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Three Mile Dam Preliminary Slope Stability Analysis

机译:三英里水坝初步边坡稳定性分析

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The Three Mile Dam is a privately owned high hazard embankment dam located northwest of Helena, Montana. The height of the dam is 63 feet and the crest of the dam is 450 feet long. The Three Mile Dam was originally a railroad embankment built in the late 1800s. Around 1927, long after the railroad had been abandoned, the embankment over Three Mile creek was converted to a dam for the purpose of irrigation. Static and seismic analysis was performed on the upstream and downstream slopes of the dam to determine the dam's stability.rnThe stability analysis was done using the computer software SLIDE 5.0 from the Rocscience package. The embankment was tested using the Bishop method of slices. Given that minimal subsurface data are available on the dam it was hard to determine subsurface parameters to use in the SLIDE program. The dam is built on a shale bed dipping to the southwest. The geological materials of the dam had to be determined using soil samples from the surface of the dam. Field developed cross-sections were also used in the determining the slope stability. The embankment stability was calculated at high and low reservoir conditions. At low reservoir static conditions both the upstream and downstream faces of the dam were stable. However, at high reservoir conditions the downstream face of the dam was determined to be potentially unstable as shown in Figures 4 and 5. Seismic conditions were based upon peak acceleration of seismic shaking in the area. Models run on the stability under these conditions also displayed instability in the embankment on both the upstream and downstream sides.rnMany assumptions had to be made, in computing the slope stability of the dam, due to insufficient data. More investigations are necessary to get a more accurate picture of the stability of this dam. Information on the subsurface geology in the dam is crucial to getting more accurate numbers on the factors of safety. Knowing the subsurface geology will also help in seepage analysis. More data would allow for less conservative assumptions and could potentially prove that the dam is stable under current conditions.
机译:三英里大坝是位于蒙大拿州海伦娜西北的私人高危堤防大坝。大坝的高度为63英尺,大坝的顶部为450英尺长。三英里水坝最初是建于1800年代后期的铁路路堤。 1927年左右,在铁路被废弃很久之后,三英里河的堤防被改建为大坝,用于灌溉。在大坝的上游和下游边坡进行了静力和地震分析,以确定大坝的稳定性。rnRoc使用Rocscience软件包中的SLIDE 5.0计算机软件进行了稳定性分析。使用Bishop切片法对路堤进行了测试。鉴于大坝上只有很少的地下数据,因此很难确定要在SLIDE程序中使用的地下参数。该水坝建在向西南倾斜的页岩层上。大坝的地质材料必须使用大坝表面的土壤样品来确定。现场开发的横截面也用于确定边坡稳定性。计算了高低储层条件下的路堤稳定性。在低水库静态条件下,大坝的上游和下游面都是稳定的。但是,在高水库条件下,如图4和5所示,确定大坝的下游面可能不稳定。地震条件是基于该地区地震震动的峰值加速度。在这些条件下以稳定度运行的模型在上游和下游侧的路堤上也显示出不稳定性。由于数据不足,在计算大坝的边坡稳定性时必须做出许多假设。为了更准确地了解该大坝的稳定性,需要进行更多的调查。大坝地下地质信息对于获取有关安全因素的更准确数字至关重要。了解地下地质也将有助于渗流分析。更多数据可以减少保守的假设,并有可能证明大坝在当前条件下是稳定的。

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