Correlations between geotechnical and electrical data: A case study at Garchy in France

被引:125
作者
Cosenza, Philippe
Mannet, Enic
Rejiba, Faycal
Cui, Yu Jun
Tabbagh, Alain
Charlery, Yvelle
机构
[1] Univ Paris 06, UMR Sisyphe 7619, F-75252 Paris 05, France
[2] Univ Paris 06, Inst Sci & Technol, F-75252 Paris, France
[3] Inst Navier, ENPC LCPC, CERMES, Champs Sur Marne, France
关键词
geotechnical tests; electrical tomography; Ground Penetrating Radar; water content;
D O I
10.1016/j.jappgeo.2006.02.003
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Geophysical (Electrical Resistivity Tomography, Ground Penetrating Radar profiles and seismic refraction) and geotechnical (dynamic penetrometer, in situ vane test) surveys were carried out at Garchy (Nievre, France). The main objective of this study was to establish qualitative and quantitative correlations between electrical and geotechnical data from this site in a simple geological context. Concerning qualitative correlations, geotechnical tests and Electrical Resistivity Tomography sections are consistent with a three-layers model: a fine soil with a significant clay fraction sandwiched between a low moisture sandy soil and oolitic limestones. Despite the usual difficulty to locate clearly interfaces in inverted ERT sections, both methods provide consistent depths of the substratum top. Moreover, this study confirms that correlations between reflectors of GPR profiles and vertical geotechnical property variations are mainly explained by vertical water content changes. As far as quantitative correlations are concerned, no clear relationship between cone resistance and inverted resistivity extracted from ERT sections has been observed. Nevertheless, if we do not consider the upper sandy soil composed with gravels. the couple inverted resistivity-cone resistance would be a lithological discriminator. This lithological discrimination is enhanced when inverted resistivity values obtained from extracted 1D soundings are considered. This original result should be validated in other sites. Moreover, a satisfactory quantitative correlation between inverted resistivity values and measured water content values has been obtained; this correlation demonstrates once more that resistivity is a good indirect predictor of water content. (C) 2006 Elsevier B.V. All rights reserved.
引用
收藏
页码:165 / 178
页数:14
相关论文
共 20 条
[1]  
ABRAHAM O, 1998, 4 M ENV ENG GEOPH BA, P343
[2]   Vadose zone flow model parameterisation using cross-borehole radar and resistivity imaging [J].
Binley, A ;
Cassiani, G ;
Middleton, R ;
Winship, P .
JOURNAL OF HYDROLOGY, 2002, 267 (3-4) :147-159
[3]  
Braga ACO., 1999, J ENVIRON ENG GEOPH, V4, P123, DOI [10.4133/JEEG4.2.123, DOI 10.4133/JEEG4.2.123, 10.4133/jeeg4.2.123]
[4]  
Dannowski G., 1999, EUR J ENV ENG GEOPHY, V4, P71
[5]   OCCAM INVERSION TO GENERATE SMOOTH, 2-DIMENSIONAL MODELS FROM MAGNETOTELLURIC DATA [J].
DEGROOTHEDLIN, C ;
CONSTABLE, S .
GEOPHYSICS, 1990, 55 (12) :1613-1624
[6]  
DESTADELHOFEN CM, 1991, APPL GEOPHYS RECHERC
[7]   MODIFIED PSEUDO-SECTION FOR RESISTIVITY AND IP [J].
EDWARDS, LS .
GEOPHYSICS, 1977, 42 (05) :1020-1036
[8]  
ENDRES AL, 1998, S APPL GEOPH ENG ENV
[9]  
ENKATRAMAIAH, 1993, GEOTECHNICAL ENG
[10]  
Filliat G., 1981, PRATIQUE SOLS FONDAT