Geotechnical & Geological Engineering

, Volume 9, Issue 1, pp 1–26 | Cite as

Geotechnical properties of the Corinth Canal marls

  • A. G. Anagnostopoulos
  • N. Kalteziotis
  • G. K. Tsiambaos
  • M. Kavvadas
Papers

Summary

The Corinth Canal crosses the isthmus of Corinth and is of great importance for Mediterranean navigation as well as the railroad and highway connections between southern and central Greece. In the century-long history of the Canal, the slopes have shown only minor stability problems despite their significant length, very steep inclination and, more importantly, the strong earthquakes that have frequently shaken the Corinth area. This type of unsual behaviour has motivated research into the mechanical behaviour of the bluish grey marl which is the main geological formation in the Canal area.

Geotechnical investigation of the Corinth Canal marl was performed with an extensive laboratory testing programme on high quality undisturbed samples of the intact marl. The material was shown to exhibit brittle behaviour, high stiffness and significant apparent cohesion at low and moderate stress levels. These characteristics indicate that the material possesses significant structural bonding which is believed to be due to cementation between individual particles, caused by the deposition of carbonates at the time of material genesis. With stressing, the material yields due to a gradual bond degradation. The locus of the initial yield points (yield surface) seems to be an ellipse oriented along the isotropic axis.

The testing programme was supplemented with a series of tests on the de-structured marl obtained by thorough remoulding. These tests showed a significant difference in the pre-yield stiffness and the peak strength at low stress levels, but comparable post-rupture shear strengths.

Keywords

Shear Strength Cementation Minor Stability Geotechnical Investigation Canal Area 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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References

  1. Anagnostopoulos, A., Christoulas, S., Kalteziotis, N. and Tsiambaos, G. (1989) Some geotechnical aspects of the marls of Corinth Canal,Proceedings of the 12th ICSMFE, Rio de Janeiro, Brazil, 491–4.Google Scholar
  2. Andrikopoulou, K.P., Marinos, P.G. and Vainalis, D. (1988) Geotechnical zoning in the Corinth Canal,Proceedings of an International Symposium on the Engineering Geology of Ancient Works, Monuments and Historical Sites, Athens, Greece, Balkema, Vol. 1, 231–5.Google Scholar
  3. Barth, T.F.W., Correns, C.W. and Eskola, P. (1939)Die Entstehung der Gesteine, Springer-Verlag, Berlin, 422 p.Google Scholar
  4. Christoulas, S.G., Kalteziotis, N.A. and Tsiambaos, G.K. (1984) Geotechnical problems in a bridge over Corinth Canal,International Conference on Case Histories in Geotechnical Engineering, St. Louis, Missouri, Vol. 3, 849–54.Google Scholar
  5. Collier, R.E.L.L. (1990) Eustatic and tectonic controls upon quaternary coastal sedimentation in the Corinth Basin, Greece,Journal of the Geological Society,147, 301–14.Google Scholar
  6. Datta, M., Gulhuti, S.K. and Rao, G.V. (1982) Engineering behaviour of carbonate soils of India and some observations on classification of such soils, InGeotechnical Properties, Behaviour and Performance of calcareous Soils, ASTM Special Technical Publication777, 113–40.Google Scholar
  7. Drakopoulos, J., Leventakis, G. and Roussopoulos, A. (1978) Micro-zonation in the seismic area of Corinth-Loutraki,Annali di Geofisica, Vol. 31, 31–95.Google Scholar
  8. Freyberg, V. (1973) Geologie des Isthmus von Korinth,Erlangen Geologische Ablhandlungen, Heft 95, Junge und Sohn, Universitats Buchdruckerei Erlangen, p. 183.Google Scholar
  9. Fuchs, E. (1877) L'Isthme de Corinthe, sa construction geologique son percement, Association Francaise pour l'Avancement des Sciences, Toulouse, France.Google Scholar
  10. Galanopoulos, A. (1968) On the quantitative determination of earthquake risk,Annali di Geofisica, Vol. 21 193–206.Google Scholar
  11. Hawkins, A.B., Lawrence, M.S. and Privett, K.D. (1988) Implications of weathering on the engineering properties of the Fuller's Earth formation,Geotechnique, Vol. 38(4), 517–32.Google Scholar
  12. Kavvadas, M. (1990) Some considerations on the stability of the Corinth Canal slopes,Presentation at the 4th Young Geotechnical Engineers Conference, Delft, The Netherlands.Google Scholar
  13. Lee, H.J. (1985) Laboratory determination of the strength of marine soilsState-of-the-art report, Strength Testing of Marine Sediments, ASTM Specialty Technical Publication,883, 181–250.Google Scholar
  14. Leroueil, S., Tavenas, F., Brucy, F., LaRochelle, P. and Roy M. (1979) Behaviour of destructured natural clays,Journal of Geotechnical Division, ASCE,105, 759–78.Google Scholar
  15. Maccarini, M. (1987) Laboratory studies of a weakly bonded artificial soil,PhD Thesis, University of London.Google Scholar
  16. Mariolakos, I. and Stiros, S.C. (1987) Quaternary deformation of the Isthmus and Gulf of Corinth (Greece),Geology,15, 225–8.Google Scholar
  17. Marsland, A. (1971) Laboratory and in-situ measurements of the deformation moduli of London clay,Proceedings of a Symposium on Interaction of Structure and Foundation, Birmingham, UK, 7–17.Google Scholar
  18. Mitchell, J.K. (1976)Fundamentals of Soil Behaviour, John Wiley, New York.Google Scholar
  19. Papazachos, B.C., Comninakis, P.E., Moundrakis, D.M. and Pavlides, S.B. (1981) Preliminary results of an investigation of the February–March 1981 Alkionides Gulf (Greece) earthquakes,International Symposium on the Hellenic Arc and Trench, Vol. 1, 400–20.Google Scholar
  20. Pettijohn, F. (1975)Sedimentary Rocks, Harper and Row publishers, London, 526 p.Google Scholar
  21. Philippson, A. (1890) Der Isthmus von Korinth,Z. Ges. Erdkde. Berlin 25, 1–98.Google Scholar
  22. Ritsema, A. (1974) The earthquake mechanism of the Balkan region,Royal Netherlands Met. Inst. Sci., Nr 74, 1–36.Google Scholar
  23. Sebrier, M. (1977) Tectonique recente d'une transversale a l'arc Egeen: Le Golfe de Corinthe et ses regions peripheriques,These, Universite de Paris XI, Centre d'Orsay.Google Scholar
  24. Skempton, A.W. (1953) The colloidal activity of clay,3rd ICSMFE Zurich, Switzerland, Vol 1, p. 57–61.Google Scholar
  25. Tsiambaos, G. (1988) Engineering Geological characteristics of Iraklion marls,PhD Thesis (in Greek), University of Patras, Greece, 358 p.Google Scholar
  26. Vaughan, P.R. (1985) Mechanical and hydraulic properties of in-situ residual soils.Proceedings of the First International Conference in Geomechanics in Tropical, Lateritic and Saprolitic Soils, Brasilia, Vol 3, 231–63.Google Scholar
  27. Vaughan, P.R., Maccarini, M. and Mokhtar, S.M. (1988) Indexing the engineering properties of residual soil,Quarterly Journal of Engineering Geology,21, 69–84.Google Scholar

Copyright information

© Chapman and Hall Ltd 1991

Authors and Affiliations

  • A. G. Anagnostopoulos
    • 1
  • N. Kalteziotis
    • 1
    • 2
  • G. K. Tsiambaos
    • 1
    • 2
  • M. Kavvadas
    • 1
  1. 1.Geotechnical DepartmentNational Technical University of AthensGreece
  2. 2.Geotechnical Engineering SectionCentral Laboratory of Public WorksAthensGreece

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