Section 27-675. Classification of soil materials  


Latest version.
  • For  purposes of this
      subchapter,  soil  materials  shall  be  classified  and  identified  in
      accordance  with  table  11-1.  In addition, the following supplementary
      definitions shall apply.
        (a) Rock.
        (1) HARD SOUND  ROCK.  Includes  crystalline  rocks  such  as  Fordham
      geniss,   Ravenswood   geniss,   Palisades  diabase,  Manhattan  schist.
      Charateristics are: The rock rings when struck with pick  or  bar;  does
      not disintegrate after exposure to air or water; breaks with sharp fresh
      fracture;  cracks  are  unweathered  and less than one-eighth inch wide,
      generally no closer than three feet apart; core recovery with  a  double
      tube,  diamond  core  barrel is generally eighty-five percent or greater
      for each five foot run.
        (2) MEDIUM HARD ROCK. Includes crystalline rocks of paragraph  one  of
      this  subdivision,  plus  Inwood  marble and serpentine. Characteristics
      are: all those listed in paragraph one of this subdivision, except  that
      cracks  may  be  one-quarter inch wide and slightly weathered, generally
      spaced no closer than two feet apart; core recovery with a double  tube,
      diamond  core barrel is generally fifty percent or greater for each five
      foot run.
        (3) INTERMEDIATE ROCK. Includes rocks of paragraphs  one  and  two  of
      this  subdivision,  plus  cemented  shales  and  sandstone of the Newark
      formation.  Characteristics are: the rock gives dull sound  when  struck
      with  pick or bar; does not disintegrate after exposure to air or water;
      broken pieces may show weathered  surfaces;  may  contain  fracture  and
      weathered  zones  up  to one inch wide spaced as close as one foot; core
      recovery  with  a  double  tube,  diamond  core  barrel   is   generally
      thirty-five per cent or greater for each five foot run.
        (4) SOFT ROCK. Includes rocks of paragraphs one, two and three of this
      subdivision in partially weathered condition, plus uncemented shales and
      sandstones.  Characteristics  are: rock may soften on exposure to air or
      water; may contain throughly weathered zones up to three inches wide but
      filled with stiff soil; core recovery with a double tube,  diamond  core
      barrel  is  less  than  thirty-five  percent for each five foot run, but
      standard penetration resistance in soil  sampling  is  more  than  fifty
      blows  per  foot. Where core recoveries are less than twenty percent and
      the material is to be used for bearing, a minimum three inches  diameter
      core  shall  be recovered and the material recovered shall be classified
      in accordance with table 11-1.
        (b) Special soil types.
        (1) FINE SAND. Soils of group SM, containing more than  fifty  percent
      (by weight) of particles passing a number sixty mesh sieve.
        (2)  HARDPAN.  Soils  of  groups  GM,  GC,  and SW, generally directly
      overlying rock, and which are sufficiently cemented to be  difficult  to
      remove by picking.
        (3) CLAY SOILS. Soils of each group SC, CL, and CH shall be classified
      according to consistency as hard, medium, or soft in accordance with the
      following:
        a.  Hard clay. A clay requiring picking for removal, a fresh sample of
      which cannot be molded by pressure of the fingers.
        b. Medium clay. A clay that can be removed by spading, a fresh  sample
      of which can be molded by a substantial pressure of the fingers.
        c.  Soft  clay.  A  clay,  a  fresh sample of which can be molded with
      slight pressure of the fingers.
        (4) SILT SOILS. Soils of each group ML and MH shall be  classified  as
      dense, medium, or loose depending on relative difficulties of removal as
      described  for  hard,  medium, and soft clays in paragraph three of this
      subdivision.
    
        (5) VARVED SILT. A natural soil deposit consisting of alternating thin
      layers of silt, clay, and sand in which  the  silt  or  silt  plus  sand
      layers predominate.