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首页> 外文期刊>Plant Ecology >True water constraint under a rainfall interception experiment in a Mediterranean shrubland (Northern Tunisia): confronting discrete measurements with a plant-soil water budget model
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True water constraint under a rainfall interception experiment in a Mediterranean shrubland (Northern Tunisia): confronting discrete measurements with a plant-soil water budget model

机译:地中海灌木丛(突尼斯北部)降雨拦截试验下的真实水分约束:用植物-土壤水分预算模型处理离散测量

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Increased drought length and intensity is expected in the Mediterranean basin under anthropogenic increase in atmospheric CO2, leading to extreme events not yet encountered in the present climate variability. Understanding ecosystems responses and capturing peculiar ecophysiological processes related to these events have been investigated in the field by rainfall manipulation experiments. Quantifying the actual drought faced by the ecosystem under control and dry plots, or among experiments remain a key challenge for explaining functional impacts on plant growth. Full-profile soil water content can be tricky to assess in rocky soils, and time-consuming plant water potential measurements remain a discrete information unable to capture short rainfall pulses. We propose here to fully investigate the water budget of a total rainfall interception manipulation on a Mediterranean shrubland, coupled with a plant-soil water balance model. We could accurately simulate the seasonal course of plant water status, including small rainfall pulses. We then derived yearly estimates of water stress integral for each water treatment, leading to an estimate of 66-86 % increase of drought intensity for the dry treatment compared to the control. Comparing actual and expected plant water budget from simulations in the dry plots allowed to identify and quantify the impact of methodological issues related to rainfall interception experiments as side effects for intrusive rain drops and subsurface lateral water flow
机译:在人为造成的大气二氧化碳增加下,地中海盆地的干旱时间和强度预计会增加,从而导致目前气候变化尚未遇到的极端事件。在野外通过降雨操纵实验研究了了解生态系统的响应并捕获与这些事件有关的特殊生态生理过程。量化在控制区和干旱区,或在实验区中的生态系统面临的实际干旱,仍然是解释功能对植物生长的影响的主要挑战。全面的土壤水分含量很难在岩石土壤中评估,并且耗时的植物水势测量值仍然是无法捕获短降雨脉冲的离散信息。我们建议在这里全面调查地中海灌木丛中总降雨拦截操纵的水预算,并结合植物-土壤水平衡模型。我们可以准确地模拟植物水分状况的季节性过程,包括小的降雨脉冲。然后,我们得出了每种水处理的水胁迫积分的年度估计值,与对照相比,干旱处理的干旱强度估计增加了66-86%。通过比较干旱地区的模拟结果,比较实际和预期的植物用水预算,可以识别和量化与降雨截留实验相关的方法学问题的影响,作为侵入性降雨和地下横向水流的副作用

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