首页> 外文会议>Information technology in geo-engineering >Soil Compaction Characterizations through Electrical Resistivity in Field Investigations
【24h】

Soil Compaction Characterizations through Electrical Resistivity in Field Investigations

机译:在田间调查中通过电阻率对土壤压实进行表征

获取原文
获取原文并翻译 | 示例

摘要

This paper presents soil compaction characterizations in field using soil electrical resistivity. In roads and highway engineering, it is necessary to achieve the expected dry density of soil through field and laboratory tests. Conventional tests include the standard procedures like sand cone method, rubber balloon method and nuclear method are normally conducted at sites as compaction work is progressing. To achieve field dry density of 90 to 95 % of maximum dry density the samples are determined from standard proctor tests in laboratory. Conventional methods are costly and tedious when large number of soil samples are to be collected from field for tests. Measurements of moisture contents are obtained by drying process of moist soil excavated from sites. Soil resistivity method is used in this research to obtain soil dry density, particle size distributions and soil compaction characteristics in field investigations. High precision digital multimeter, Fluke 8846A and insulation tester, KEW 3111V are used to measure soil electric resistivity of compacted soils. Results of standard proctor tests for maximum dry density in laboratory are compared with the performance of field compaction characterizations using electrical resistivity. The main advantage of using soil resistivity method and computer database programming is the acquisition of immediate and hence reliable results where field tests data is consequently characterized using information stored in a computer database. Soil compaction characterizations using resistivity method show good agreement with conventional method of soil investigations conducted in geotechnical laboratory of Universiti Kebangsaan Malaysia (UKM).
机译:本文利用土壤电阻率介绍了田间土壤压实特征。在道路和公路工程中,有必要通过野外和实验室测试达到预期的土壤干密度。随着压实工作的进行,常规测试通常包括在现场进行诸如砂锥法,橡皮球法和核法等标准程序。为了达到最大干密度的90%到95%的田间干密度,样品是通过实验室的标准监理员测试确定的。当要从田间收集大量土壤样品进行测试时,常规方法既昂贵又乏味。水分含量的测量是通过对从现场挖出的潮湿土壤进行干燥处理而获得的。本研究采用土壤电阻率法获得田间调查的土壤干密度,粒径分布和土壤压实特性。高精度数字万用表Fluke 8846A和绝缘测试仪KEW 3111V用于测量压实土壤的土壤电阻率。将实验室中最大干密度的标准监理器测试结果与使用电阻率的现场压实特性进行了比较。使用土壤电阻率法和计算机数据库编程的主要优点是获得即时且因此可靠的结果,因此使用存储在计算机数据库中的信息来表征现场测试数据。使用电阻率法进行的土壤压实特性与在马来西亚马来西亚大学岩土工程实验室(UKM)的岩土实验室中进行的常规土壤调查方法显示出良好的一致性。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号