首页> 外文会议>2005年大坝安全与堤坝隐患探测国际学术研讨会(International Symposium on Dam Safety and Detection of Hidden Troubles of Dams and Dikes) >SEEPAGE AND STRAIN MONITORING IN EMBANKMENT DAMS USING DISTRIBUTED SENSING IN OPTICAL FIBRES-THEORETICAL BACKGROUND AND EXPERIENCES FROM SOME INSTALLATIONS IN SWEDEN
【24h】

SEEPAGE AND STRAIN MONITORING IN EMBANKMENT DAMS USING DISTRIBUTED SENSING IN OPTICAL FIBRES-THEORETICAL BACKGROUND AND EXPERIENCES FROM SOME INSTALLATIONS IN SWEDEN

机译:基于光纤的分布式传感的堤坝渗流和应变监测-理论背景和瑞典一些机构的经验

获取原文

摘要

Temperature measurement is probably the most sensitive geophysical method to detect and quantify seepage flow. The best application of the method is long term monitoring, where slow and small seepage flow changes can be detected. The sensibility is in the order of some 10-5m3/(s,m) for normal dams, but may be lower or higher depending on where the temperature is measured and local conditions. Temperature measurements in embankment dams started initially in Germany in 1957. Further improvements of the evaluation methodology were made in Sweden during the 1990-ties, when the fundamentals of thermal processes were studied. However, the acceptance and a general use of the method have been slow, but today it is getting more and more accepted. It has during the last five years been used as a standard tool at embankment dam investigations and monitoring in Sweden, and also in Germany. Until today, HydroResearch and Sensornet have installed optical fibres for monitoring of seepage and/or movements in more than 20 dams, dykes and tailing dams at 16 different dam sites in Sweden. Different installation techniques have been developed depending on the dam. These include embedding of the fibre inside the dam (at new constructions), in the crest during raising of a dam, within new toe berms at upgrading work, just downstream of the dam toe or vertically in standpipes. The experiences from field the measurements show that optical fibres installed along a dam toe will provide possibilities to both locate anomalous seepage areas and to estimate the seepage flow after short time investigations (normally some days). Longer measurements or repeated measurements will improve the detection capability and the accuracy of the seepage flow evaluations, and are therefore recommended.
机译:温度测量可能是检测和量化渗流的最灵敏的地球物理方法。该方法的最佳应用是长期监测,可以检测到缓慢而小的渗流变化。普通大坝的敏感度约为10-5m3 /(s,m),但可能更低或更高,具体取决于测量温度和当地条件。堤坝的温度测量最初于1957年在德国开始。在1990年代初期,对热过程的基础进行了研究,评估方法在瑞典得到了进一步的改进。但是,该方法的接受和普遍使用进展缓慢,但是今天它越来越被接受。在过去的五年中,它已被用作瑞典和德国堤坝调查和监测的标准工具。直到今天,HydroResearch和Sensornet都已安装了光纤,以监测瑞典16个不同水坝站点中20多个水坝,堤坝和尾矿坝的渗漏和/或运动。根据水坝的不同,已经开发出了不同的安装技术。这些措施包括将纤维嵌入坝内(在新建建筑物中),在坝上升期间在波峰中,在升级工作时在新的脚趾护堤中,紧靠坝脚趾的下游或垂直放置在立管中。现场测量的经验表明,沿着坝脚安装的光纤将提供定位异常渗流区域并在短时间调查后(通常为几天)估计渗流的可能性。较长的测量或重复的测量将提高检测能力和渗流评估的准确性,因此建议使用。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号