Page 116 - Geotechnical Engineering Soil and Foundation Principles and Practice
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The Soil Profile
                                                                                         The Soil Profile  111

                  5.5.5  Drilling to Locate a Groundwater Table
                  Groundwater elevations are routinely measured and recorded during geotechnical
                  exploration drilling, by measuring water levels after they stabilize in open borings.
                  Even this is not foolproof because if a boring penetrates into a zone of artesian
                  pressure, the water level not only will rise higher in the hole but will shoot up as
                  a geyser. If a boring encounters and punches through a perched groundwater
                  table, the boring may drain before the water level can be measured. Special tech-
                  niques, namely the use of expandable packers, can be used to seal off artesian
                  or perched water. Moisture contents and densities of soil samples provide
                  information on the level(s) of saturation.


                  5.5.6  Relation of Groundwater Level to Soil Color

                  Engineers must design for worst anticipated groundwater conditions, so past
                  positions are as important as current positions. If groundwater elevations are
                  assigned too low, a rise in the groundwater table can readily float an empty
                  swimming pool or underground tank.
                                                                                    2þ
                  Below a permanent groundwater table iron oxides usually are in a reduced (Fe )
                  state because of deoxidation by organic matter. The soil color is a shade of gray
                  and may have a greenish or bluish tint. A horizon subscript g, for gleying, signifies
                  gray colors in a soil profile. Above the groundwater table, tan, brown, or rusty
                                                                       3þ
                  red colors indicate oxidation of the iron compounds (Fe ) by infiltrating
                  oxygen-charged rain water.

                  Gray colors may dominate in a zone of capillary saturation, but there will be
                  vertical fingers of tan or brown where oxygen-charged water has penetrated
                  downward through cracks and empty root channels. Soluble iron compounds
                  migrating to these sites can precipitate and make concretionary ‘‘pipestems.’’



                                                                                          Figure 5.6
                                                                                          Perched
                                                                                          groundwater table.
                                                                                          (From The Day the
                                                                                          House Fell by
                                                                                          R. L. Handy, with
                                                                                          permission of the
                                                                                          American Society
                                                                                          of Civil Engineers.)








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