The coarse-grained materials as a whole are the rock and soil mixtures with the wide range of particle size, from the massive rock with hundreds mm of diameter to the fine soils. The design density and its quality control limits are determined through a series of indoor compaction tests using the downsized samples, the larger size portion being cut off, along with the particle size correction (for example Walker-Holtz method) in the conventional design procedure. However it is almost impossible at the moment to predict the field compaction density satisfactorily from the indoor test results, because the method of compaction and the distribution of the particle size in the field embankment differ greatly from the indoor compaction condition. On the other hand, the well-known and widely used replacement method is not appropriate for the coarse material, because it cannot afford sufficient number of sampling data enough to evaluate the reliable field density from its persistent character, i.e. labor intensive and time consuming. We carried out a series of field test embankments under the several different water content condition, to simulate the indoor compaction test for the two cases of coarse fill materials. In order to evaluate the most reliable compaction density, the newly developed RI density meter of scanning type (SRID) was used in the field embankment tests. SRID has sufficient sensitive volume, roughly ten times as large as the conventional RI density meter, and its density sampling capacity is far greater than the replacement method, so applicable to the coarse materials and suitable to the multi-data sampling. In this report the field test results are shown and the correlation of the compaction characteristics in the field compaction work with the one in the indoor compaction tests are discussed.
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