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CLEARWATER DAMFOUNDATION DRILLING AND GROUTING FOR REPAIR OF SINKHOLE ONUPSTREAM EMBANKMENT

机译:清水大坝基础钻孔和灌浆修复上游堤岸的渗漏

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摘要

Clearwater Dam, located in Southeast Missouri, experienced a sinkhole on the face of thernupstream embankment on 14 January 2003. The sinkhole appeared approximately 8 monthsrnafter the dam experienced a pool of record in May 2002.rnThe presentation will begin with a brief discussion of the dolomite karstic geology, the tworntypical zoned embankment sections, which comprise 2000 feet of the dam on the left abutmentrnridge (average height of 35 feet), and the 2300 feet of dam in the river valley (average heightrnof 170 feet) and the seepage history at Clearwater Dam, which was initially impounded inrn1948. Throughout the history of the dam, the left abutment ridge and the leftrnabutment/embankment contact was the focal point of seepage and the major cause ofrnconcern. On 14 January 2003, a sinkhole formed in the valley section of the embankment, onrnthe upstream face of the pervious shell, causing concern that the entire dam may bernexperiencing unacceptable seepage distress.rnThe presentation covers the emergency response to the sinkhole discovery and initialrnassessment of risk and consequences of dam failure. Geophysical investigations performedrn(Feb 2003) on the upstream face of the dam are discussed to infer embankment andrnfoundation material damage relative to depth and position from the sinkhole surface. The usernof the Sonic drilling method to investigate the foundation of the dam (March 2003) and therndownhole geophysical tests performed utilizing these boreholes (May 2003) will be discussed.rnOriginal construction photographs are presented of geological features, which may haverncontributed to sinkhole development.rnIn December 2003, a drilling investigation and grouting program was begun to provide arnlocalized repair of the foundation rock in the vicinity of the sinkhole (200 feet either side of thernsinkhole). The Sonic drilling method is being used to advance the boreholes through thernpervious shell and the clay core of the embankment. During the investigation process, in-siturnfalling head tests and low pressure hydraulic testing will be performed to determine thernintegrity of the embankment/foundation rock contact. A detailed discussion will present thernfindings of the computerized grouting program performed in the top 50 feet of the foundationrnrock. The presentation will conclude with a brief discussion of the long-term solutionsrnconsidered for the seepage problem.
机译:位于密苏里州东南部的克利尔沃特水坝于2003年1月14日在上游河堤上遇到了一个深水坑。在2002年5月大坝经历了一个记录池后约8个月,该深水坑才出现。本演讲将首先对白云石进行简要讨论。岩溶地质,两个典型的带状路堤部分,包括左桥台上的2000英尺大坝(平均高度为35英尺)和河谷的2300英尺大坝(平均高度为170英尺)以及克利尔沃特的渗流历史大坝,最初于1948年被扣押。在大坝的整个历史中,左基台脊和左基台/路堤接触是渗流的焦点,也是引起关注的主要原因。 2003年1月14日,在堤坝谷部,透水壳的上游面形成了一个污水坑,引起了人们对整个大坝可能遭受不可接受的渗流困扰的担忧.rn该报告涵盖了对污水坑发现和对风险的初步评估的应急措施。和大坝破坏的后果。讨论了在大坝上游面进行的地球物理调查(2003年2月),以推断路堤和地基材料相对于从沉孔表面的深度和位置的破坏。将讨论使用声波钻探方法研究大坝基础的用户(2003年3月)和使用这些钻孔进行的地下地球物理测试(2003年5月)。提供了一些原始地质构造照片,这些地质特征可能对下沉孔的发展做出了贡献。 2003年12月,开始进行钻探调查和注浆程序,以对下沉孔附近(下沉孔两侧200英尺)的基础岩石进行局部定位修复。声波钻探方法正被用于使钻孔穿过可渗透的壳层和路堤的粘土芯。在调查过程中,将进行倾覆式水头测试和低压水力测试,以确定路堤/基础岩石接触的完整性。详细的讨论将介绍在基岩顶部50英尺处执行的计算机注浆程序的发现。演讲的结尾将简要讨论针对渗流问题的长期解决方案。

著录项

  • 来源
    《Dam safety 2004》|2004年|1-13|共13页
  • 会议地点 Phoenix AZ(US);Phoenix AZ(US)
  • 作者

    Mark Harris; Leroy Arnold;

  • 作者单位

    U.S. Army Corps of Engineers, Little Rock District;

    U.S. Army Corps of Engineers, Little Rock District;

  • 会议组织
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

  • 入库时间 2022-08-26 14:27:33

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