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Hydrologic experiments and modeling of two laboratory bioretention systems under different boundary conditions

机译:不同边界条件下两个实验室生物滞留系统的水文实验和建模

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Hydrologic performance of bioretention systems is significantly influenced by the media composition and underdrain configuration. This research measured hydrologic performance of column-scale bioretention systems during a synthetic design storm of 25.9 mm, assuming a system areaxatchment area ratio of 5%. The laboratory experiments involved two different engineered media and two different drainage configurations. Results show that the two engineered media with different sand aggregates were able to retain about 36% of the inflow volume with free drainage configuration. However, the medium with marine sand is better at delaying the occurrence of drainage than the one with pumice sand, denoting the better detention ability of the former. For both engineered media, an underdrain configuration with internal water storage (IWS) zone lowered drainage volume and peak drainage rate as well as delayed the occurrence of drainage and peak drainage rate, as compared to a free drainage configuration. The USEPA SWMM V5.1.11 model was applied for the free drainage configuration case, and there is a reasonable fit between observed and modeled drainage-rates when media-specific characteristics are available. For the IWS drainage configuration case, air entrapment was observed to occur in the engineered medium with marine sand. Filling of an IWS zone is most likely to be influenced by many factors, such as the structure of the bioretention system, medium physical and hydraulic properties, and inflow characteristics. More research is needed on the analysis and modeling of hydrologic process in bioretention with IWS drainage configuration.
机译:生物滞留系统的水文性能受介质组成和暗渠结构的影响很大。本研究在25.9 mm的合成设计风暴期间测量了柱级生物保留系统的水文性能,假设系统面积与汇水面积之比为5%。实验室实验涉及两种不同的工程介质和两种不同的排水配置。结果表明,两种具有不同砂粒聚集体的工程介质在自由排水的情况下能够保留大约36%的流入量。然而,与浮石砂相比,含海砂的介质在延缓排水的发生方面更好,表明前者的滞留能力更好。对于两种工程介质,与自由排水配置相比,带有内部储水(IWS)区域的地下排水配置降低了排水量和峰值排水速率,并延迟了排水和峰值排水速率的发生。 USEPA SWMM V5.1.11模型适用于自由排水配置情况,并且当可获得特定于介质的特性时,观测到的排水速率与模型排水速率之间存在合理的拟合。对于IWS排水配置情况,观察到夹带海砂的工程介质中发生了空气夹带。 IWS区域的填充最有可能受到许多因素的影响,例如生物保留系统的结构,介质的物理和水力性质以及流入特征。 IWS排水配置的生物滞留过程中的水文过程分析和建模需要更多的研究。

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