盐渍化和肥力胁迫下玉米土壤水分、蒸散量和产量变化过程的AquaCrop模型评价

R. Saeidi, H. R. Etedali, A. Sotoodehnia, B. Nazari, A. Kaviani
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Between the two irrigation intervals, the stomatal resistance of maize leaf, was measured by the AP4 prometer device. At the same time as increasing stomatal resistance, RAW was calculated and plots were irrigated. In the days of between two irrigation, was measured the soil moisture content of the plots at the depth of root development. The daily evapotranspiration of the plant, was calculated based on the amount of daily water depletion. For optimal calibration of parameters in the AquaCrop model, was used the method of Generalized Likelihood Uncertainty Estimation (GLUE). Among 16 treatments, 8 treatments were randomly selected for calibration and the rest were selected for validation. Results and discussionResults were obtained for evaluating the AquaCrop model at the validation stage. The root mean square error (RMSE) of soil moisture simulation, varied from 1.43 to 2.6%. The normalized error value (NRMSE) ranged from 4 to 6 percent. 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引用次数: 1

摘要

在存在环境胁迫的情况下,如盐度和肥力胁迫,植物吸收的水分和养分较少。尽管存在盐度和氮缺乏(生育压力)的压力,但用AquaCrop模型确定植物的实际需水量将是重要的。因此,本研究的目的是评价AquaCrop模型在盐度和肥力胁迫下估算玉米土壤水分、蒸散量和产量的效果。材料与方法本研究采用随机完全区组设计,采用4个水平、3个重复的水盐度和氮缺乏2个处理,各设1个对照图。试验植物为704sc玉米,种植面积为3 × 3 m,间距为1.5 m。在该方案中,肥力胁迫表现为氮肥消耗,并分为四个层次。n_0、n_1、N_2和n_34个处理的氮肥用量分别为氮肥推荐用量的100%、75%、50%和25%。盐胁迫是通过用盐水灌溉植株来施加的。根据玉米产量潜力在100、90、75和50% 4个水平上选择水盐处理(3)。根据以上4个性能水平,包括s_0、s_1、S_2和S_3处理;灌溉水电导率分别为0.5、1.2、3.5、7.5 (ds/m)。确定灌溉时间,与水分含量达到RAW(可利用水分)水平相同。在两个灌溉间隔期,用AP4型促气孔仪测定玉米叶片气孔阻力。在增加气孔阻力的同时,计算生长量并进行小区灌溉。在两次灌溉的间隙,测定了各地块根系发育深度的土壤水分含量。植物的日蒸散量是根据日耗水量计算的。采用广义似然不确定性估计(GLUE)方法对AquaCrop模型参数进行最优标定。16个处理中,随机选择8个处理进行校正,其余处理进行验证。结果和讨论在验证阶段对AquaCrop模型进行了评估。土壤湿度模拟的均方根误差(RMSE)在1.43 ~ 2.6%之间。归一化误差值(NRMSE)在4%到6%之间。AquaCrop模式在蒸散发模拟中也表现出类似的趋势。蒸散发模拟的均方根误差(RMSE)在1.85 ~ 2.35 mm之间。归一化误差值(NRMSE)在3.5% ~ 4.5%之间。对于产量模拟,RMSE为0.34吨。ha-1和NRMSE为0.65%。R^2、EF和d统计值表明数据与建模的最佳效率之间具有良好的相关性。结果表明,该模型具有较好的参数估计性能。结论评价模型的能力对农业部门规划者进行参数估计有很大的帮助。本研究利用AquaCrop模型对盐渍化和肥力胁迫下玉米土壤水分、蒸散量和产量进行了估算。模型校准的目的是使模拟数据接近于实际数据(在该地区测量)。得到的NRMSE和R^2分别小于10%和大于0.9,表明模型在这方面的性能最优。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Evaluation of AquaCrop model for estimating of changes process of soil moisture, evapotranspiration and yield of maize under salinity and fertility stresses
IntroductionIn the presence of environmental stresses such as salinity and fertility stresses, water and nutrients less absorbed by the plant. Despite the stresses of salinity and nitrogen deficiency (fertility stress), the determination of the actual water requirement of plants with the AquaCrop model, will be important. Therefore, the aim of this research was to evaluate the AquaCrop model for estimating the soil moisture, evapotranspiration and yield of maize, under the salinity and fertility stresses.Materials and methodsIn this research, two treatments of water salinity and nitrogen deficity in four levels and three replications, with a control plot, were implemented as a factorial experiment in a randomized complete of block design. The studied plant was maize with cultivar of 704 Sc and was planted in plots with dimensions of 3 × 3 meters and 1.5 meters apart. In this plan, fertility stress was in the form of nitrogen fertilizer consumption and at four levels. Treatments of N_0، N_1، N_2 and N_3consisted of consumption of 100, 75, 50 and 25% of nitrogen fertilizer based on fertilizer recommendation, respectively. Salinity stress has been applied by irrigation of the plant with saline water. Water salinity treatments were selected based on yield potential of maize at four levels of 100, 90, 75 and 50% (3). According to the above four performance levels, treatments of S_0، S_1، S_2 and S_3 were included; irrigation water with electric conductivity of 0.5, 1.2, 3.5 and 7.5 (ds/m) respectively. Determining the irrigation time, was the same as the moisture content reached the RAW (Readily Available Water) level. Between the two irrigation intervals, the stomatal resistance of maize leaf, was measured by the AP4 prometer device. At the same time as increasing stomatal resistance, RAW was calculated and plots were irrigated. In the days of between two irrigation, was measured the soil moisture content of the plots at the depth of root development. The daily evapotranspiration of the plant, was calculated based on the amount of daily water depletion. For optimal calibration of parameters in the AquaCrop model, was used the method of Generalized Likelihood Uncertainty Estimation (GLUE). Among 16 treatments, 8 treatments were randomly selected for calibration and the rest were selected for validation. Results and discussionResults were obtained for evaluating the AquaCrop model at the validation stage. The root mean square error (RMSE) of soil moisture simulation, varied from 1.43 to 2.6%. The normalized error value (NRMSE) ranged from 4 to 6 percent. The AquaCrop model showed a similar trend in the evapotranspiration simulation. The root mean square error (RMSE) of evapotranspiration simulation, varied from 1.85 to 2.35 mm. The normalized error value (NRMSE) ranged from 3.5 to 4.5 percent. For yield simulation, RMSE was 0.34 ton. ha-1 and NRMSE was 0.65%. The value of the R^2, EF, and d statistics showed a good correlation between the data and the optimal efficiency of the modeling. Therefore, the results showed that the performance of the model was good in estimating the parameters. ConclusionsEvaluating the capability of the models is a great help to the agricultural sector planners, in estimation the parameters. In this research, evaluated the estimation of soil moisture content, evapotranspiration and yield of maize, under salinity and fertility stresses with AquaCrop model. The purpose of the model calibration was to nearing the simulated data to the real data (measured in the region). The obtained amounts for NRMSE and R^2 were less than 10% and greater than 0.9, respectively, which indicated the optimal performance of the model in this regard.
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