Page 305 - Geotechnical Engineering Soil and Foundation Principles and Practice
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Compaction
                300   Geotechnical Engineering

                 Figure 13.16
                 The expanding
                 steel mold of the
                 ‘‘K test’’ enables
                 rapid estimates of
                 soil strength and
                 compressibility
                 parameters from
                 Proctor density
                 specimens, but
                 drainage may be
                 incomplete.










                                    compressibility in an expandable steel mold (Fig. 13.16). A specimen from a
                                    Proctor density test is inserted in the mold and compressed at the ends, which
                                    causes the mold to expand and automatically exert a gradually increasing lateral
                                    confining stress on the sample.

                                    In geotechnical engineering, K denotes the ratio between horizontal and vertical
                                    stress. In a ‘‘K test,’’ vertical stress is measured and the lateral stress is obtained
                                    from a suitable calibration from expansion of the steel mold. As both stresses
                                    simultaneously increase it is possible to obtain running estimates of both the soil
                                    cohesion and the angle of internal friction, as well as a compression modulus and
                                    soil-to-steel sliding friction. Although the soil is confined between porous stones
                                    to allow drainage, compacted specimens contain sufficient air that little drainage
                                    occurs. K-test results have been used with bearing capacity theory for design of
                                    tamping-foot rollers.


                13.10    GRADATION AND COMPACTED DENSITY



                                    Density after compaction is closely related to the range of particle sizes, as
                                    progressively smaller particles fill in the voids, whereas density also is influenced
                                    by the largest particles present, as a solid particle is more dense than a cluster of
                                    many smaller particles.

                                    A variety of moisture-density curves representing different gradations of soil is
                                    shown in Fig. 13.17, where it will be seen that, in general, the coarser the soil, the
                                    higher the compacted density and lower the OMC. However, it also may be noted

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