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Evapotranspiration Model of Maize Field with Ridge Culture Under Alternate Furrow Irrigation

机译:交替沟灌条件下垄作玉米田的蒸散模型。

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To precisely predict evapotranspiration of a maize field with ridge culture under alternate furrow irrigation, a modified Shuttleworth-Wallace (S-W) model was developed by estimating soil surface resistances in irrigated and non-irrigated zones with a proportional coefficient of the wet area, and calculating canopy resistance with the temperature difference between the upper and lower layer canopy. A field experiment with ridge-tillage maize with alternate furrow irrigation was carried out in the 2009 and 2010 seasons. Leaf transpiration was measured using a LI-6400 photosynthesis system, and soil evaporation measured by micro-lysimeter. Soil moisture, stomatal conductance and meteorological factors were collected to estimate soil surface resistance and canopy resistance. Results show that the relative errors between the simulated and observed values of daily soil evaporation were 0.0-10.3%, while the values were 1.4-7.1% for daily crop transpiration. Moreover, the mean absolute error and the root mean square error for simulating daily soil evaporation was 0.2 and 0.3 mm d(-1), respectively, while the values for daily transpiration estimation were 1.5 and 1.8 mm d(-1), respectively. The index of agreement was greater than 0.785, and the determination coefficient higher than 0.90. Therefore, the modified S-W model can well predict evapotranspiration of ridge-culture maize with alternate furrow irrigation. Copyright (c) 2015 John Wiley & Sons, Ltd.
机译:为了精确预测交替垄沟灌溉下垄作玉米田的蒸散量,通过估计灌溉区和非灌溉区的土壤表面阻力(与湿区成比例),开发了改进的Shuttleworth-Wallace(SW)模型,冠层阻力随上,下层冠层之间的温差而变化。在2009年和2010年季节进行了垄耕玉米交替垄沟灌溉的田间试验。使用LI-6400光合作用系统测量叶片的蒸腾作用,并通过微量渗漏仪测量土壤蒸发。收集土壤水分,气孔导度和气象因素以估算土壤表面阻力和冠层阻力。结果表明,模拟和观测的土壤日蒸发量之间的相对误差为0.0-10.3%,而作物日蒸发量的相对误差为1.4-7.1%。此外,模拟每日土壤蒸发的平均绝对误差和均方根误差分别为0.2和0.3 mm d(-1),而每日蒸腾量估算的值分别为1.5和1.8 mm d(-1)。一致性指数大于0.785,测定系数大于0.90。因此,改进的S-W模型可以很好地预测垄沟灌溉玉米的垄作蒸腾量。版权所有(c)2015 John Wiley&Sons,Ltd.

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