化,而且要考虑环境驱动变量的变化的重要性。当平均温度升高时,该模型预测到季节结束时土壤中会残留更多的硝酸盐,但提高CO2水平可以抵消这种影响。将温度的可变性加倍对土壤氮平衡具有更复杂的影响,预计土壤硝酸盐残留量的平均水平与基准水平大致相同,并且其变异系数的变化相对较小。这些结果是根据矿化速率对温度的钟形响应来解释的。提高枝条中最大氮浓度(N-max)的值会增加从土壤中提取的NO3-N量。但是,总的效果并不仅仅与氮最大含量成正比,因为作物还可能受到土壤中氮的供应的限制。

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