利用不同方法估算和比较突尼斯不同生物气候阶段橄榄树灌溉计划的参考蒸散量

Amani Bchir, R. Lemeur, F. B. Mariem, N. Boukherissa, W. Gariani, Haifa Sbaii, A. B. Dhiab, Samia Ben Mansour Gueddes, M. Braham
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引用次数: 4

摘要

橄榄树水分需求的研究可以通过使用更精确的方法,包括土壤-植物-大气连续体的最大参数,来实现更好的水管理。Penman-Monteith方程被认为是计算蒸散发最合理、最可靠的方法。只有这种方法才需要大量的气候参数。使用其他不那么复杂和使用较少气候参数的方程可能是一种可靠和有效的替代方法。本试验以2个品种cv为研究对象。“梅斯基”和简历。“Chemlali”在突尼斯不同生物气候阶段(半湿润、半干旱和干旱)的集约化系统中进行。本研究旨在利用蒸发蒸腾计算方法估算橄榄树在三个不同生物气候阶段的需水量。为此,我们将Penman-Monteith公式与Blaney-Criddel、Hargreaves- temperature、Hargreaves- Radiation和Priestley-Taylor公式进行比较,估算参考蒸散量(ET0)。结果表明,Priestley-Taylor和Blaney-Criddel公式计算的ET0值与Penman-Monteith公式计算的ET0值或多或少相似。哈格里夫斯-温度法和哈格里夫斯-辐射法计算的ET0值是Penman-Monteith公式计算值的两倍。Penman-Monteith方程计算的参考蒸散量与Priestley-Taylor和Blaney-Criddel方程计算的参考蒸散量在所有生物气候阶段均具有良好的相关性(R2大于0.85,p < 1%)。对ET0的敏感性分析表明,在不同气候区水平上,太阳辐射和气温(能量气候参数)对ET0的影响占主导地位。因此,在缺乏某些气候参数的情况下,在半湿润、半干旱和干旱条件下,对于橄榄树的不同物候阶段,我们可以使用Priestley-Taylor和/或Blaney-Criddle公式来估计水分需求。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Estimation and comparison of reference evapotranspiration using different methods to determine olive trees irrigation schedule in different bioclimatic stages of Tunisia
The study of olive trees water requirements allows a better water management by using more accurate methods including maximum parameters of the continuum soil-plant- atmosphere. The Penman-Monteith equations is consideredas the most rational approach and the most reliable for calculating evapotranspiration. Only this approach necessarily requires an important number of climate parameters. The use of other equations, less complicated and using less climate parameters may be a reliable and efficient alternative. This experimental study was carried out on two cultivars cv. "Meski" and cv. "Chemlali" conducted in the intensive system in different bioclimatic stages (Subhumid, Semi-Arid and Arid) in Tunisia. This work aims to estimate olive trees water needs using evapotranspiration calculation in three different bioclimatic stages. For that, we compared the Penman-Monteith formula with Blaney-Criddel, Hargreaves-Temperature, Hargreaves- Radiation and Priestley-Taylor formulas to estimate reference evapotranspiration (ET0). Results show that ET0 values calculated by Priestley-Taylor and Blaney-Criddel formulas were more or less similar to Penman-Monteith. The ET0 values found by Hargreaves-Temperature and Hargreaves-Radiation were twice the values calculated by Penman-Monteith formula. We also found good correlations between the reference evapotranspiration calculated by the Penman-Monteith equation and that calculated by Priestley-Taylor and Blaney-Criddel equations in all bioclimatic stages (R2 more than 0.85, p < 1%). The ET0 sensitivity analysis has shown that solar radiation and air temperature (energetic climatic parameters) have the dominant effect on the ET0 at the level of the different climatic regions. Accordingly, in the case of lack of some climatic parameters and in sub-humid, semi-arid and arid conditions and for the different phenological stages of the olive tree, we can use Priestley-Taylor and/or Blaney-Criddle formulas to estimate water needs.
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