Significance:
Mechanical
compaction is one of the most common and cost effective means of stabilizing
soils. An extremely important task of
geotechnical engineers is the performance and analysis of field control tests
to assure that compacted fills are meeting the prescribed design
specifications. Design specifications
usually state the required density (as a percentage of the “maximum” density
measured in a standard laboratory test), and the water content. In general, most engineering properties, such
as the strength, stiffness, resistance to shrinkage, and imperviousness of the
soil, will improve by increasing the soil density.
The
optimum water content is the water content that results in the greatest density
for a specified compactive effort.
Compacting at water contents higher than (wet of ) the optimum water
content results in a relatively dispersed soil structure (parallel particle
orientations) that is weaker, more ductile, less pervious, softer, more
susceptible to shrinking, and less susceptible to swelling than soil compacted
dry of optimum to the same density. The
soil compacted lower than (dry of) the optimum water content typically results
in a flocculated soil structure (random particle orientations) that has the
opposite characteristics of the soil compacted wet of the optimum water content
to the same density.
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