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首页> 外文期刊>Ciência Rural >Evapotranspira??o real e coeficiente da cultura da laranja lima durante a fase inicial de desenvolvimento na regi?o de Rio Largo, Alagoas
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Evapotranspira??o real e coeficiente da cultura da laranja lima durante a fase inicial de desenvolvimento na regi?o de Rio Largo, Alagoas

机译:阿拉戈斯州里奥拉戈地区初始发展阶段的实际蒸散量和石灰橙作物系数

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Determining actual crop evapotranspiration (ETa) is paramount for irrigation management. The principal measurement methods and physical models generally require crop and weather data that are not readily available. We determined the crop coefficient (Kc) of sweet oranges during the initial development stage and evaluated the performance of the Poulovassilis semi-empirical model coupled with a simple soil water balance for estimating the ETa. The ETa was inferred from the variation in the soil water content over time, measured by time-domain reflectometry. In the Poulovassilis model, the ETa is obtained by multiplying the crop evapotranspiration (ETc) by an adjustment coefficient (ca), which accounts for a reduction in the evapotranspiration caused by soil water depletion. Soil water storage was obtained using the daily and 10-day soil water balances, computed by considering inputs and outputs of water from the system. The empirical parameter, ca, was determined using inverse modeling. The optimal ca value obtained through inverse modeling was 0.05 and 0.03 for the daily and 10-day soil water balances, respectively. The model performed better for the daily soil water balance than the 10-day balance, with performance comparable with the other ETa models. Average Kc during the sweet orange initial crop stage was 0.85.
机译:确定实际作物的蒸散量(ETa)对于灌溉管理至关重要。主要的测量方法和物理模型通常需要不易获得的作物和天气数据。我们确定了甜橙在初始发育阶段的作物系数(Kc),并评估了Poulovassilis半经验模型与简单的土壤水平衡来估算ETa的性能。根据时域反射仪测量的土壤水分含量随时间的变化推断出ETa。在Poulovassilis模型中,通过将作物的蒸散量(ETc)乘以调整系数(ca)来获得ETa,这说明了土壤耗水导致的蒸散量减少了。使用每日和10天的土壤水平衡来获得土壤水储量,并通过考虑系统中水的输入和输出来计算。使用反模型确定经验参数ca。通过逆模型获得的最佳ca值分别为每日和10天土壤水平衡的0.05和0.03。该模型的每日土壤水平衡比10天的平衡更好,其性能可与其他ETa模型相媲美。甜橙初始作物阶段的平均Kc为0.85。

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