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Seismic Site Characterization in Support of Drilled Shaft Design in Southern Nevada

机译:内华达州南部钻探井设计的地震现场表征

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In advance of conducting drilled-shaft load testing for a highway interchange in Las Vegas, Nevada, the site investigations have included borehole-based soil sampling and logging, standard penetration testing, and both surface-based and downhole seismic testing. Sediments in the area tend to be dense, deep, and sporadically carbonate-cemented. Locally measured velocities are significantly higher than global expectations for the same sediment types. The measured shear-wave velocity profiles fit local expectations in the dry zone (the upper 14 meters) and in the presence of secondary carbonate cementation. For wet, uncemented media, velocities are closer to global-reference velocities. Compression-wave velocities indicate depth to moist soil, which reaches well above the observed groundwater table. Correlation of shear-wave velocity to blow count is weak. The measurements will be compared with data from O-Cell™ (Osterberg Method) load tests of co-located drilled shafts, with the end goal of improving abilities to predict the capacity of drilled shafts in the Las Vegas area using site characteristics that are readily measured in situ.
机译:在对内华达州拉斯维加斯的高速公路立交进行钻探井轴载荷测试之前,现场调查包括基于钻孔的土壤采样和测井,标准穿透测试以及基于地面和井下的地震测试。该地区的沉积物往往是致密,深沉的,偶有碳酸盐胶结物。对于相同的沉积物类型,本地测量的速度显着高于全球预期。测得的剪切波速度曲线符合干旱地区(上部14米)和存在次级碳酸盐胶结作用的局部预期。对于湿的,未胶结的介质,速度更接近于全局参考速度。压缩波的速度表示到潮湿土壤的深度,该深度远高于所观测的地下水位。横波速度与打击次数的相关性较弱。将该测量结果与来自同位置钻探井的O-Cell™(奥斯特伯格法)载荷测试的数据进行比较,最终目标是提高使用现场特征的能力来预测拉斯维加斯地区钻探井的能力原位测量。

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