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Crosshole seismic methods to assess the seismic stability of earthen dams

机译:跨孔地震方法评估土坝的地震稳定性

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An in situ geophysical investigation consisting of crosshole and downhole shear wave (S-wave) and surface vibratory tests was performed at Sardis Dam, located on the Tallahatchie River in northwest Mississippi. Tests were conducted in a pile test section at the downstream toe of the dam. The purpose of the investigation was to determine changes in S-wave velocities, which are related to soil strength, in the test section due to pile driving activities. Comparison tests were conducted three times: prior to driving the piles, immediately after, and three months after the piles had been driven. The S-wave crosshole and surface vibratory tests indicated a significant velocity increase, averaging more than 20 percent, due to the driving of piles in the test section. Of the geophysical tests conducted, crosshole testing was the most sensitive in denoting velocity changes. The downhole S-wave test did not detect any significant velocity increases. The scope of this paper is limited to results of crosshole testing.
机译:在Sardis Dam在位于西北密西西比州的塔拉瓦特河上的Sardis Dam中进行了一种由十字孔和井下剪力波(S波)和表面振动试验组成的原位地球物理研究。在坝下游脚趾的桩试验部分中进行测试。调查的目的是确定由于桩驾驶活动而在试验部分中的S波速度的变化。比较试验进行三次:在驱动桩之前,立即在桩后三个月后。由于在试验部分中的桩驱动,S波十字孔和表面振动试验表明,平均速度增加,平均超过20%。在进行的地球物理测试的情况下,十字孔测试是表示速度变化最敏感的。井下S波试验未检测到任何显着的速度增加。本文的范围仅限于交叉孔测试的结果。

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