A Comparison Between Field-Measured and Empirically Estimated Rock Mass Modulus Values

E. Lindenbach, Steve Dalton, R. Bearce, Gergo Arany
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Abstract

Rock mass modulus, also referred to as the deformation modulus, is an important input variable for any load-deformation analysis of a foundation, such as a finite-element analysis for a dam. As the representative volume of rock is increased the rock mass will appear weaker and more deformable due to the inclusion of more discontinuities. The rock mass modulus can be measured directly downhole with a variety of devices, such as a uniaxial or radial jacking rig, a flat jack, or more commonly, a dilatometer. Modulus values can be estimated indirectly using site-specific empirical relationships.This paper provides a comparison of field- and laboratory-derived rock mass modulus values in an effort to develop a range of likely parameters and evaluate data quality/confidence levels. The in-situ values were compared to values developed from eight commonly used empirical relationships. Results indicate that the dilatometer-measured and empirically estimated values are similar where the rock is massive and relatively intact but vary significantly where the rock is fractured or weathered. These significant variations appear to be related to how the rock deforms in unconfined/semi-confined conditions (i.e., failure occurs into open space).
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现场实测与经验估计岩体模量的比较
岩体模量,也称为变形模量,是任何基础荷载-变形分析的重要输入变量,例如大坝的有限元分析。随着岩体代表体积的增大,由于包含更多的不连续面,岩体会显得更弱,更容易变形。岩体模量可以通过多种设备直接在井下测量,例如单轴或径向千斤顶钻机、平面千斤顶,或者更常见的膨胀仪。模数值可以使用特定地点的经验关系间接估计。本文提供了现场和实验室导出的岩体模量值的比较,以开发一系列可能的参数并评估数据质量/置信度。将原位值与从八种常用经验关系中得出的值进行比较。结果表明,膨胀计测量值和经验估计值在岩石块状和相对完整的情况下是相似的,但在岩石破碎或风化的情况下差异很大。这些显著的变化似乎与岩石在非密闭/半密闭条件下的变形有关(即,破坏发生在开放空间)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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