确定采用生物滞留池的斜坡的水文地质过程的特征

IF 3.2 3区 地球科学 Q1 Environmental Science Hydrological Processes Pub Date : 2024-08-27 DOI:10.1002/hyp.15268
Boji Chen, Ting Fong May Chui
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引用次数: 0

摘要

由于人们担心低影响开发(LID)方法的水文性能差以及对斜坡稳定性的潜在影响,因此很少在斜坡上实施这种方法。在斜坡上实施低影响开发(LID),涉及到改变地表地形和地下水文(特别是形成地下水丘),会给保持斜坡稳定性带来挑战。然而,斜坡地区往往需要采用 LIDs 来实现可持续发展。必须对传统设计标准进行补充,以应对这些挑战。在提出具体解决方案之前,应首先了解 LID 对斜坡稳定性的影响。这包括量化 LID 实施前后斜坡稳定性的变化程度,以及确定影响稳定性的关键因素。为了解决这些问题,我们在 HYDRUS-2D 中开发了一个数值模型,用于模拟采用两阶生物蓄渗池 (BC) 系统的斜坡的水文和岩土过程。利用美国俄亥俄州辛辛那提市一个阶梯式生物蓄水池的监测数据对数值模型进行了校准和验证。模拟场景包括三个一般坡角(15°、20° 和 25°)、两个地下水位初始位置和两个流入量。水文过程以地下水丘的演变为特征,岩土过程则使用安全系数(FoS)进行量化。我们的研究结果表明,当安全系数(FoS)增加 0.1 时,削坡和填土可能会增强稳定性。然而,地下水渗出形成的地下水丘会导致安全系数降低约 0.1-0.2,具体取决于流入量。随后的地下水丘演变对稳定性没有进一步影响。最终,在切割和填土作业以及地下水丘的共同作用下,FoS 略微降低了约 0-0.1。在坡度为 15° 的斜坡上采用低能耗设计一般是安全的。对于较陡的斜坡,设计时必须考虑特殊因素,例如减少排水面积,以在水文性能和斜坡安全之间取得平衡。
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Characterizing hydro-geotechnical processes of slopes implemented with bioretention cells

Low impact development (LID) practices are rarely implemented on slopes due to concerns about their poor hydrological performance and the potential impact on slope stability. Implementing LIDs on slopes, involving alterations to surface topography and subsurface hydrology (specifically, the formation of a groundwater mound), can pose challenges in maintaining slope stability. However, sloping areas often require LIDs for sustainable development. It is imperative to supplement the conventional design standard to address these challenges. Before proposing specific solutions, the impact of LIDs on slope stability should be understood first. This includes quantifying the extent of changes in slope stability before and after LID implementation, as well as identifying the key factors that influence stability. To address these, we developed a numerical model in HYDRUS-2D to simulate the hydrological and geotechnical processes of slopes implemented with a two-stepped bioretention cell (BC) system. The numerical model was calibrated and validated using monitoring data from a stepped BC in Cincinnati, Ohio, USA. Simulation scenarios encompassed three generic slope angles (15°, 20°, and 25°) with and without BCs, two initial groundwater table positions and two inflow volumes. The hydrological process was characterized by the evolution of the groundwater mound, and the geotechnical process was quantified using the factor of safety (FoS). Our findings indicated slope cutting and filling was likely to enhance stability with an increase in the FoS of 0.1. However, the formation of groundwater mounds, resulting from exfiltration, led to an approximate 0.1–0.2 reduction in the FoS, depending on the inflow volume. The subsequent groundwater mound evolution had no further impact on stability. Ultimately, the FoS was slightly reduced by around 0–0.1 due to the combined effect of cutting and filling operations and groundwater mounds. It was generally safe to implement LIDs on 15° slopes. For steeper slopes, special design considerations are necessary, such as reducing the drainage area to strike a balance between hydrological performance and slope safety.

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来源期刊
Hydrological Processes
Hydrological Processes 环境科学-水资源
CiteScore
6.00
自引率
12.50%
发文量
313
审稿时长
2-4 weeks
期刊介绍: Hydrological Processes is an international journal that publishes original scientific papers advancing understanding of the mechanisms underlying the movement and storage of water in the environment, and the interaction of water with geological, biogeochemical, atmospheric and ecological systems. Not all papers related to water resources are appropriate for submission to this journal; rather we seek papers that clearly articulate the role(s) of hydrological processes.
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