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IITK-BMTPC Earthquake Tip 31

            Why do Buildings Sink into the Ground during Earthquakes?                                       page 2
               disintegration  of  the  large  soil  mass  behind  it.
               Therefore,  structures  may  sink  and  destabilize,  if
                                                                                                 Refill
               supported by such soil (Figure 4b). Soil movement                  Vibrator       mate
               due  to  lateral  spreading  can  exert  significant
               stresses  and  damage  in  foundations  and  bridge
               abutments causing damages.                                Original                    Compacted
                                                                           Soil                      Soil

                                                                                       (a)

                                                                            Seepage Flow
                                                                                            Excess
                                                                                            pore
                                Soil that can
                                  liquefy                                                   water

                                                                       Stone Columns        pressure
                                                                                            release
                                  (a)
                                                                             Surcharge      Surcharge





                                Soil that can liquefy                                  (b)
                                                                   Original GL
                                  (b)
                                                                                          Lowering of the ground
               Figure 4: Lateral spreading of slopes – (a) steep           Soil that can liquefy
                 slopes slide, and (b) gentle slopes subside                                             New GL



            Parameters Influencing Liquefaction
               Susceptibility of a site to liquefaction depends on
            following factors:
            (1)  Soil  properties:  Uniformly-graded,  fully-saturated
              cohesionless  (sandy)  soils  are  more  prone  to
              liquefaction than well-graded soils. Also, fine sands
                                                                                    Liquefied Soil
              are  more  susceptible  to  liquefaction  than  coarse
              sands, gravelly soils, silts or clays. Sands with some
              clay  content  also  can  liquefy.  Loose  sands  have                   (c)
              much higher tendency to liquefy than dense sands.
            (2)  Earthquake  shaking  characteristics:  As  shaking      Figure 5: Measures to overcome liquefaction –
                                                                      three options
              intensity increases, soil is subjected to higher stresses
              and strains, and is more susceptible to liquefaction.

              Also, strong shaking with  longer duration causes a   Related    -      Earthquake Tip
              larger number of stress and strain cycles in soil; this
                                                                Tip 31: What is important in foundations of earthquake-resistant
              increases chances for liquefaction.                   buildings?

            (3)  Geologic  conditions:  Some  geologic  processes  sort   Resource Material
              soils  into  uniform  grain  size  and  deposit  them
                                                                Kramer,S.L.,  (1996),  Geotechnical  Earthquake  Engineering,  Prentice
              loosely, as in Aeolian, Fluvial and Colluvial deposits;   Hall, Inc., New Jersey, USA
              such soils are candidates for liquefaction.       Towhata,I.,  (2008),  Geotechnical  Earthquake  Engineering,  Springer-
            Measures to overcome Liquefaction                     Verlag, Berlin

               To overcome liquefaction one may:
            (a)  Increase liquefaction-resistance of soil, e.g., densify      Authored by:

               loose  deposits  (by  vibro-compaction,  impact     C.V.R.Murty
               compaction  and  pressure  grouting)  or  replace   Indian Institute of Technology Jodhpur, India
               susceptible soil (by vibro-replacement) (Figure 5a);   Sponsored by:
            (b)  Reduce earthquake demand on soil, e.g., release of   Building Materials and Technology Promotion
               pore water pressure by allowing drainage of water   Council, New Delhi, India
               (by  stone  columns),  or  increase  confinement  by
               adding a surcharge (Figure 5b);                   This release is a property of IIT Kanpur and BMTPC. It may
            (c)  Remove  soil  layers  that  can  liquefy,  or  use   be  reproduced  without  changing  its  contents  with  due
                                                                 acknowledgement.  Suggestions  or  comments  may  be  sent
               anchored  piles  as  foundations  going  through   to: nicee@iitk.ac.in. To see all IITK-BMTPC Earthquake Tips, visit
               liquefiable soil layers (Figure 5c).              www.nicee.org or www.bmtpc.org.
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