Page 49 - Petrology of Sedimentary Rocks
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poorest   sorted   sediments,   such  as  glacial   tills,   mudflows,   etc.,   have   a,  values   in  the
            neighborhood   of  .!$I  to  8  or  even   IO+.


            Measures   of  Skewness   or  Asymmetry

                  Curves   may  be  similar   in  average   size  and  in  sorting   but  one  may  be  symmetrical,
            the  other   asymmetrical.   Skewness   measures   the  degree   of  asymmetry   as  well   as  the
            ‘tsignlf--   i.e.,  whether   a  curve   has  an  asymmetrical   tail  on  the  left  or  right.

            Phi   Quartile   Skewness   (Skq@).   This   is  found   by  (425  +  $75  -  2(Md$))/2.   A  (+>  value
            indicates   that  the  sediment   has  an  excess  amount   of  fines   (the  frequency   curve   shows  a
            tail   on  the  right)   and  a  (-)  value   indicates   a  tail   in  the  coarse   (left>.   The  disadvantage
            of  this  measure   is  that   it  measures   only  the  skewness   in  the  central   part   of  the  curve,
            thus  is  very   insensitive;   also,   it  is  greatly   affected   by  sorting   so  is  not  a  “pure”   measure
            of  skewness.   In  two  curves   with   the  same  amount   of  asymmetry,   one  with   poor   sorting
            will  have  a  much  higher   quartile   skewness   than  a  well-sorted   sample.

                  Graphic   Skewness.   As  a  measure   of  skewness,   the  Graphic   Skewness   (SkG)  given

            by  the  formula
                                                  9 I6$.&84$~50

            may  be  used  (Inman).   This  measures   the  displacement   of  the  median   from   the  average
            of  the  $16  and  $84  points   (see  figure   below),   expressed   as  a  fraction   of  the  standard
            deviation,   thus   the  measure   is  geometrically   independent   of  sorting.   The   derivation

                                                        Let   “x”  be  the  midpoint   of  the  $16  and  $84
                                                        values,   found   by  ($  I6  +  $84)  /2--in   this  case
    100%                                                (I  +3)  /2  or  2.0$.   Then   the  distance   “A”   is
                                                        the   displacement   of  the  Median   ($50)   from
    84%                                                 the  xAmidpoint.   The   skewness   measure   is
                                                        then  a

                                                              But  A  =  4  ’ y4   -  050,

                                                        and        o=   4@+-gW,

                                                        so  clearing   fractions   gives



                                                         In  this  case,           I +3-2(  I .5)
                                                                                  -7m--
      0%                                                Or   skG  =  +0.50.   Note   that   the   median   is
                                                        displaced   0.50   of   the   way   from   the   “x”
                                                        midpoint   to  the  $ I6  or  standard   deviation
                                                        mark.


                  lnctusive   Graphic   Skewness   (Sk,)  (Folk).   The   skewness   measure   discussed   above
           covers   only   the  central   68%  of  the  curve.   Inasmuch   as  most   skewness   occurs   in  the
            “tails”   of  the  curve,   this  is  not  a  sensitive   enough   measure.   A  much   better   statistic,
            one  that   includes   90%  of  the   curve,   is  the   Inclusive   Graphic   Skewness   given   by  the
            formula





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