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Modelling soil water dynamics of full and deficit drip irrigated maize cultivated under a rain shelter

机译:雨棚下滴灌玉米全亏缺灌溉的土壤水分动力学模拟

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The model HYDRUS-1D was used to simulate soil water dynamics of full and deficit irrigated maize grown under a rainout shelter during two crop seasons. Four irrigation treatments were established based on the amount of water applied to fulfil crop water requirements. Treatment D1 was irrigated to fully satisfy crop water requirements, while treatments D2 (mild deficit), D3 (moderate deficit), and D4 (severe deficit) were for increased controlled water stress conditions. The computation and partitioning of evapotranspiration data into soil evaporation and crop transpiration was carried out with the SIMDualKc model, and then used with HYDRUS-1D. The soil hydraulic properties were determined from numerical inversion of field water content data. The compensated root water uptake mechanism was used to describe water removal by plants. The HYDRUS-1D model successfully simulated the temporal variability of soil water dynamics in treatments irrigated with full and deficit irrigation, producing RMSE values that varied between 0.014 and 0.025 cm(3) cm(-3) when comparing model simulations with field measurements. Actual transpiration varied between 224 and 483 mm. Potential transpiration reductions varied from 0.4 to 48.8% due to water stress, but plants were able to compensate for the water deficits in the surface layers by removing more water from the deeper, less stressed layers. HYDRUS-1D water balance estimates were also comparable with the corresponding ones determined with the SIMDualKc water balance model. Both modelling approaches should contribute to improve the web-based IRRIGA system, used to support farm irrigation scheduling in Brazil. (C) 2015 IAgrE. Published by Elsevier Ltd. All rights reserved.
机译:HYDRUS-1D模型用于模拟两个作物季节在雨棚下种植的全灌和缺水灌溉玉米的土壤水分动态。根据满足作物需水量的水量,确定了四种灌溉处理方法。处理D1被灌溉以完全满足作物的需水量,而处理D2(轻度亏缺),D3(中度亏缺)和D4(严重亏缺)则是为了增加受控水分胁迫条件。利用SIMDualKc模型将蒸散数据计算和划分为土壤蒸发和农作物蒸腾,然后将其与HYDRUS-1D一起使用。根据田间含水量数据的数值反演确定土壤的水力特性。补偿的根系吸水机制用于描述植物对水分的去除。 HYDRUS-1D模型成功地模拟了全量和亏缺灌溉条件下土壤水动力学的时变性,将模型模拟与现场测量相比较时,产生的RMSE值在0.014至0.025 cm(3)cm(-3)之间变化。实际蒸腾量在224至483毫米之间变化。由于水分胁迫,潜在的蒸腾作用减少量从0.4到48.8%不等,但是植物能够通过从压力较小的较深层中除去更多的水分来补偿表层的水分亏缺。 HYDRUS-1D的水平衡估算值也与使用SIMDualKc水平衡模型确定的相应估算值具有可比性。两种建模方法都应有助于改善基于Web的IRRIGA系统,该系统用于支持巴西的农田灌溉计划。 (C)2015年。由Elsevier Ltd.出版。保留所有权利。

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