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Titlebook: 5th International Conference on New Developments in Soil Mechanics and Geotechnical Engineering; Proceedings of ZM 20 Cavit Atalar,Feyza Çi

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Rainer Lasch,Christian G. Jankeretween the CST and a compacted sand is determined. First, characterization of the chosen quarry sand comprised identification tests, Proctor tests and the direct shear test (DST). Then follows the preparation of sand samples compacted, in Proctor molds, at the optimum modified and normal Proctor wat
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https://doi.org/10.1007/978-3-658-37286-6ariation for identical specimens. It was found that slight deformation of might not be the fundamental reason for . variation, however, slight deformation may introduce difficulties of dry density measurement, which may result in apparent . variation. With the new apparatus, good repeatability of .
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Rekonstruktive Bildungsforschungalues obtained from ‘so called’ extremely small undisturbed samples tested in the laboratory. The variation of compression index with depth of the deposit are also presented for different OCR values considered.
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