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Evaluation of a simple approach for crop evapotranspiration partitioning and analysis of the water budget distribution for several crop species.

机译:评价一种简单的作物蒸散量分配方法,并分析几种作物的水预算分配。

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Climate variability and climate change induce important intra- and inter-annual variability of precipitation that significantly alters the hydrologic cycle. The surface water budgets and the plant or ecosystem water use efficiency (WUE) are in turn modified. Obtaining greater insight into how climatic variability and agricultural practices affect water budgets and regarding their components in croplands is, thus, important for adapting crop management and limiting water losses. Therefore, the principal objectives of this study are: (1) to assess the contribution of different components to the agro-ecosystem water budget and (2) to evaluate how agricultural practices and climate modify the components of the surface water budget. To achieve these goals, we tested a new method for partitioning evapotranspiration (ETR), measured by means of an eddy-covariance method, into soil evaporation (E) and plant transpiration (TR) based on marginal distribution sampling (MDS). The partitioning method proposed requires continuous flux recording and measurements of soil temperature and humidity close to the surface, global radiation above the canopy and assessment of leaf area index dynamics. This method is well suited for crops because it requires a dataset including long bare-soil periods alternating with vegetated periods for accurate partitioning estimation. We compared these estimations with calibrated simulations of the ICARE-SVAT double source mechanistic model. The results showed good agreement between the two partitioning methods, demonstrating that MDS is a convenient, simple and robust tool for estimating E with reasonable associated uncertainties. During the growing season, the proportion of E in ETR was approximately one-third and varied mainly with crop leaf area. When calculated on an annual time scale, the proportion of E in ETR reached more than 50%, depending on the crop leaf area and on the duration and distribution of bare soil within the year.
机译:气候多变性和气候变化引起重要的年际和年际降水变化,从而大大改变了水文循环。反过来修改了地表水预算和植物或生态系统的用水效率。因此,对于气候变化和农业实践如何影响水预算及其在农田中的组成部分,有更深入的了解,对于适应作物管理和限制水的流失至关重要。因此,本研究的主要目标是:(1)评估不同组成部分对农业生态系统水预算的贡献;(2)评估农业实践和气候如何改变地表水预算的组成部分。为了实现这些目标,我们测试了一种新的方法,该方法将利用涡度协方差法测量的蒸散量(ETR)划分为基于边缘分布采样(MDS)的土壤蒸发量(E)和植物蒸腾量(TR)。提出的分区方法要求连续记录通量,并测量靠近表面的土壤温度和湿度,冠层上方的全球辐射以及评估叶面积指数动态。该方法非常适合农作物,因为它需要一个包含较长裸土周期和植被周期的数据集,以进行准确的分区估算。我们将这些估计与ICARE-SVAT双源机制模型的校准仿真进行了比较。结果表明两种划分方法之间具有很好的一致性,表明MDS是一种方便,简单且可靠的工具,用于估计具有合理相关不确定性的E。在生长期,ETR中E的比例约为三分之一,并且主要随作物叶片面积而变化。如果按年度时间尺度计算,则ETR在ETR中的比例达到50%以上,这取决于作物叶面积以及一年中裸土的持续时间和分布。

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