An attempt at soil profiling on a river embankment using geophysical data*
Toru Takahashi 1 3 Tsuyoshi Yamamoto 21 Fukada Geological Institute, 2-13-12 Honkomagome, Bunkyo-ku, Tokyo 113-0021, Japan.
2 Kinki Regional Development Bureau, Ministry of Land, Infrastructure, Transport and Tourism, Osaka Godochosha, Bldg. No. 1, 1-5-44, Otemae, Chuo-ku, Osaka 540-8586, Japan.
3 Corresponding author. Email: takahashi@fgi.or.jp
Exploration Geophysics 41(1) 102-108 https://doi.org/10.1071/EG09049
Submitted: 10 September 2009 Accepted: 27 November 2009 Published: 19 February 2010
Abstract
The internal structure of a river embankment must be delineated as part of investigations to evaluate its safety. Geophysical methods can be most effective means for that purpose, if they are used together with geotechnical methods such as the cone penetration test (CPT) and drilling. Since the dyke body and subsoil in general consist of material with a wide range of grain size, the properties and stratification of the soil must be accurately estimated to predict the mechanical stability and water infiltration in the river embankment. The strength and water content of the levee soil are also parameters required for such prediction. These parameters are usually estimated from CPT data, drilled core samples and laboratory tests. In this study we attempt to utilise geophysical data to estimate these parameters more effectively for very long river embankments. S-wave velocity and resistivity of the levee soils obtained with geophysical surveys are used to classify the soils. The classification is based on a physical soil model, called the unconsolidated sand model. Using this model, a soil profile along the river embankment is constructed from S-wave velocity and resistivity profiles. The soil profile thus obtained has been verified by geotechnical logs, which proves its usefulness for investigation of a river embankment.
Key words: geophysical data, resistivity, river embankment, S-wave velocity, soil profiling, unconsolidated sand model.
Acknowledgments
The data used in this study were acquired in the research project ‘Study on geophysical methods and instruments for investigation of river embankments’ by Kinki Technical Office, Kinki Regional Development Bureau, MLIT, being supervised by the Kyoto University River Embankment Research Consortium chaired by Professor Yuzuru Ashida.
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* *Part of this paper was presented at the 9th SEGJ International Symposium (2009).