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Soil water status triggers CO2 fertilization effect on the growth of winter wheat (Triticum aestivum)

机译:土壤水分状态触发CO2施肥对冬小麦生长(Triticum Aestivum)的影响

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Understanding the key processes and potential mechanisms of crops in response to elevated atmospheric CO2 concentration and drought may further shed lights on the impacts of climate change on the global agriculture ecosystems. This study examined the effects of elevated atmospheric CO2 concentration on the growth of winter wheat under different soil water conditions (full irrigation, mild water stress, moderate water stress, and severe water stress) with growth chambers where the CO2 concentration was controlled at 400 and 800 mu mol mol(-1) , respectively. We found a very strong CO2 fertilization effect on the growth of winter wheat under full irrigation condition, whereas this CO2 fertilization effect declined and eventually vanished with soil water stress, as evidenced by the decreased plant biomass and leaf photosynthesis of winter wheat independent of CO2 concentration. This adverse impact of water stress on the CO2 fertilization effect for plant growth may attribute to the changes in morphological characteristics of individual stoma and spatial distribution pattern of stomata as well as the non-structural carbohydrates of winter wheat. These results suggested that water stress may lower the CO2 fertilization effect on plant growth through altering stomatal traits, leaf photochemical processes, and biochemical compositions of winter wheat. Therefore, many current climate models based on earlier "double-CO2" experiment may overestimate the CO2 fertilization effect on crops, and meanwhile underestimate the impacts of climate change on global agriculture production when the elevated atmospheric CO2 concentration confounded with drought stress under future climate change.
机译:了解作物响应升高的大气二氧化碳浓度和干旱的关键过程和潜在机制可能进一步揭示了气候变化对全球农业生态系统的影响。本研究检测了大气CO2浓度升高对不同土壤水条件下冬小麦生长的影响(全灌溉,温和的水胁迫,中度水分胁迫和严重水胁迫,浓度的生长室,其中CO 2浓度在400℃下控制分别为800 mol mol(-1)。我们对全灌时的冬小麦的生长造成了非常强大的二氧化碳施肥对冬小麦的增长,而这种二氧化碳施肥效果下降并最终因土壤水分胁迫消失,而冬小麦的植物生物质和叶片光合作用而言依赖于二氧化碳浓度。水分胁迫对植物生长的二氧化碳施肥效应的这种不利影响可能归因于冬小麦单个造口和空间分布模式的形态特征的变化。这些结果表明,通过改变冬小麦的气孔特征,叶片光化学方法和生化组成,水分应激可能降低植物生长的二氧化碳施肥对植物生长。因此,基于早期的“双二氧化碳”实验的许多当前气候模型可能会高估对作物的二氧化碳施肥效应,同时低估了气候变化对全球农业生产的影响,当未来的气候变化下有升高的大气二氧化碳浓度时。

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