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Investigation of Water Dynamics and the Effect of Evapotranspiration on Grain Yield of Rainfed Wheat and Barley under a Mediterranean Environment: A Modelling Approach

机译:地中海环境下水动力学和蒸散量对雨养小麦和大麦籽粒产量的影响研究:一种建模方法

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摘要

Agro-hydrological models have increasingly become useful and powerful tools in optimizing water and fertilizer application, and in studying the environmental consequences. Accurate prediction of water dynamics in such models is essential for models to produce reasonable results. In this study, detailed simulations were performed for water dynamics of rainfed winter wheat and barley grown under a Mediterranean climate over a 10-year period. The model employed (Yang et al., 2009. J. Hydrol., 370, 177-190) uses easily available agronomic data, and takes into consideration of all key soil and plant processes in controlling water dynamics in the soil-crop system, including the dynamics of root growth. The water requirement for crop growth was calculated according to the FAO56, and the soil hydraulic properties were estimated using peto-transfer functions (PTFs) based on soil physical properties and soil organic matter content. Results show that the simulated values of soil water content at the depths of 15, 45 and 75 cm agreed with the measurements well with the root of the mean squared errors of 0.027 cm3 cm-3 and the model agreement index of 0.875. The simulated seasonal evapotranspiration (ET) ranged from 208 to 388 mm, and grain yield was found to correlate with the simulated seasonal ET in a linear manner within the studied ET range. The simulated rates of grain yield increase were 17.3 and 23.7 kg ha-l for every mm of water evapotranspired for wheat and barley, respectively. The good agreement of soil water content between measurement and simulation and the simulated relationships between grain yield and seasonal ET supported by the data in the literature indicates that the model performed well in modelling water dynamics for the studied soil-crop system, and therefore has the potential to be applied reliably and widely in precision agriculture. Finally, a two-staged approach using inverse modelling techniques to further improve model performance was discussed.
机译:农业水文模型已日益成为优化水和肥料施用以及研究环境后果的有用和强大的工具。这种模型中水动力学的准确预测对于模型产生合理的结果至关重要。在这项研究中,对地中海气候下长达10年的雨养冬小麦和大麦的水分动力学进行了详细的模拟。使用的模型(Yang等,2009。J. Hydrol。,370,177-190)使用易于获得的农艺数据,并考虑了控制土壤作物系统中水动力学的所有关键土壤和植物过程,包括根系生长的动态。根据FAO56计算作物生长的需水量,并根据土壤物理性质和土壤有机质含量,使用peto-transfer函数(PTF)估算土壤的水力性质。结果表明,在15、45和75 cm深度处的土壤水分模拟值与测量值吻合得很好,均方根误差为0.027 cm 3 cm -3 ,模型一致性指数为0.875。模拟的季节蒸散量(ET)范围为208至388 mm,并且在研究的ET范围内发现谷物产量与模拟的季节性ET呈线性相关。小麦和大麦每蒸腾一毫米水的模拟产量分别为17.3和23.7 kg ha -l <​​/ sup>。文献数据支持了测量与模拟之间土壤水分含量与谷物产量与季节性ET之间模拟关系的良好一致性,表明该模型在所研究的土壤-作物系统的水动力学建模中表现良好,因此具有在精密农业中可靠和广泛应用的潜力。最后,讨论了使用逆建模技术进一步改善模型性能的两阶段方法。

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