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首页> 外文期刊>Journal of Hydrology >Determining the extent of groundwater interference on the performance of infiltration trenches
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Determining the extent of groundwater interference on the performance of infiltration trenches

机译:确定地下水对渗透沟性能的干扰程度

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Infiltration trenches are widely used in stormwater management, but their capacity decreases when installed in areas with shallow groundwater where infiltration is limited by groundwater drainage. Here the hydrological performance of single infiltration trenches in areas with shallow water tables is quantified in terms of their capability to reduce peak flow, peak volume and annual stormwater runoff volume. To simulate the long term hydrological performance of infiltration trenches two different models are employed. The models continuously simulate infiltration rates from infiltration trenches using a 19 year rainfall time series from Copenhagen as input. The annual and single event stormwater runoff reduction from infiltration trenches was determined for 9 different scenarios that covered different soil conditions and infiltration trench dimensions. Monte Carlo simulations were used in order to quantify the impact of parameter variability for each scenario. Statistical analysis of the continuous long term model simulations was used to quantify the hydrological performance of infiltration trenches. Results show that infiltration trenches are affected by groundwater when there is an unsaturated depth of less than 1.5-3 m in sandy loam, 6.5-8 m in silt loam and 11-12 m in silty clay loam. A correction factor that can be applied for infiltration trench design when there is a shallow groundwater table is presented. The analyses showed that below a certain value of unsaturated depth the dissipation capacity of the mound/ground-water becomes the dominant process determining the infiltration capacity from infiltration trenches. In these cases it is essential to consider the local groundwater conditions in the infiltration trench design process. (C) 2015 Elsevier B.V. All rights reserved.
机译:渗透沟在雨水管理中被广泛使用,但是当其安装在地下水较浅的地区时,其容量会下降,这些地区的渗透受到地下水排泄的限制。在这里,浅渗水区的单个入渗沟的水文性能通过减少峰值流量,峰值量和年度雨水径流量的能力来量化。为了模拟入渗沟的长期水文性能,采用了两种不同的模型。这些模型使用来自哥本哈根的19年降雨时间序列作为输入,连续模拟入渗沟的入渗率。针对覆盖不同土壤条件和渗透沟尺寸的9种不同情况,确定了渗透沟每年和单事件雨水径流的减少量。为了量化每种情况下参数可变性的影响,使用了蒙特卡洛模拟。连续长期模型模拟的统计分析用于量化入渗沟的水文性能。结果表明,当沙质壤土的非饱和深度小于1.5-3 m,粉质壤土为6.5-8 m,粉质粘土壤土为11-12 m时,入渗沟受到地下水的影响。提出了一种在地下水位浅的情况下可用于渗透沟设计的校正因子。分析表明,在一定的非饱和深度以下,土墩/地下水的消散能力成为决定渗透沟的渗透能力的主要过程。在这些情况下,在渗透沟设计过程中必须考虑当地的地下水条件。 (C)2015 Elsevier B.V.保留所有权利。

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