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首页> 外文期刊>European Journal of Agronomy >Modelling of actual evapotranspiration in open top chambers (OTC) at daily and seasonal scale: Multi-annual validation on soybean in contrasted conditions of water stress and air ozone concentration
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Modelling of actual evapotranspiration in open top chambers (OTC) at daily and seasonal scale: Multi-annual validation on soybean in contrasted conditions of water stress and air ozone concentration

机译:每天和季节性尺度上开放式顶棚(OTC)中实际蒸散的建模:在水分胁迫和空气臭氧浓度不同的条件下,对大豆进行多年验证

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The present study describes an analytical model, based on the Penman-Monteith equation, for estimating the daily evapotranspiration (ET) inside open top chambers (OTCs). It includes two functions, making it possible to separately take into account the effects of water stress and of high concentrations of air ozone. The input variables of the model are: (i) the diurnal values of global radiation and temperature, usually measured routinely in a standard agro-meteorological station; (ii) the daily values of the AOT40 index accumulated (accumulated ozone over a threshold of 40 ppb during daylight hours, when global radiation exceeds 50 Wm(-2)); and (iii) the periodic measurements of the predawn leaf water potential. These latter two variables were determined inside the OTC.The ability of the model to take into account contrasting conditions of ozone air concentration and water stress was evaluated over three successive years, for 468 days, in 10 crop growth cycles, excluding the days employed to calibrate the model. Tests were carried out in several chambers for each year and take into account the intra- and inter-year variability of ET measured inside the OTCs.On the daily scale, the slope of the linear regression between the ET measured by the soil water balance and that calculated by the model under different water conditions are 0.94 and 1.05 for the filtered and unfiltered (or enriched) OTCs. The correlation coefficients r(2) observed are 0.71 and 0.64 for the two situations. On the seasonal scale, the mean difference between measured and calculated ET is equal to +3% and +10% for the filtered and unfiltered OTCs respectively. The ability of the model to estimate the daily and seasonal ETinside the OTCs was quite good in all of the experimental situations. Thus, the model hypothesis and the calibration considered seem to be realistic and robust.The modifications of the daily ET as a result of the use of OTCs in a Mediterranean region, as compared to a crop cultivated in an open field, were also evaluated. Finally, the possibility of developing a version of the model using only automatically collected variables inside the OTCs was also discussed
机译:本研究描述了一种基于Penman-Monteith方程的分析模型,用于估算顶舱(OTC)内的日蒸散量(ET)。它包括两个功能,可以分别考虑水分胁迫和高浓度空气臭氧的影响。该模型的输入变量为:(i)全球辐射和温度的日数值,通常在标准农业气象台站中进行常规测量; (ii)每天累积的AOT40指数的值(当全球辐射超过50 Wm(-2)时,白天的累积臭氧量超过40 ppb的阈值); (iii)定期测量黎明前叶子的水势。后两个变量是在OTC内确定的。在10个作物生长周期中连续468天(连续468天)评估了该模型考虑臭氧空气浓度和水分胁迫的对比条件的能力,其中不包括校准模型。每年在多个试验箱中进行测试,并考虑到场外交易中心内测得的ET的年内和年际变化性。在日尺度上,通过土壤水平衡和ET测得的ET之间的线性回归斜率。由模型在不同水条件下计算得出的过滤后和未过滤(或浓缩)OTC的平均值分别为0.94和1.05。在两种情况下,观察到的相关系数r(2)为0.71和0.64。在季节性尺度上,已过滤和未过滤OTC的实测ET和计算ET的平均差分别等于+ 3%和+ 10%。在所有实验情况下,该模型估计OTC内每日和季节性ET的能力都非常好。因此,模型假设和校准似乎是现实和稳健的。与露天场所种植的农作物相比,还评估了由于在地中海地区使用OTC而导致的每日ET的变化。最后,还讨论了仅使用OTC内部自动收集的变量来开发模型版本的可能性

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