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首页> 外文期刊>Journal of Hydrology >Simulating riparian evapotranspiration: A new methodology and application for groundwater models
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Simulating riparian evapotranspiration: A new methodology and application for groundwater models

机译:模拟河岸蒸散:地下水模型的新方法和应用

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This paper describes the development and application of a new methodology to simulate riparian and wetland evapotranspiration (ET) in groundwater models. Traditional approaches for modeling ET are based on quasi-linear relationship between ET flux rate and hydraulic head (groundwater elevation). The approach presented here uses multiple non-linear, segmented flux curves that reflect the ecophysiology of the plant species in these systems. Five plant functional groups (PFGs) based on water tolerance ranges and rooting depths are used to elucidate the interactive processes of plant transpiration with groundwater conditions. ET flux rate curves set the extinction and saturation extinction depths and define the group's ET flux rate as a function of water table depth relative to the ground surface. The calculated ET loss from a riparian or wetland system is dependent on the contributing area of each plant functional subgroup present and water table conditions. The new methodology requires a fractional coverage for each of the PFGs present within the groundwater model cell and allows for more accurate assignment of land surface elevations. Model results for a case-study show significant differences in predicted ET and subsequent depth to groundwater between the new and the traditional approaches. The development of physiologically based transpiration curves combined with the traditional linear curve for bare soil/open water results in more accurate determinations of riparian ET and improved basin scale water budgets. The use of PFGs in combination with the new RIP-ET package provides an explicit link between groundwater and riparian/wetland habitat conditions and offers an opportunity to better manage and restore riparian and wetland systems. (c) 2005 Elsevier B.V. All rights reserved.
机译:本文介绍了在地下水模型中模拟河岸和湿地蒸散量(ET)的新方法的开发和应用。传统的ET建模方法基于ET通量率与水头(地下水高程)之间的准线性关系。这里介绍的方法使用了多个非线性的分段通量曲线,这些曲线反映了这些系统中植物物种的生态生理。基于水分耐受范围和生根深度的五个植物功能组(PFG)用于阐明植物蒸腾作用与地下水条件的相互作用过程。 ET通量速率曲线设定了消光和饱和消光深度,并定义了该组的ET通量速率是地下水位相对于地面深度的函数。从河岸或湿地系统计算出的ET损失取决于存在的每种植物功能亚组的贡献面积和地下水位状况。新方法要求对地下水模型单元内存在的每个PFG进行部分覆盖,并允许更准确地分配地面高度。案例研究的模型结果表明,新方法和传统方法在预测的ET和随后的地下水深度方面存在显着差异。基于生理的蒸腾曲线与裸土/裸露水的传统线性曲线相结合,可以更准确地确定河岸ET,并改善流域规模的水预算。 PFG与新的RIP-ET软件包结合使用可在地下水与河岸/湿地栖息地条件之间建立明确的联系,并为更好地管理和恢复河岸和湿地系统提供了机会。 (c)2005 Elsevier B.V.保留所有权利。

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