APPLICATION OF 2D SURFACE ELECTRICAL RESISTIVITY TOMOGRAPHY TO DETECT THE UNDERGROUND CAVITIES A CASE SITE STUDY: TOLGA AREA (ALGERIA)
Résumé
Electrical resistivity tomography method is considered among the best non-destructive and non invasive geophysical techniques for detecting and characterizing the underground cavities and associated disorders. The detection of cavities in urban areas is important to prevent against different causes of accidents related to possible collapse and subsidence. This study focused on the application of electrical resistivity measurements to locate and identify cavities in the soil. The survey site is located in Biskra City, south-east of Algeria. This field contains cavities of natural origin and different sizes. The procedure using the electrical resistivity tomography of Wenner array permitted to detect the cavities in the range of depth 2 to 4m. These cavities were caused by the dissolution phenomena of carbonate materials. Also mechanical and dynamic penetrometer tests were performed in order to propose a solution for foundations building.Références
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[3] Fehdi C, Baali F, Boubaya D, Rouabhia A (2011) Detection of sinkholes using 2D electrical resistivity imaging in the Cheria Basin (north-east of Algeria). Arab J Geosci 4:181–187.
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[7] Muztaza NM, Mokhtar Saidin M, Shyeh SK, Saad, R (2012) 2D Resistivity Method to investigate an Archaeological Structure in Jeniang, Kedah, EJGE, 17:353-360.
[8] Martínez J, Benavente J, García-Aróstegui JL, Hidalgo MC, Rey J (2009) Contribution of electrical resistivity tomography to the study of detrital aquifers affected by seawater intrusion–extrusion effects: the river Vélez delta (Vélez-Málaga, southern Spain). Eng Geol 108:161–168.
[9] Šumanovac F (2006) Mapping of thin sandy aquifers by using high resolution reflection seismics and 2-D electrical tomography. J Appl Geophys 58:144–157.
[10] Al-fares. W, M. Bakalowicz, Y. Alboury, J.-M. Vouillamoz, M. Dukhan, G. Toe, R. Guerin, Contribution de la géophysique à l’étude d’un aquifère karstique – Exemple: le site karstique du Lamalou, 3e Colloque GEOFCAN, Orléans, 25–26 septembre 2001. Prospecting 44, 131–152.
[11] Park. G, Park. S, Yi. MJ, Rim. H, Cho. SJ, Kim JH (2010) Geostatistical integration using 2-D electrical resistivity and 3-D gravity methods for detecting cavities in a Karst area. Environ Earth Sci 60:965–974.
[12] El-Qady G, Hafez M, Abdalla MA, Ushijima K (2005) Imaging subsurface cavities using geoelectric tomography and ground-penetrating radar. J Cave Karst Stud 67:174–181.
[13] Dahlin T, Loke M (1998) Resolution of 2-D Wenner resistivity imaging as assessed by numerical modelling. J Appl Geophys 38:237–249
[14] Dahlin T, Zhou B (2004) A numerical comparison of 2D resistivity imaging with 10 electrode arrays. Geophys Prospect 52:379–398.
[15] Loke MH, Barker RD (1996) Rapid least-squares inversion of apparent resistivity pseudosections by a quasi-Newton method. Geophys Prospect 44:131–152.
[16] Griffiths DH, Barker RD (1993) Two-dimensional resistivity imaging and modeling in areas of complex geology. J Appl Geophys 29:211–226 .
[17] DeGroot-Hedlin C, Constable S (1990) Occam’s inversion to generate smooth, two-dimensional models from magnetotelluric data. Geophysics 55:1613–1624
[18] Sasaki Y (1992) Resolution of resistivity tomography inferred from numerical simulation. Geophys Prospect 40:453–4
[19] Edwards LS (1977) A modified pseudosection for resistivity and IP. Geophysics 42(5):1020–1036.
combinée géoélectrique–radar géologique des cavités souterraines de la ville de Zaouit Ech Cheikh (Maroc). CR Geosci 339:460–467.
[2] Emin U. U., and Irfan A., Detection of cavities in gypsum. JOURNAL On THE BALKAN. GEOPHYSICAL SOCIETY, Vol. 9, No. 1, December 2006, p. 8-19, 13 figs.
[3] Fehdi C, Baali F, Boubaya D, Rouabhia A (2011) Detection of sinkholes using 2D electrical resistivity imaging in the Cheria Basin (north-east of Algeria). Arab J Geosci 4:181–187.
[4] Metwaly M, AlFouzan F (2013) Application of 2-D geoelectrical resistivity tomography for subsurface cavity detection in the eastern part of Saudi Arabia. Geosci Front 4:469–476.
[5] Oldenburg DW, Y Li (1999) Estimating depth of investigation in DC resistivity and IP surveys, Geophysics, 64:403–416.
[6] Van Schoor M (2002) Detection of sinkholes using 2D electrical resistivity imaging. J Appl Geophys 50:393–399.
[7] Muztaza NM, Mokhtar Saidin M, Shyeh SK, Saad, R (2012) 2D Resistivity Method to investigate an Archaeological Structure in Jeniang, Kedah, EJGE, 17:353-360.
[8] Martínez J, Benavente J, García-Aróstegui JL, Hidalgo MC, Rey J (2009) Contribution of electrical resistivity tomography to the study of detrital aquifers affected by seawater intrusion–extrusion effects: the river Vélez delta (Vélez-Málaga, southern Spain). Eng Geol 108:161–168.
[9] Šumanovac F (2006) Mapping of thin sandy aquifers by using high resolution reflection seismics and 2-D electrical tomography. J Appl Geophys 58:144–157.
[10] Al-fares. W, M. Bakalowicz, Y. Alboury, J.-M. Vouillamoz, M. Dukhan, G. Toe, R. Guerin, Contribution de la géophysique à l’étude d’un aquifère karstique – Exemple: le site karstique du Lamalou, 3e Colloque GEOFCAN, Orléans, 25–26 septembre 2001. Prospecting 44, 131–152.
[11] Park. G, Park. S, Yi. MJ, Rim. H, Cho. SJ, Kim JH (2010) Geostatistical integration using 2-D electrical resistivity and 3-D gravity methods for detecting cavities in a Karst area. Environ Earth Sci 60:965–974.
[12] El-Qady G, Hafez M, Abdalla MA, Ushijima K (2005) Imaging subsurface cavities using geoelectric tomography and ground-penetrating radar. J Cave Karst Stud 67:174–181.
[13] Dahlin T, Loke M (1998) Resolution of 2-D Wenner resistivity imaging as assessed by numerical modelling. J Appl Geophys 38:237–249
[14] Dahlin T, Zhou B (2004) A numerical comparison of 2D resistivity imaging with 10 electrode arrays. Geophys Prospect 52:379–398.
[15] Loke MH, Barker RD (1996) Rapid least-squares inversion of apparent resistivity pseudosections by a quasi-Newton method. Geophys Prospect 44:131–152.
[16] Griffiths DH, Barker RD (1993) Two-dimensional resistivity imaging and modeling in areas of complex geology. J Appl Geophys 29:211–226 .
[17] DeGroot-Hedlin C, Constable S (1990) Occam’s inversion to generate smooth, two-dimensional models from magnetotelluric data. Geophysics 55:1613–1624
[18] Sasaki Y (1992) Resolution of resistivity tomography inferred from numerical simulation. Geophys Prospect 40:453–4
[19] Edwards LS (1977) A modified pseudosection for resistivity and IP. Geophysics 42(5):1020–1036.
Publiée
2016-11-29
Comment citer
HEBBACHE, K; MELLAS, M; BOUBAYA, D.
APPLICATION OF 2D SURFACE ELECTRICAL RESISTIVITY TOMOGRAPHY TO DETECT THE UNDERGROUND CAVITIES A CASE SITE STUDY: TOLGA AREA (ALGERIA).
Courrier du Savoir, [S.l.], v. 21, nov. 2016.
ISSN 1112-3338.
Disponible à l'adresse : >http://univ-biskra.dz/revues/index.php/cds/article/view/1827>. Date de consultation : 22 déc. 2024
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