Page 18 - 2006 DT 12 Issues
P. 18

Quicksand!                           ing earthquakes, not too much.       on you. They might pull you “into two
                                                                                  pieces if [they] try hard to pull [you]
                                                  It’s all a matter of physics. Be-
                                             cause the human body is less dense  out,” said Daniel Bonn, a physics pro-
                s the story goes, on a dark  than  quicksand,  it  cannot  sink  (at  fessor at the Van der Waals-Zeeman
                and stormy night in La Porte,  least not like in the movies, where the  Institute at the University of Amster-
        AIndiana several workers from  villain disappears beneath the mud).  dam. “The way to do it is to wriggle
        the West Michigan Railroad watched  According to a study published in the  your legs around. This creates a space
        in horror as a train engine and several  British journal Nature in December,  between the legs and the quicksand,
        boxcars crossed Lily Lake and slowly  2004, it is impossible for a person  through which water can flow down
        sank, never to be seen again. Fortu-  immersed in quicksand to be drawn  to dilate [loosen] the sand. You can
        nately, no one was hurt. Some say the  completely under. You can more easily  get out using this technique, if you do
        marsh over which the track had been  float on quicksand than in water—but  it slowly and progressively.”
        laid had a quicksand bottom. Others  there are some caveats.                   Most patches of quicksand are
        say that divers have actually seen the    The ratio of soil to water de-  rarely more than a few feet deep, but
        engine and cars that will never be re-  termines buoyancy; therefore, some  falling in head first could be lethal. (Try
        covered from the quicksand.                                               not to get stuck at low tide on a beach,
        No one will ever know for                                                 either.) Heat exhaustion, unfriendly
        sure because the marsh has                                                animals and other elemental hazards
        long since been filled in.                                                 are dangerous, too, once you’re in the
             What exactly is quick-                                               muck. While most quicksand lore is
        sand? According  to  the                                                  just myth, don’t write it off completely
        United  States  Geological                                                just yet. Read on . . . .
        Survey, it’s nothing more                                                      Surely  you’ve  heard  tales  of
        than  a  soupy  mixture  of                                               travelers, vehicles and even whole
        sand and water. It can form                                               caravans suddenly vanishing into the
        anywhere underground wa-                                                  sands. (Hollywood has thrived on them
        ter rises up to over-saturate                                             for years). Until recently, such stories
        or liquefy an area of sand,                                               were considered mere folklore. The
        silt, clay or any other grainy                                            truth, however, may lie in “dry quick-
        soil, causing the grains to become  quicksands may be more difficult to    sand,” described as a mysterious, more
        more buoyant. In this semi-liquid state,  deal with. A heavy backpack will make   sinister, and potentially more danger-
        the sand shifts very easily and quickly,  you less buoyant, so a quick-release   ous, form of quicksand which has the
        thus the name. Just how quickly can  buckle is important. And don’t panic.   ability to quickly engulf anything that
        often be seen during an earthquake in  Even objects more dense than quick-  crosses its surface. While such a phe-
        areas where deep, sandy soils aren’t  sand won’t sink until they start to move   nomenon has not yet been confirmed
        supported by bedrock. All that shak-  around. Flailing arms and legs won’t   in nature, rheologist Detlef Lohse, who
        ing can increase groundwater pressure   sink you, but can lock you in tighter.   studies the deformation and flow of
        forcing it to the surface, quickly lique-  Movement causes the apparent viscos-  matter at the University of Twente in
        fying the ground and causing buildings   ity (flow resistance) to increase as you   Enschede, Netherlands, has succeeded
        on top of it to sink.                move, creating more vacuum on your   in creating it in the laboratory.
             Quicksand occurs in all 50 states.  submerged half. It’s best to relax, float   Dry  quicksand  is  loose  sand
        You’ll find it on riverbanks, in marshes,  on your back and slowly paddle your  whose  bulk  density  is  reduced  by
        in beach areas and even in the desert  way out.                           blowing air through it so that it yields
        where underground springs flow. How        If you are in above your waist,  easily to surface weight or pressure.
        concerned should you be? Except dur-  however, don’t ask your friends to tug  What water is to normal quicksand, air
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