Pavement thickness and stabilised foundation layer assessment using ground-coupled GPR

被引:26
作者
Hu, Jinhui [1 ]
Vennapusa, Pavana K. R. [1 ]
White, David J. [1 ]
Beresnev, Igor [2 ]
机构
[1] Iowa State Univ, Dept Civil Construct & Environm Engn, Ames, IA 50011 USA
[2] Iowa State Univ, Dept Geol & Atmospher Sci, Ames, IA USA
关键词
Ground penetrating radar; dielectric constant; asphalt pavement; layer thickness; moisture content; PENETRATING RADAR; QUALITY-ASSURANCE; ASPHALT PAVEMENTS; SOIL;
D O I
10.1080/10589759.2015.1111890
中图分类号
TB3 [工程材料学];
学科分类号
0805 ; 080502 ;
摘要
Experimental results from field and laboratory investigations using a ground-coupled ground penetrating radar (GPR), dielectric measurement, magnetic imaging tomography (MIT) and dynamic cone penetrometer (DCP) tests are presented. Dielectric properties of asphalt pavement and stabilised and unstabilised pavement foundation materials were evaluated in the laboratory in frozen and unfrozen conditions. Laboratory test results showed that dielectric properties of materials back-calculated from GPR in comparison to dielectric gauge measurements are strongly correlated and repeatable. For chemically stabilised materials, curing time affected the dielectric properties of the materials. Field tests were conducted on asphalt pavement test sections with different foundation materials (stabilised and unstabilised layers), drainage conditions and layer thicknesses. GPR and MIT results were used to determine asphalt layer thicknesses and were compared with measured core thicknesses, while GPR and DCP were used to assess foundation layer profiles. Asphalt thicknesses estimated from GPR showed an average error of about 11% using the dielectric gauge values as input. The average error reduced to about 4% when calibrated with cores thicknesses. MIT results showed thicknesses that are about 9% higher than estimated using GPR. Foundation layer thicknesses could not be measured using GPR due to variations in moisture conditions between the test sections, which is partly attributed to variations in gradation and drainage characteristics of the subbase layer.
引用
收藏
页码:267 / 287
页数:21
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