In granular soils, the degree of compaction in the field can be measured according to the
relative density, defined as
where
The relative density can also be expressed in terms of dry unit weight, or
The denseness of a granular soil is sometimes related to the soil’s relative density.
Table 1.5 gives a general correlation of the denseness and For naturally occurring
sands, the magnitudes of and [Eq. (1.23)] may vary widely. The main reasons for
such wide variations are the uniformity coefficient, and the roundness of the particles.
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