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Stream Bank Remediation; Not Just a Geotechnical Problem

机译:流库修复;不只是岩土问题

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Slope failures along stream banks are caused by a combination of unfavorable conditions. Geotechnical engineers often focus on soils and groundwater issues and develop remedial schemes that are derived from a two dimensional stability analysis without giving due consideration to geologic conditions. Remedial solutions that do not account for stream dynamics may not have the anticipated life cycle and may exacerbate erosion upstream and downstream of the site under repair. Remedial solutions that consider the stream dynamics improve the slope stability and can be applied in an ecologically friendly manner. This paper presents two case histories that illustrate the geotechnical and geomorphic causes of slope failures along streams. For one case history, geotechnical issues, such as weak soils, steep slopes, high groundwater levels, and poor drainage, are the predominant causes of the slope instability. For the second case history, stream dynamics, particularly erosion of the slope's toe, caused the slopes to fail. The case histories illustrate how remedial methods are developed to address both the geotechnical and geomorphic issues. This includes traditional methods to improve geotechnical conditions and some non-traditional methods such as using the dry-mix method to improve the strength of soft sensitive clay soil. Remedial methods to address the stream conditions include measures such as river training, bank armoring, and revegetation.
机译:沿河堤岸的斜坡破坏是由多种不利条件共同造成的。岩土工程师经常关注土壤和地下水问题,并制定了从二维稳定性分析中得出的补救方案,而没有适当考虑地质条件。不考虑水流动力学的补救解决方案可能没有预期的生命周期,并且可能加剧维修地点上游和下游的侵蚀。考虑水流动力学的补救方案可以改善边坡的稳定性,并且可以以生态友好的方式加以应用。本文介绍了两个案例历史,说明了沿河道边坡破坏的岩土工程和地貌原因。在一个案例中,土质问题,例如土壤薄弱,斜坡陡峭,地下水位高和排水不良,是导致斜坡失稳的主要原因。对于第二个案例历史,流动力学,特别是斜坡脚趾的侵蚀,导致斜坡失效。案例历史说明了如何开发补救方法来解决岩土工程和地貌问题。这包括改善土工条件的传统方法和一些非传统方法,例如使用干混法来改善软敏感粘土的强度。解决溪流状况的补救方法包括采取措施,例如河道整治,河岸装甲和植被恢复。

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