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Slides in subaqueous slopes in loose sand and silt
Types of slides occurring in loose fine sands and coarse silts that are characterized by liquefaction of sand at small strains are described; it has proved useful to distinguish between two different types of slides -- flow slides and liquefaction slides; it is believed that susceptibility of loose sand to liquefaction is result of small strain at failure, low frictional resistance, rapid rise in pore pressure during shearing, and rapid loss in strength after failure; finally, description is given of method used in Norway to determine whether or not sand deposit may be subject to liquefaction. (24381)
Slides in subaqueous slopes in loose sand and silt
Types of slides occurring in loose fine sands and coarse silts that are characterized by liquefaction of sand at small strains are described; it has proved useful to distinguish between two different types of slides -- flow slides and liquefaction slides; it is believed that susceptibility of loose sand to liquefaction is result of small strain at failure, low frictional resistance, rapid rise in pore pressure during shearing, and rapid loss in strength after failure; finally, description is given of method used in Norway to determine whether or not sand deposit may be subject to liquefaction. (24381)
Slides in subaqueous slopes in loose sand and silt
Norg Geotek Inst, Publ
Andresen, A. (author) / Bjerrum, L. (author)
1968
9 pages
Article (Journal)
English
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