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Large regional differences of soil water limitation effect on ozone induced yield loss for wheat and potato in Switzerland

机译:瑞士小麦和马铃薯产量损失土壤水分损失的大型区域差异

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The accumulated stomatal ozone (O_3) uptake over a threshold (Phytotoxic Ozone Dose POD_6), calculated by an ozone deposition model, has been shown to be the most appropriate metric to quantify negative effects of O_3 on food crops. In this study we used data of 13 sites in different regions of Switzerland with multiple years of O_3 measurements to quantify the stomatal O_3 uptake and the related yield loss of wheat and potato. Flux patterns for different years were calculated with the DO_3SE model to disentangle the influence of contrasting seasonal environmental conditions. Regional and inter-annual differences in meteorological conditions led to considerable variations in soil water conditions and the POD_6 values for wheat. Potato stomatal uptake was much less influenced by soil water and showed a more even distribution of P0D_6 values across sites and years. The estimated nationally and temporally average yield loss was 3.2 ± 1.2% for wheat and 2.4 ± 0.8% for potato, calculated based on an area weighting. It was found that soil water deficit, observed frequently in the western part of Switzerland, had a large attenuation effect on stomatal O_3 uptake by wheat and on corresponding yield losses. This highlights the importance of including soil moisture limitation in O_3 uptake modelling even in moist climatic regions. The comparison of modelled evapotranspiration with water flux measurements over a wheat field showed a reasonable agreement concerning the temporal pattern and the magnitude. But it is also concluded that the DO_3SE soil moisture module will need further testing and adaptation to improve accuracy of the model in dryer conditions.
机译:通过臭氧沉积模型计算的阈值(植物毒性臭氧剂量POD_6)的累积气孔臭氧(O_3)吸收已被证明是最适合量的度量,以量化O_3对食物作物的负面影响。在这项研究中,我们使用瑞士不同地区的13个站点的数据,多年来进行O_3测量,以量化气孔o_3摄取和小麦和马铃薯的相关产量丧失。用DO_3SE模型计算不同年份的助焊剂图案,以解除对比季节环境条件的影响。气象状况的区域和年间差异导致土壤水条件和小麦POD_6值相当大的变化。土壤水域的土豆气孔摄取程度较小,并在跨地网站和多年来表现出更均匀的P0D_6值分布。估计的全国和暂时平均屈服损失为小麦的3.2±1.2%,对土豆的2.4±0.8%,基于面积加权计算。发现瑞士西部经常观察到土壤水赤字对小麦​​和相应产量损失对气孔O_3吸收具有大的衰减作用。这凸显了甚至在潮湿气候区域中均匀的土壤水分限制包括土壤水分限制的重要性。在麦田上使用水通量测量的模型蒸散的比较显示了关于时间图案和幅度的合理协议。但还有得出结论,DO_3SE土壤水分模块将需要进一步的测试和适应,以提高烘干机条件下模型的准确性。

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