Near-surface water content measurement by Ground Penetrating Radar
The measurement of the near-surface water content is very important for engineering and environmental application. Ground penetrating radar (GPR) is a very effective tool for near-surface water content measurement. The corresponding principle was outlined. An important step is to calculate the interval velocity by velocity analysis method for common middle-point (CMP) data, then dielectric converted from the velocity is used to calculate the water content by Topps formula. A local aquifer constant model was established to check the method. A Finite-Difference Time-Domain (FDTD)method was used to simulate the GPR response for the designed local aquifer model. The synthetic CMP data were used calculated the 2-dimensional water content distribution. The calculated results reveal the model well.
Ground penetrating radar Local aquifer Velocity analysis Near-surface water content
LIU Sixin WANG Chunhui ZENG Zhaofa LU Qi WANG Zhejiang YI Bing
Department of Geophysics, Jilin University, Changchun,China The Institute of Hydrogeology and Engineering Technique, CGS, Baoding,China
国际会议
The 19th International Workshop on Electromagnetic Induction in the Earth(第十九届国际地球电磁感应学术研讨会)
北京
英文
7-12
2008-10-23(万方平台首次上网日期,不代表论文的发表时间)