CRA-Research Unit for Agriculture in Dry Environments, Via C. Ulpiani, 5, 70125 Bari, Italy.
Environ Monit Assess. 2012 Oct;184(10):6377-94. doi: 10.1007/s10661-011-2427-6. Epub 2011 Nov 25.
The present study describes an operational method, based on the Katerji et al. (Eur J Agron 33:218-230, 2010) model, for determining the daily evapotranspiration (ET) for soybean inside open top chambers (OTCs). It includes two functions, calculated day par day, making it possible to separately take into account the effects of concentrations of air ozone and plant water stress. This last function was calibrated in function of the daily values of actual water reserve in the soil. The input variables of the method are (a) the diurnal values of global radiation and temperature, usually measured routinely in a standard weather station; (b) 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)) determined inside the OTC; and (c) the actual water reserve in the soil, at the beginning of the trial. The ensemble of these input variables can be automatable; thus, the proposed method could be applied in routine. The ability of the method to take into account contrasting conditions of ozone air concentration and water stress was evaluated over three successive years, for 513 days, in ten crop growth cycles, excluding the days employed to calibrate the method. 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 proposed method, under different water conditions, are 0.98 and 1.05 for the filtered and unfiltered (or enriched) OTCs with root mean square error (RMSE) equal to 0.77 and 1.07 mm, respectively. On the seasonal scale, the mean difference between measured and calculated ET is equal to +5% and +11% for the filtered and unfiltered OTCs, respectively. The ability of the proposed method to estimate the daily and seasonal ET inside the OTCs is therefore satisfactory following inter- and intra-annual tests. Finally, suggestions about the applications of the proposed method for other species, different from soybean, were also discussed.
本研究描述了一种基于 Katerji 等人(Eur J Agron 33:218-230, 2010)模型的操作方法,用于确定开放式顶部气室(OTC)内大豆的日蒸散量(ET)。它包括两个函数,逐日计算,可分别考虑空气臭氧浓度和植物水分胁迫的影响。后一个功能是根据土壤中实际水分储备的日值进行校准的。该方法的输入变量为:(a)通常在标准气象站常规测量的日全辐射和温度的日变化值;(b)在 OTC 内累积的 AOT40 指数(白天全球辐射超过 50 Wm(-2) 时超过 40 ppb 的臭氧累积量)的日值;(c)试验开始时土壤中的实际水分储备。这些输入变量的集合可以实现自动化;因此,该方法可以常规应用。该方法在三年的 513 天内,在十个作物生长周期中,评估了臭氧空气浓度和水分胁迫的不同条件下的能力,不包括方法校准的天数。每年在多个气室内进行测试,并考虑了 OTC 内测量的 ET 的年际和年内变异性。在日尺度上,在不同水分条件下,土壤水分平衡法测量的 ET 与提出的方法计算的 ET 之间的线性回归的斜率分别为 0.98 和 1.05,对于过滤和气室和未过滤(或富氧)气室,根均方误差(RMSE)分别为 0.77 和 1.07mm。在季节尺度上,测量和计算的 ET 的平均差异分别为过滤和气室为+5%和+11%。因此,经过年际和年内测试,该方法在 OTC 内估计日和季节 ET 的能力令人满意。最后,还讨论了该方法在大豆以外的其他物种中的应用建议。