STABILITY OF THAWING SLOPES: FIELD AND THEORETICAL INVESTIGATIONS
Stability analyses of thawing slopes in cohesive soils are examined. On the basis of field investigations it was found that current methods which explain instabilities in thawing slopes are not correct in assuming the failing mass as a continuous and rigid translational block. Instead the structure of the failing mass was recorded to be composed of a deformable mixture of soil lumps and muddy water, the product of the thawing of a reticulate ice vein network subdividing the previously frozen soil into irregular blocks. A theoretical approach of stability analysis based on the particulate structure of the failing thawing slopes is presented. (TRRL)
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Supplemental Notes:
- Proceedings of the 10th International Conference on Soil Mechanics and Foundation Engineering, Volume 3, Stockholm.
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Corporate Authors:
AA Balkema
P.O. Box 1675
Rotterdam, Netherlands BR-3000 -
Authors:
- Vallejo, L E
- Edil, T B
- Conference:
- Publication Date: 1981
Media Info
- Features: Figures; References; Tables;
- Pagination: p. 545-548
Subject/Index Terms
- TRT Terms: Cohesive soils; Conferences; Failure; Field tests; Freeze thaw durability; Mathematical models; Slope stability; Stability analysis; Thaw
- ITRD Terms: 4157: Cohesive soil; 8525: Conference; 5520: Failure; 2577: Freezing thawing cycle; 6226: In situ; 6473: Mathematical model; 5783: Slope stability
- Subject Areas: Geotechnology; Highways; I26: Water Run-off - Freeze-thaw;
Filing Info
- Accession Number: 00370161
- Record Type: Publication
- Source Agency: Swedish National Road and Transport Research Institute (VTI)
- Files: ITRD, TRIS
- Created Date: Mar 31 1983 12:00AM