Page 294 - Geotechnical Engineering Soil and Foundation Principles and Practice
P. 294

Compaction
                                                                                            Compaction   289

                  regardless of the number of additional passes of a compactor. If processing
                  continues past that point, the result is called overcompaction.

                  A Conflict over Nomenclature
                  ‘‘Consolidation’’ was first described by a geologist, Sir Charles Lyell, in a
                  textbook published in 1851. Lyell noted that sediments on the sea bottom are
                  compressed and consolidate under their own weight and not from the weight of
                  hundreds or thousands of feet of sea water. Despite this prior definition by an
                  eminent geologist, geologists in the petroleum industry call the process
                  ‘‘compaction’’ and refer to shale as being ‘‘highly compacted.’’ The Oxford
                  English Dictionary favors the engineering usage, defining consolidation as
                  bringing together and compaction as packing together. It is important that
                  geotechnical engineers not confuse the two terms and their distinctive meanings.

                  13.5.2   Overcompaction

                  A continued application of compactive effort after soil reaches near-saturation
                  point not only wastes energy, but the energy is redirected into shearing and
                  remolding the compacted and nearly saturated soil. Shearing smears clay particles
                  so that they are oriented parallel to the shear surfaces and permanently weaken
                  the soil. This must be carefully guarded against, as the soil then must be dried and
                  pulverized before it can be recompacted.

                  The effect of overcompaction on strength of a clay is shown in Fig. 13.8, which
                  shows stress-strain curves for two samples of the same soil at the same moisture
                  content and same density, the difference being that the weaker soil was compacted
                  at a higher moisture content than the stronger one.

                  Clues to overcompaction are vibrations that can be felt under foot, and an
                  occasional ‘‘thunky’’ sound when stomped on. A bulge of soil sometimes may be

                                                                                          Figure 13.8
                                                                                          Stress-strain
                                                                                          curves show the
                                                                                          reduction in
                                                                                          strength after a soil
                                                                                          becomes
                                                                                          dispersed through
                                                                                          overcompaction
                                                                                          and shearing.
                                                                                          (After Seed and
                                                                                          Chan 1959, with
                                                                                          permission of the
                                                                                          American Society
                                                                                          of Civil Engineers.)


                          Downloaded from Digital Engineering Library @ McGraw-Hill (www.digitalengineeringlibrary.com)
                                             Copyright © 2007 The McGraw-Hill Companies. All rights reserved.
                                                Any use is subject to the Terms of Use as given at the website.
   289   290   291   292   293   294   295   296   297   298   299