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Engineering characteristics of sensitive marine clays - examples of clays in eastern Canada.

机译:敏感海洋粘土的工程特性-加拿大东部的粘土实例。

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摘要

Sensitive marine clay in Ottawa is a challenging soil for geotechnical engineers. This type of clay behaves differently than other soils in Canada or other parts of the world. They also have different engineering characteristic values in comparison to other clays. Cone penetration testing in sensitive marine clays is also different from that carried out in other soils. The misestimation of engineering characteristics from cone penetration testing can result. Temperature effects have been suspected as the reason for negative readings and erroneous estimations of engineering characteristics from cone penetration testing. Furthermore, the applicability of correlations between cone penetration test (CPT) results and engineering characteristics is ambiguous. Moreover, it is important that geotechnical engineers who need to work with these clays have background information on their engineering characteristics. This thesis provides comprehensive information on the engineering characteristics and behaviour of sensitive marine clays in Ottawa. This information will give key information to geotechnical engineers who are working with these clays on their behaviour. For the purpose of this research, fifteen sites in the Ottawa area are taken into consideration. These sites included alternative technical data from cone and standard penetration tests, undisturbed samples, field vanes, and shear wave velocity measurements. Laboratory testing carried out for these sites has resulted in acquiring engineering parameters of the marine clay, such as preconsolidation pressure, overconsolidation ratio, compression and recompression indexes, secondary compression index, coefficient of consolidation, hydraulic conductivity, clay fraction, porewater chemistry, specific gravity, plasticity, moisture content, unit weight, void ratio, and porosity. This thesis also discusses other characteristics of sensitive marine clays in Ottawa, such as their activity, sensitivity, structure, interface shear behaviour, and origin and sedimentation. Furthermore, for the purpose of increasing local experience with the use of cone and ball penetrometers in sensitive marine clays in Ottawa, three types of penetrometer tips are used in the Canadian Geotechnical Research Site No. 1 located in south-west Ottawa: 36 mm cone tip, and 40 mm and 113 mm ball tips. The differences in their response in sensitive marine clays will be discussed. The temperature effects on the penetrometer equipment are also studied. The differences in the effect of temperature on these tips are discussed. Correlations between the penetrometer results and engineering characteristics of Ottawa's clays are verified. The applicability of correlations between the testing results and engineering characteristics of sensitive marine clays in Ottawa is also presented in this thesis. Two correlations from the Canadian Foundation Engineering Manual are examined. One of these correlations is between the N60 values from standard penetration testing and undrained shear strength. The other correlation is between the shear wave velocity measurement and site class. Temperature corrections are suggested and discussed for penetrometer equipment according to laboratory calibrations. The significance of the effects due to radical temperature changes in Canada and Ottawa is discussed. Some of the main findings from this research are as follows. • The Canadian Foundation Engineering Manual presents a correlation between standard penetration tests (SPTs) and the undrained shear strength of soils. This relationship may not be applicable to sensitive marine clays in Ottawa. • Another correlation between the site class, shear wave velocity, and undrained shear strength is presented by this same manual which may not be applicable to sensitive marine clays in Ottawa. • The rotation rate for field vane testing as recommended by ASTM D2573 is slow for sensitive marine clays in Ottawa. • Correction factors applied to undrained shear strength from laboratory vane tests may not result in comparable values with the undrained shear strength obtained by using field vane tests. • Loading schemes in consolidation or oedometer testing may affect the quality of the targeted results. • Temperature corrections should be applied to penetrometer recordings to compensate for the drift in the results of these recordings due to temperature changes. • The secondary compression index to compression index ratio presented in the literature may not be the value obtained from this research.
机译:渥太华的敏感海洋粘土对岩土工程师而言是充满挑战的土壤。这种类型的粘土的行为与加拿大或世界其他地区的其他土壤不同。与其他粘土相比,它们还具有不同的工程特性值。敏感海洋粘土中的锥孔渗透测试也不同于其他土壤中的锥孔渗透测试。可能会根据锥孔穿透测试对工程特性进行错误估计。人们已经怀疑温度效应是造成锥度渗透测试结果为负读数和错误估计工程特性的原因。此外,锥体渗透测试(CPT)结果与工程特性之间的相关性的适用性还不清楚。此外,重要的是需要使用这些粘土的岩土工程师必须具备有关其工程特性的背景信息。本文提供了有关渥太华敏感海洋粘土的工程特性和性能的综合信息。该信息将为使用粘土的行为的岩土工程师提供关键信息。为了本研究的目的,考虑了渥太华地区的十五个地点。这些站点包括来自锥形和标准穿透测试,未受干扰的样本,现场叶片和剪切波速度测量的替代技术数据。在这些地点进行的实验室测试导致获得了海洋黏土的工程参数,例如预固结压力,超固结比,压缩和再压缩指数,二次压缩指数,固结系数,水力传导率,黏土分数,孔隙水化学,比重,可塑性,水分含量,单位重量,空隙率和孔隙率。本文还讨论了渥太华敏感海洋粘土的其他特征,例如它们的活性,敏感性,结构,界面剪切行为以及成因和沉积。此外,为了增加本地经验,在渥太华的敏感海洋粘土中使用锥形和球形渗透仪,在位于渥太华西南的加拿大第一岩土工程研究站点中使用了三种类型的渗透仪尖端:36 mm锥尖端,以及40毫米和113毫米的球形尖端。将讨论它们在敏感海洋粘土中反应的差异。还研究了温度对渗透仪设备的影响。讨论了温度对这些吸头的影响。渗透度仪结果与渥太华粘土的工程特性之间的相关性得到了验证。本文还提出了渥太华敏感海相粘土的检测结果与工程特性之间的相关性适用性。检查了《加拿大基础工程手册》中的两个相关性。这些相关性之一是标准渗透测试的N60值与不排水的剪切强度之间的关系。另一个相关性是在剪切波速度测量值和地点类别之间。建议并讨论了根据实验室校准对渗透仪设备进行的温度校正。讨论了加拿大和渥太华因温度急剧变化而产生的影响的重要性。这项研究的一些主要发现如下。 •《加拿大基础工程手册》介绍了标准渗透试验(SPT)与土壤不排水的抗剪强度之间的相关性。这种关系可能不适用于渥太华的敏感海洋粘土。 •该手册还提供了场地类别,剪切波速度和不排水抗剪强度之间的另一种相关性,可能不适用于渥太华的敏感海相粘土。 •对于渥太华的敏感海洋粘土,ASTM D2573建议的现场叶片测试的旋转速度较慢。 •用于实验室叶片测试的不排水抗剪强度的校正系数可能无法获得与使用现场叶片测试获得的不排水抗剪强度相当的值。 •合并或里程表测试中的加载方案可能会影响目标结果的质量。 •应该对渗透计的记录进行温度校正,以补偿由于温度变化而导致记录结果的漂移。 •文献中提出的二次压缩指数与压缩指数之比可能不是从本研究中获得的值。

著录项

  • 作者

    Nader, Athir.;

  • 作者单位

    University of Ottawa (Canada).;

  • 授予单位 University of Ottawa (Canada).;
  • 学科 Engineering Civil.
  • 学位 M.A.Sc.
  • 年度 2014
  • 页码 0 p.
  • 总页数
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

  • 入库时间 2022-08-17 11:54:01

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