The causes of and a prediction of slump displacement along the section between the straightened Karamyshev and Khoroshev sections of the Moscow River are examined. It is shown that the cause of the slump slide in 2006 was the above-norm settlement and erosion due to rainwater drainage in the lower part of the slope. The slump continues to move and predicted displacements will attain significant values, which may result in the formation of a new slump.
Similar content being viewed by others
References
O. I. Ignatova, "Deformation characteristics of the Jurassic clayey soils of Moscow," Osn. Fundam. Mekh. Gruntov, No. 5, 24-28 (2009).
R. Kerry Rowe, ed., Geotechnical and Geoenvironmental Engineering Handbook, Kluwer Academic Publishers (2001).
S. K. Kim et.al, "Prediction of rainfall-triggered slides in Korea," Proc. 6-th Int. Symp. on Land slides, Christchurch (1992). 2, 989-994.
Manual to SNiP 2.06-15-85, Forecasting Groundwater Encroachment and Analysis of Drain Systems in Areas Being Developed or Existing Development, Stroiizdat, Moscow (1991).
Author information
Authors and Affiliations
Additional information
Translated from Osnovaniya, Fundamenty i Mekhanika Gruntov, No. 1, pp. 25-29, January-February, 2016.
Rights and permissions
About this article
Cite this article
Kolybin, I.V., Popsuenko, I.K. & Kogai, V.K. A Study of a Slump in the Moscow River Slope. Soil Mech Found Eng 53, 46–52 (2016). https://doi.org/10.1007/s11204-016-9363-y
Published:
Issue Date:
DOI: https://doi.org/10.1007/s11204-016-9363-y