Page 60 - Petrology of Sedimentary Rocks
P. 60

Comparison    of  two  means.   We  have   studied   the  heavy   mineral   suites   of  two  formations.
      We  examine   50  samples   of  the  Abner   formation   and  find   that   within   the  heavy   minerals,
      of  the  garnet   content   averages   15.0%   with   a  standard   deviation   of  5%;  and  30  samples
      of  the  Benjamin   formation   show   a  garnet   content   of   10.0  with   a  standard   deviation   of
      4.0%.   The   question   arises,   does   the  Abner   really   have   more   garnet   than   the  Benjamin,
      or  could   such  differences   have   arisen   by  chance   sampling   of  a  homogeneous   population?
      The   so-called   “t  test”   has  been   devised   to  answer   this   question   and  is  one  of  the  most
      useful   statistical   devices.   We  substitute   our  values   in  the  following   equation,   where   ;;i: is
      our   mean   garnet   content,   and   n  equals   the   number   of  samples   (subscript   a  refers   to
      values   from   the  Abner   formation   ,  b  to  the  Benjamin   formation).









      where   s  approximately   equals   the  average   standard   deviation   of  the  two   sets  of  values,
      and   is  found   by  the   following   equation   (which   is  merely   an  expansion   of  our   regular
      formula   for   the  standard   deviation):










      We  come   out   with   a  certain   value   for   t.   From   here   we  enter   a  table   (p.  59)  showing   t
      values   as  a  function   of  the  number   of  “degrees   of  freedom”   and  of  ?  (probability).   To
      find   the  degree   of  freedom   in  this  case,   we  add  up  the  number   of  values   in  both  sets  of
      data   and  subtract   2  from   the   result   (in  the   example,   50  +  30-2   =  78  d.f.)   Entering   the
      table   with   78  degrees   of  freedom,   we  read   across   the  horizontal   row   at  this  value   until
      we  encounter   the  correct   t  value.   From   this  t  value   we  read   straight   up  to  see  what   P
      corresponds   to   our   t.   If  P  lies   between   .05  and   . IO,  then   we   know   that   there   is
      something   between   a  5%  and   10%  chance   of  our   obtaining   such   differences   (or  larger)
      by  chance   sampling   of  a  homogeneous   population.   This   may   be  colloquially   stated   as
      saying   “our   experiment   has  shown   that   there   are  only   5  to  IO  chances   in  100  that   the
      garnet   content   of  the  two   formations   is  the  same,”   or  the  reverse,   “there   is  a  90  to  95%
      chance   that   the   Abner   really   does  contain   more   garnet   than   the  Benjamin.”   Both   these
      statements   are  technically   not  exactly   precise,   but  may  be  considered   as  pretty   close   to
      the  truth.

            As  stated   before,   statisticians   ordinarily   consider   that   in  any   experiment   that
      fails   to  reach   the   5%  level,   the   data   do  not   warrant   making   a  conclusion.   In  other
      words   if  your   P  comes   out   to  the   10%  level,   it  means   that   you  have   failed   to  find   a
      really   significant   difference   between   the  two  formations,   either   because   the  difference
      in  means   is  too   small,   or   the   standard   deviation   is  too   large,   or  you   took   too   few
      samples.   The  only   way   to  remedy   this   situation   is  to  take   enough   samples   to  push  the
      results   beyond   the  5%  level.

            The
            --   X2   (Chi   square)   test.   The   t  test   is  used  when   you  are   comparing   means   of
      measurementsme        grain   size,   percentages,   porosities,   densities,   etc.)   between   two
      formations   and  can  generally   be  done  on  only  one  property   at  a  time.







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