Page 52 - Geotechnical Engineering Soil and Foundation Principles and Practice
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Special Problems with Sedimentary Rocks
                                                                       Special Problems with Sedimentary Rocks  47

                  Caverns and Sinks
                  Whereas clay pockets penetrate from the ground surface downward, caverns
                  occur at the level of a groundwater table and remain as open voids until the top
                  caves in. Caverns are difficult to locate as they can readily be missed by borings,
                  and geophysical seismic and resistivity measurements focus on what is there and
                  not what is gone. Ground-penetrating radar would be most useful but the
                  penetration depth is limited, particularly in clay.

                  Caves are of obvious concern in foundation engineering, as a roof collapse can
                  drop part or all of a building or other structure into the ground without advance
                  warming. The consequences can be devastating. A cavern collapse under a
                  railroad track in South Africa left a train suspended in midair by welded rails.

                  A cavern that already has collapsed is a sink, and cavernous ground often can be
                  recognized from the occurrence of sinks. Sinks may be obvious, as in Fig. 3.4, or
                  also can be detected from streams that disappear and have no visible outlet.

                  Sinks also are a major concern for groundwater supplies, as they are direct conduits
                  leading into aquifers. Whatever falls or is thrown into a sink therefore may be only
                  a step away from the well, and the once-common practice of dumping everything
                  into a sink from bald tires to dead dogs and old automobile batteries must stop.

                  Sinks also are a challenge for investigators because a floor may only conceal part
                  of a deeper cavern. A hint as to consequences of a brash action may be found in
                  animal bones lying in the bottom of a sink.

                  Cavernous ground impacts the feasibility of a dam because of the potential for
                  leakage. Sealing of leaky dam foundations and abutments can be attempted by


                                                                                          Figure 3.4
                                                                                          Collapsed caverns,
                                                                                          or sinks, commonly
                                                                                          dot the landscape
                                                                                          in limestone areas.
                                                                                          It is the caverns
                                                                                          that are not known
                                                                                          and have not yet
                                                                                          collapsed that are
                                                                                          more likely to
                                                                                          create serious
                                                                                          foundation
                                                                                          problems.





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