When triaxial compression (TC) tests are performed for the design of fills of sandy soil, the specimens are usually prepared by uniform compaction in the laboratory. On the other hand, in field compaction, the dry density, ρd, noticeably decreases with depth in each compaction layer, while the surface layer of fill may be considerably disturbed due to local shear failure at the contact with a rigid steel roller. In this study, full-scale compaction tests were performed at various compaction energy levels in a wide range of ρd and water content, w, and the strength and deformation characteristics of field-compacted sandy soil were evaluated by TC tests on undisturbed samples from the test fills and those compacted in the laboratory. Empirical equations expressing the strength and stiffness of compacted soil were derived, which consists of an increasing function of ρd multiplied by a decreasing function of the degree of saturation, Sr. The equations take into account the effects of compaction disturbance and wetting/saturation while not including the compaction energy and compaction method as variables. It is shown that, when compacted at Sr equal to, or around, the optimum degree of saturation, (Sr)opt, the effects of these factors are negligible, so, results of TC tests on unsaturated specimens compacted in the laboratory are applicable to the design field conditions.
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