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Towards modeling soil texture-specific sensitivity of wheat yield and water balance to climatic changes

机译:建立模拟小麦产量和水分平衡对土壤质地的敏感性的气候变化模型

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Climate change has significant influences on agricultural water management particularly in arid and semi-arid regions. Increased water scarcity and consecutive droughts in these regions must be extensively taken into considerations in any water management scheme dealing with agricultural production. This study was aimed to find out climate changes impacts on soil water balance components and rainfed wheat yield, phenology and failure across eight different soil textural classes over 2070-2099. In order to project the future conditions, outputs of five climate models under RCP-4.5 and RCP-8.5 downscaled by MarkSimGCM were used to drive the CSM-CERES-Wheat v4.6 model. Results indicated that crop-growing season will be shorter by 10.7-21.6 days under RCP-4.5 and 25.8-45.5 days under RCP-8.5. Averaged across all investigated soils, the crop yield would decline in four studied large areas mainly due to drought and inappropriate planting date. Yield loss, averaged across all sites, are likely to be higher in finer-texture soils. More frequent harvest failure can occur over the 2080s particularly in the finer-textured soils at most studied sites. Deep drainage and runoff are expected to drop in almost all soils due to rainfall deficit. Decline of evaporation appears likely as a consequence of drought, shorter growing period and change of evapotranspiration partitioning. The crop model projected larger reduction in drainage and evaporation for coarse soils and in runoff for finer-textured soils. Higher transpiration, averaged over all sites, in coarser soils can be attributed to considerable decline of nitrogen leaching and higher subsoil water content. Furthermore, there would be an increase in soil water storage under most soil-climate simulation runs particularly in heavy-textured soils. In general, soil texture as an inherent static property highly conditions crop-climate interactions in changing climates. Furthermore, rainfed wheat production would likely be more sustainable on coarser soil textures under climate changes. (C) 2016 Elsevier B.V. All rights reserved.
机译:气候变化对农业水管理产生重大影响,特别是在干旱和半干旱地区。在任何涉及农业生产的水资源管理计划中,都必须广泛考虑到这些地区日益严重的缺水和连续干旱。这项研究旨在找出2070-2099年间八种不同土壤质地类别的气候变化对土壤水分平衡成分和雨养小麦产量,物候和破坏的影响。为了预测未来的状况,使用了MarkSimGCM缩减的RCP-4.5和RCP-8.5下的五个气候模型的输出来驱动CSM-CERES-Wheat v4.6模型。结果表明,在RCP-4.5下,农作物的生长季节缩短了10.7-21.6天,在RCP-8.5下,农作物的生长季节缩短了25.8-45.5天。在所有调查土壤上取平均值,主要是由于干旱和不适当的播种日期,在四个研究的大面积地区农作物产量将下降。在质地较细的土壤中,所有地点的平均产量损失可能会更高。在2080年代,收割失误会更加频繁,尤其是在大多数研究地点的质地较细的土壤中。由于降雨不足,预计几乎所有土壤的深层排水和径流都会减少。干旱,生长周期缩短和蒸散分配的变化可能导致蒸发量下降。作物模型预计粗土壤的排水和蒸发量将大大减少,质地较细的土壤的径流将大大减少。在较粗糙的土壤中,所有地点的蒸腾作用均较高,这可归因于氮素浸出的显着下降和较高的底土含水量。此外,在大多数土壤气候模拟运行中,特别是在重质土壤中,土壤水的储存量将增加。通常,土壤质地作为一种固有的静态特性,在不断变化的气候中高度制约着作物与气候之间的相互作用。此外,在气候变化下,如果土壤质地较粗,雨养小麦的生产将更具可持续性。 (C)2016 Elsevier B.V.保留所有权利。

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