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Table  5-1.-Classification  of  Pits  and  Quarries
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Types of Quarry Material

exposed to the atmosphere, it undergoes a physical and chemical  process  called  WEATHERING,  which,  over  a sufficient length of time, disintegrates and decomposes the rock into a loose, incoherent mixture of gravel, sand, and finer material. Soil Quality The intended use of the soil is the determining factor in the quality required. In general, soil used for fills and subgrades do not have to meet the same specifications as those used for compacted rock surfaces, base courses, or  pavements. Seven properties of rock are used to help select rock and aggregates for construction. Briefly, these rock properties  are  as  follows:  toughness,  hardness, durability, chemical stability, crushed shape, surface character,  and  density.  Toughness,  hardness,  and durability are commonly checked in the field with a simple  field  test. Hardness is the resistance of a rock to scratching or abrasion.  This  property  is  important  in  determining  the suitability of aggregate for construction. Hardness can be  measured  using  the  Mob’s  scale  of  hardness  (table 5-2). The harder the material, the higher its number on the Moh’s scale. Any material will scratch another of Table 5-2.-MOH’S Scale of Hardness Mineral Hardness Diamond   .   .   .   .   .   .   .   .   .   .   .   .   .   .   .   .   10 Corundum   .   .   .   .   .   .   .   .   .   .   .   .   .   .   .   9 Topaz   or   beryl   .   .   .   .   .   .   .   .   .   .   .   .   .   8 Quartz  .  .  .  .  .  .  .  .  .  .  .  .  .  .  .  .  .  .  .  .  .  7 Feldspar   .   .   .   .   .   .   .   .   .   .   .   .   .   .   .   .   .   6 Apatite   .   .   .   .   .   .   .   .   .   .   .   .   .   .   .   .   .   .   5 Fluorite   .   .   .   .   .   .   .   .   .   .   .   .   .   .   .   .   .   4 Calcite   .   .   .   .   .   .   .   .   .   .   .   .   .   .   .   .   .   .   3 Gypsum  .  .  .  .  .  .  .  .  .  .  .  .  .  .  .  .  .  .  2 Talc  .  .  .  .  .  .  .  .  .  .  .  .  .  .  .  .  .  .  .  .  1 Expedients Porcelain   .   .   .   .   .   .   .   .   .   .   .   .   .   .   .   .   7.0 Steel  file  .  .  .  .  .  .  .  .  .  .  .  .  .  .  .  .  .  .  6.5 Windowglass   .   .   .   .   .   .   .   .   .   .   .   .   .   .   5.5 Knife   blade   .   .   .   .   .   .   .   .   .   .   .   .   .   .   5.0 Copper  coin  .  .  .  .  .  .  .  .  .  .  .  .  .  .  .  .  3.0 Fingernail  .  .  .  .  .  .  .  .  .  .  .  .  .  .  .  .  .  2.0 equal or lesser hardness. In the field, hardness may be measured  using  the  common  expedients  shown  in  table 5-2; for example, when you are able to scratch a rock with a knife blade, the rock has a hardness of 5.0 or less. A rock which can be scratched by a copper coin has a hardness of 3.0 or less. Aggregates for general construction should have a hardness of 5 to 7 and should be difficult or impossible to scratch with a knife. Material with a hardness greater than 7 should be avoided since they cause excessive wear  to  crushers,  screens,  and  drilling  equipment. Material with a hardness of less than 5 may be used if other  sources  of  aggregate  prove  uneconomical. The  requirements  as  to  toughness,  durability, crushed  shape,  and  other  properties  vary  according  to the type of construction. Chemical stability has specific importance  when  considering  aggregates  for  concrete. Several  rock  types  contain  impure  forms  of  silica  that reacts with alkalies in cement. This reaction forms a gel that absorbs water and expands to crack or disintegrate hardened concrete. These reactive materials may be included  in  some  gravel  deposits  as  pebbles  or  as coatings on gravel. Potential alkali-aggregate reactions may be anticipated in the field by identifying the rock and  comparing  it  to  known  reactive  types  or  by investigating structures in which the aggregate has been used.  Generally,  light-colored  or  glassy  volcanic  rocks, chert, flints, and clayey rocks should be considered reactive  unless  proven  otherwise. An additional property of rock is gradation (fig. 5-1). This property is also important for evaluating rock as  possible  construction  material.  Gradation  is  the distribution  and  range  of  particle  sizes  that  are  present in, or can be obtained from, a deposit. The gradation of pit materials can be readily determined from a simple test. Quarry materials may be more difficult to evaluate. Figure  5-1.-Types  of  soil  gradation. 5-3

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