πŸ§—πŸ» Soil Consistence

Soil Consistence, Crusting, Compaction

  • Soil consistence is defined as β€œthe resistance of a soil at various moisture contents to mechanical stresses or manipulations”.
  • It combines both the β€˜cohesive’ and β€˜adhesive’ forces, which determine the ease with which a soil can be reshaped or ruptures.

πŸ‘‰πŸ» Soil consistence is described at three moisture levels namely β€˜wet’, β€˜moist’ and β€˜dry’.

1. Wet soils

  • Consistency is denoted by terms stickiness and plasticity
  • Stickiness is grouped into four categories namely
    • non sticky
    • slightly sticky
    • sticky
    • very sticky
  • Plasticity of a soil is its capacity to be moulded (to change its shape depending on stress) and to retain the shape even when the stress is removed.
  • Soils containing more than about 15% clay exhibit plasticity – pliability and the capacity of being molded. There are four degrees in plasticity namely
    • non plastic
    • slightly plastic
    • plastic
    • very plastic

2. Moist soil

  • Moist soil with least coherence adheres very strongly and resists crushing between the thumb and forefinger. The different categories are
    • Loose-non coherent
    • Very friable - coherent, but very easily crushed
    • Friable - easily crushed
    • Firm - crushable with moderate pressure
    • Very firm - crushable only under strong pressure
    • Extremely firm - completely resistant to crushing. (type and amount of clay and humus influence this consistency)

3. Dry soil

  • In the absence of moisture, the degree of resistance is related to the attraction of particles for each other. The different categories are
    • Loose - non coherent
    • Soft - breaks with slight pressure and becomes powder
    • Slightly hard - break under moderate pressure
    • Hard - breaks with difficulty with pressure
    • Very hard - very resistant to pressure
    • Extremely hard - extreme resistance and cannot be broken

Soil crusting

  • Formation Mechanism: Soil crusts usually are formed as a result of compaction at the immediate surface due to an externally applied force. This force is supplied primarily by the impact of raindrops as the soil is wetted and the radiant energy of the sun as the soil dries. When the rain drops fall on dry soil.
  • Soil Strength is determined by penetrometer.

Soil Compaction

  • Soil compaction is defined as the method of mechanically increasing the density of soil.
  • In construction, this is a significant part of the building process. If performed improperly, settlement of the soil could occur and result in unnecessary maintenance costs or structure failure.
  • Almost all types of building sites and construction projects utilize mechanical compaction techniques.
  • Soil consistence is defined as β€œthe resistance of a soil at various moisture contents to mechanical stresses or manipulations”.
  • It combines both the β€˜cohesive’ and β€˜adhesive’ forces, which determine the ease with which a soil can be reshaped or ruptures.

πŸ‘‰πŸ» Soil consistence is described at three moisture levels namely β€˜wet’, β€˜moist’ and β€˜dry’.

1. Wet soils

  • Consistency is denoted by terms stickiness and plasticity
  • Stickiness is grouped into four categories namely
    • non sticky
    • slightly sticky
    • sticky
    • very sticky
  • Plasticity of a soil is its capacity to be moulded (to change its shape depending on stress) and to retain the shape even when the stress is removed.
  • Soils containing more than about 15% clay exhibit plasticity – pliability and the capacity of being molded. There are four …

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