Abstract
Mapping of quick clay is important for hazard zonation, planning and protection purposes. The present study focuses on an area prone to quick clay landslides in mid Norway, which is investigated through a combination of geophysical and geotechnical methods. The following classes are suggested for a first-order interpretation of resistivity profiles in areas with few or no previous investigations: Unleached clay deposits: 1–10 Ωm; Leached clay deposits, possibly quick: 10–100 Ωm; Dry crust clay deposits and coarse sediments: >100 Ωm. In the study area, 14–80 Ωm was found as the main resistivity interval for quick clay. The resistivity values from the present study are compared to previously published values. Classification of material from resistivity values is influenced by local conditions, and there is an overlap between the classes. Resistivity profiles can give valuable information for hazard zonation and may assist in maximising subsequent intrusive investigations.
Résumé
La cartographie des argiles sensibles est importante pour des objectifs de zonage d’aléa, de planification et de protection. L’étude présentée se focalise sur une région sujette aux glissements dans des argiles sensibles du centre de la Norvège. Elle a mis en œuvre une combinaison de méthodes géophysiques et géotechniques. Les classes suivantes sont suggérées pour une première interprétation en termes de profils de résistivité dans des régions peu ou pas étudiées jusqu’alors : Dépôts d’argiles non lessivées : 1–10 Ωm; Dépôts d’argiles lessivées, pouvant être sensibles : 10–100 Ωm; Dépôts d’argiles superficielles sèches : >100 Ωm . Dans la région d’étude, des plages de valeurs de 14 à 80 Ωm caractérisent le mieux des argiles sensibles. Les valeurs de résistivité de cette étude sont comparées à des valeurs précédemment publiées. Le classement des matériaux à partir des valeurs de résistivité est influencé par des conditions locales et il y a un chevauchement entre les classes. Les profils de résistivité peuvent donner une information valable pour un zonage d’aléa et peuvent permettre d’optimiser des investigations ultérieures par méthodes intrusives.
Similar content being viewed by others
References
Aasland R (2010) Kartlegging av kvikkleire med 2D resistivitet og RCPT i Rissa. Master Thesis at Department of Civil and Transport Engineering, Norwegian University of Science and Technology (NTNU) (in Norwegian)
ABEM (1999) ABEM Terrameter SAS 4000/SAS 1000. Instruction Manual. ABEM Printed Matter 93101. ABEM, Sweden
Berger B (1980) Rapport om vertikale elektriske sonderinger i Verdal. Norwegian Institute of Technology, Trondheim (in Norwegian)
Bjerrum L (1954) Geotechnical properties of Norwegian marine clays. Géotechnique 4:49–69
Calvert HT, Hyde CSB (2002) Assessing landslide hazard in the Ottawa Valley using electrical and electromagnetic methods. In: Symposium on the application of geophysics to environmental and engineering problems (SAGEEP). Environmental and Engineering Geophysical Society. Wheat Ridge, CO, United States
Carson MA, Geertsema M (2002) Mapping in the interpretation and risk assessment of flowslides. In: Bobrowsky PT (ed) Geoenvironmental mapping: methods, theory and practice. AA Balkema, Lisse, Netherlands, pp 667–696
Dahlin T (1993) On the automation of 2D resistivity surveying for engineering and environmental applications. Dr. thesis. Lund University, Sweden
Dahlin T, Zhou B (2006) Multiple-gradient array measurements for multi-channel 2D resistivity imaging. Near Surf Geophys 4:113–123
Dahlin T, Larsson R, Leroux V, Svensson M, Wisén R (2001) Geofysik i släntstabilitetsutredningar. Statens geotekniska institut, Report 62 (in Swedish)
Dahlin T, Leroux V, Larsson R, Rankka K (2005) Resistivity imaging for mapping of quick clays for landslide risk assessment. In: Proceedings of 11th Annual Meeting EAGE-Environmental and Engineering Geophysics, Palermo, Italy, 4–7 September, 2005, A046
Dalsegg E (2008) Geofysiske målinger for løsmassekartlegging ved Rødde i Melhus kommune, Sør-Trøndelag. NGU Report 2008.084 (in Norwegian)
Donohue S, Long M, O’Connor P, Helle TE, Pfaffhuber A, Rømoen M (2009) Geophysical mapping of quick clay—a case study from Smørgrav, Norway. In: Proceedings of Near Surface 2009, Dublin, Ireland, Expanded Abstracts C17
Eggen A, Gregersen O (2004) Program for økt sikkerhet mot leirskred. Evaluering av risiko for kvikkleireskred—Melhus kommune. NGI Report 20001008-7 (in Norwegian)
Fukue M, Minato T, Horibe H, Taya N (1999) The micro-structures of clay given by resistivity measurements. Eng Geol 54:43–53
Geotech (2010) CPT Electric Conductivity Adapter. Datasheet. www.geotech.se [cited November 2010]
Glade T, Anderson M, Crozier MJ (eds) (2005) Landslide hazard and risk. Wiley, England
Gregersen O (2002) Vurdering av risiko for skred. Metode for klassifisering av faresoner, kvikkleire. NGI Report 20001008-2 (in Norwegian)
Gregersen O, Løken T (1983) Mapping of quick clay landslide hazard in Norway. Criteria and experiences. SGI Rep 17:61–174
Gregersen O, Løken T (1988) Faresonekartlegging kvikkleireskred. Kartblad Trondheim, M 1:50 000. NGI Report 84050-1 (in Norwegian)
Grønlie A (1953) Leinstrand i den aller eldste tida. Johan Christiansens boktrykkeri, Trondheim, 30 p (in Norwegian)
Hilmo BO (1989) Marine sensitive leirers mineralsammensetning, kolloidkjemi og mekaniske egenskaper. Dr. Thesis at Department of Geology and Mineral Resources Engineering, Norwegian University of Science and Technology (NTNU) (in Norwegian)
Hyde CSB, Hunter JA (1998) Formation electrical conductivity—porewater salinity relationships in Quaternary sediments from two Canadian sites. In: Proceedings of the symposium on the application of geophysics to engineering and environmental problems, March 22-26, 1998, Chicago, IL. Environmental and Engineering Geophysics Society, pp 499–510
ISSMGE TC32 Technical Committee on Risk Assessment and Management (2004) Glossary of risk assessment terms. Version 1, July 2004
Janbu N, Nestvold J, Røe Ø, Sveian H (1993) Leirras—årsaksforhold og rasutvikling. In: Walberg Ø (ed) Verdalsboka, Ras i Verdal, vol. B. Verdal kommune, pp 739–784 (in Norwegian)
Karlsrud K, Aas G, Gregersen O (1985) Can we predict landslide hazards in soft sensitive clays? Summary of Norwegian practice and experience. NGI Publication 158
Lebuis J, Robert J-M, Rissmann P (1983) Regional mapping of landslide hazard in Quebec. Symposium on slopes on soft clays. SGI Rep 17:205–262
Leroux V, Dahlin T (2003) Resistivity mapping of quick clay. Field study at Skepplanda, Utby and Munkedal in Bohuslän, Sweden. Lund University, Engineering Geology, 22 pp
Loke MH (2007) Res2DInv ver. 3.56. Geoelectrical Imaging 2D and 3D. Instruction Manual. Geotomo Software
Lundström K, Andersson M (2008) Hazard mapping of landslides, a comparison of three different overview mapping methods in fine-grained soils. In: Locat J, Perret D, Turmel D, Demers D, Leroueil S (eds) Proceedings of the 4th Canadian conference on geohazards: from causes to management. Presse de l’Université Laval, Québec, 594 pp
Lundström K, Larsson R, Dahlin T (2009) Mapping of quick clay formations using geotechnical and geophysical methods. Landslides 6:1–15
Norges vassdrags-og energidirektorat (NVE) (2009) Planlegging og utbygging i fareområder langs vassdrag. Retningslinjer 1-2008. Vedlegg: Vurdering av områdestabilitet ved utbygging på kvikkleire og andre jordarter med sprøbruddegenskaper. Revision March 5 2009 (in Norwegian)
Norsk Geoteknisk Forening (NGF) (1975) Retningslinjer for presentasjon av geotekniske undersøkelser (in Norwegian)
Ottesen HB (2009) CPTU med resistivitetsmåling. Master Thesis at Department of Civil and Transport Engineering, Norwegian University of Science and Technology (NTNU) (in Norwegian)
Quinn PE (2009) Large landslides in sensitive clay in eastern Canada and the associated hazard and risk to linear infrastructure. PhD Thesis at Department of Geological Sciences and Geological Engineering, Queens University, Canada
Railroad operation report (1867) Trondhejm-Støren Jernbanens 3. driftsberetning Aa 1867 (in Norwegian)
Reiser F, Dahlin T, Rønning JS, Solberg IL (2010) Resistivity modelling for clay layer characterisation, possibilities and limitations. NGU Report 2010.047
Reite AJ (1983) Trondheim. Beskrivelse til kvartærgeologisk kart 1621 IV—M 1:50 000. NGU Skrifter 391, 44 pp (in Norwegian)
Reite AJ, Selnes H, Sveian H (1982) A proposed deglaciation chronology for the Trondheimsfjord area, Central Norway. Geol Surv Norway 373:75–84
Reynolds JM (1997) An introduction to applied and environmental geophysics. Wiley, England
Robitaille D, Demers D, Potvin J, Pellering F (2002) Mapping of landslide prone areas in the Saguenay region, Quebec, Canada. In: Proceedings of the international conference on instability—planning and management, Ventnor, Isle of Wight, Royaume Uni
Rømoen M, Pfaffhuber AA, Karlsrud K, Helle TE (2010) Resistivity on marine sediments retrieved from RCPTU-soundings: a Norwegian case study. In: Proceedings of 2nd International Symposium on cone penetration testing, 9–11 May 2010, Huntington Beach, CA, USA
Sandven R (2002) Geoteknikk, materialegenskaper. Utstyr, prosedyrer og parameterbestemmelser. Compendium in the course SIG 2020. Department of geotechnical engineering, Norwegian University of Science and Technology, Trondheim, Norway (in Norwegian)
Schälin D, Tornborg J (2009) Evaluation of CPT-R and resistivity measurements in quick clay area. Master of Science Thesis at Department of Civil and Environmental Engineering, Chalmers University of Technology
Söderblom R (1969) Salt in Swedish clays and its importance for quick clay formation. Results from some field and laboratory studies. SGI Proceedings 22
Solberg IL, Rønning JS, Dalsegg E, Hansen L, Rokoengen K, Sandven R (2008) Resistivity measurements as a tool for outlining quick clay extents and valley fill stratigraphy: feasability study from Buvika, Central Norway. Can Geotech J 45:210–225
Solberg IL, Aasland R, Dalsegg E, Hansen L, L’Heureux JS, Rønning JS (2010) Kvikkleireproblematikk i Rissa—bruk av resistivitetsmålinger. In: Proceedings of Fjellsprengningsdagen, Bergmekanikk-og Geoteknikkdagen, 25–26 November 2010, Oslo, Norway, 37 pp (in Norwegian)
Telford WM, Geldart LP, Sheriff RE (1990) Applied geophysics. Cambridge University Press, Cambridge, UK
Tønnesen JF (2010) Refraksjonsseismiske målinger for løsmassekartlegging ved Rødde i Melhus kommune. NGU Report 2010.034 (in Norwegian)
Viberg L (1984) Landslide risk mapping in soft clays in Scandinavia and Canada. In: Proceedings of IV International symposium on landslides, 16–21 September 1984, Toronto, pp 325–348
Vik A, Havnegjerde CR (2010) Kvikkleirekartlegging—Melhus og Trondheim. Grunnundersøkelser—datarapport. Multiconsult Report 413809-1 (in Norwegian)
Wangen PA, Sand K (2007) Rødde Gård—Geoteknisk vurdering av nybygg. Sweco Grøner Notat 571701-1 (in Norwegian)
Wolff FC (1976) Geologisk kart over Norge, berggrunnskart Trondheim M 1:250 000. NGU (in Norwegian)
www.skrednett.no [cited November 2010]
Acknowledgments
The authors thank the Norwegian Water Resources and Energy Directorate (NVE), the Norwegian National Rail Administration, the Norwegian Public Roads Administration and the Administrative Board of the Norwegian Natural Perils Pool for financial support in the project. Thanks are also given to the Norwegian University of Science and Technology (NTNU) for geotechnical sampling and drilling including RCPTU.
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Solberg, IL., Hansen, L., Rønning, J.S. et al. Combined geophysical and geotechnical approach to ground investigations and hazard zonation of a quick clay area, mid Norway. Bull Eng Geol Environ 71, 119–133 (2012). https://doi.org/10.1007/s10064-011-0363-x
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s10064-011-0363-x