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A New Setup for Measuring G_o during Laboratory Compaction

机译:在实验室压实过程中测量G_o的新设置

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Soil stabilization by compaction plays an important role in foundation engineering, both for construction and maintenance. Compaction specifications often require achievement of an in situ dry density (ρ_d) of 90-95 % of the maximum value obtained from laboratory standard or modified Proctor test. However, ρ_d is not a design parameter per se; it is rather used to infer other parameters such as strength and stiffness through some empirical relationships. This paper describes a setup and procedure by which the small-strain (dynamic) shear stiffness can be measured accurately by propagating elastic shear wave through the stabilized material during laboratory compaction. The method enables measurement of the shear modulus [G_(o(ij))] in both horizontal and vertical planes. The ratio between G_o in these two orthogonal planes (i.e., G_(hh) and G_(hv)) is a measure of the degree of stiffness anisotropy, and this could be used as input parameter in deformation calculations. The setup is designed so that it can be readily incorporated into the familiar Proctor test.
机译:压实作用的土壤稳定作用在基础工程中对建筑和维护都起着重要作用。压实规范通常要求原位干密度(ρ_d)要达到实验室标准或改进的Proctor试验获得的最大值的90-95%。但是,ρ_d本身不是设计参数;而是通过一些经验关系来推断其他参数,例如强度和刚度。本文介绍了一种设置和过程,通过该过程和过程,可以在实验室压实过程中通过在稳定的材料中传播弹性剪切波,从而精确地测量小应变(动态)剪切刚度。该方法使得能够在水平和垂直平面上测量剪切模量[G_(o(ij))]。这两个正交平面中的G_o之比(即G_(hh)和G_(hv))是刚度各向异性程度的度量,可以用作变形计算中的输入参数。设计该安装程序的目的是可以轻松将其合并到熟悉的Proctor测试中。

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