首页> 外文会议>International Conference on Site Characterization(ICS-2) vol.2; 20040919-22; Porto(PT) >A brief study of the repeatability of in-situ tests at the Florida Department of Transportation deep foundations research site in Orlando, Florida, USA
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A brief study of the repeatability of in-situ tests at the Florida Department of Transportation deep foundations research site in Orlando, Florida, USA

机译:在美国佛罗里达州奥兰多市的佛罗里达交通运输部深层基础研究现场,对原位测试的可重复性进行了简要研究

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摘要

An experimental test site located at the University of Central Florida, Orlando was established for deep foundation engineering research. An initial site characterization program was performed in January and February of 2002. The scope of work included fourteen cone penetration tests, two miniature cone penetration tests, four dilatometer tests, and six standard penetration tests. Qualitative comparisons among cone penetration test and dilatometer test soundings using three different agencies revealed consistent results with little variation between agencies, respective to test. The results of the standard penetration test program were less conclusive because of compounding variables including hammer type, hole type, operator, and limited testing. Considerable difference was observed between drillers at the same site regardless of equipment. However, these isolated results support the argument that the cone penetration and dilatometer tests are more repeatable than the standard penetration test. Based on the exploration program an initial generalized soil profile was established: 1) 0-1.5 m. medium sand, 2) 1.5-10 m sand-silty sand, 3) 10-15.8 m silty clay-clay, and 4) 15.8-18.3 m medium cemented sand. From the center eastward a hard pan sand layer existed from about 3 to 4.5 m.
机译:建立了一个位于奥兰多中央佛罗里达大学的实验测试站点,用于深层基础工程研究。在2002年1月和2002年2月执行了初始站点表征程序。工作范围包括14个圆锥体渗透测试,2个微型圆锥体渗透测试,4个膨胀计测试和6个标准渗透测试。使用三个不同的机构对锥孔穿透测试和膨胀计测试测深进行定性比较,结果显示一致的结果,各测试机构之间的变化很小。由于包括锤子类型,孔类型,操作员和有限测试在内的复合变量,标准渗透测试程序的结果不太确定。不论设备如何,在同一地点的司钻之间都观察到了很大的差异。但是,这些孤立的结果支持这样的论点,即圆锥体穿透和膨胀计测试比标准穿透测试更具可重复性。根据勘探计划,初步建立了广义的土壤剖面:1)0-1.5 m。中型砂; 2)1.5-10 m的粉质砂,3)10-15.8 m的粉质粘土,以及4)15.8-18.3 m的中型胶结砂。从中心向东存在约3至4.5 m的硬盘沙层。

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