Time-lapse cross-hole electrical resistivity tomography monitoring effects of an urban tunnel

被引:24
|
作者
Bellmunt, F. [1 ]
Marcuello, A. [1 ]
Ledo, J. [1 ]
Queralt, P. [1 ]
Falgas, E. [1 ]
Benjumea, B. [2 ]
Velasco, V. [3 ,4 ]
Vazquez-Sune, E. [3 ]
机构
[1] Univ Barcelona, Dept Geodinam & Geofis, E-08028 Barcelona, Spain
[2] IGC, Barcelona 08006, Spain
[3] CSIC, IDAEA, Dept Geociencias, Barcelona 08034, Spain
[4] Univ Politecn Cataluna, GHS, Dept Ingn Geotecn & Geociencias, BarcelonaTech, ES-08034 Barcelona, Spain
关键词
Electrical resistivity tomography (ERT); Cross-hole apparent resistivity pseudosection; Tunnel boring machine; Experimental electrodes; BOREHOLE; SENSITIVITY; ZONE;
D O I
10.1016/j.jappgeo.2012.09.003
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Tunnel construction in urban areas has recently become a topic of interest and has increased the use of tunnel boring machines. Monitoring subsurface effects due to tunnel building in urban areas with conventional surface geophysical techniques is not an easy task because of space constraints. Taking advantage of the construction of a new metro line in Barcelona (Spain), a geoelectrical experiment, which included borehole logging and time-lapse cross-hole measurements using permanent electrode deployments, was designed to characterise and to study the subsurface effects of the tunnel drilling in a test site. We present a case study in which the differences between time-lapse cross-hole resistivity measurements acquired before, during and after the tunnel drilling below the test site have been calculated using three different procedures: a constrained time-lapse inversion, a model subtraction and an inversion of the normalised data ratio. The three procedures have provided satisfactory images of the resistivity changes and tunnel geometry, but resistivity changes for the tunnel void were lower than predicted by modelling. This behaviour has been explained by considering a conductive zone around the tunnel. Further, an apparent resistivity pseudosection for the cross-hole data, equivalent to the case of the equatorial dipole-dipole on the surface, is introduced. (C) 2012 Elsevier B.V. All rights reserved.
引用
收藏
页码:60 / 70
页数:11
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