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首页> 外文期刊>Hydrological Processes >Simulating soil-water movement under a hedgerow surrounding a bottomland reveals the importance of transpiration in water balance
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Simulating soil-water movement under a hedgerow surrounding a bottomland reveals the importance of transpiration in water balance

机译:模拟围绕低地的树篱下的土壤水运动,揭示了蒸腾作用对水平衡的重要性

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摘要

The objective of this study was to quantify components of the water balance related to root-water uptake in the soil below a hedgerow. At this local scale, a two-dimensional (2D) flow domain in the x-z plane 6 m long and 1-55 m deep was considered. An attempt was made to estimate transpiration using a simulation model. The SWMS-2D model was modified and used to simulate temporally and spatially heterogeneous boundary conditions. A function with a variable spatial distribution of root-water uptake was considered, and model calibration was performed by adjusting this root-water uptake distribution. Observed data from a previous field study were compared against model predictions. During the validation step, satisfactory agreement was obtained, as the difference between observed and modelled pressure head values was less than 50 cm for 80% of the study data. Hedge transpiration capacity is a significant component of soil-water balance in the summer, when predicted transpiration reaches about 5-6 mm day~(-1). One of the most important findings is that hedge transpiration is nearly twice that of a forest canopy. In addition, soil-water content is significantly different whether downslope or upslope depending on the root-water uptake. The high transpiration rate was mainly due to the presence of a shallow water table below the hedgerow trees. Soil-water content was not a limiting factor for transpiration in this context, as it could be in one with a much deeper water table. Hedgerow tree transpiration exerts a strong impact not only on water content within the vadose zone but also on the water-table profile along the transect. Results obtained at the local scale reveal that the global impact of hedges at the catchment scale has been underestimated in the past. Transpiration rate exerts a major influence on water balance at both the seasonal and annual scales for watersheds with a dense network of hedgerows.
机译:这项研究的目的是量化与树篱下土壤中的根系水分吸收有关的水分平衡成分。在这个局部尺度上,考虑了x-z平面中6 m长和1 55 m深的二维(2D)流域。尝试使用模拟模型估算蒸腾量。修改了SWMS-2D模型,并用于模拟时间和空间异构边界条件。考虑具有可变的根水吸收空间分布的函数,并且通过调节该根水吸收分布来进行模型校准。将来自先前现场研究的观察数据与模型预测进行比较。在验证步骤中,获得了令人满意的一致性,因为对于80%的研究数据,观察到的压头值与模型压头值之间的差小于50 cm。当预测的蒸腾量达到约5-6 mm day〜(-1)时,树篱的蒸腾能力是夏季土壤水平衡的重要组成部分。最重要的发现之一是绿篱蒸腾作用几乎是森林冠层的蒸腾作用的两倍。另外,取决于根水的吸收量,无论是下坡还是上坡,土壤含水量都存在显着差异。高蒸腾速率主要是由于在树篱树下存在浅水位。在这种情况下,土壤水分不是蒸腾的限制因素,因为地下水位可能更高。绿篱树的蒸腾不仅对渗流带内的水分含量有很大影响,而且对沿样带的地下水位也有很大的影响。在当地范围内获得的结果表明,过去对冲措施对集水区规模的全球影响被低估了。对于具有密集树篱网络的流域,蒸腾速率在季节和年度尺度上都对水平衡产生重大影响。

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