๐Casagrande apparatus: used to determine liquid limit.
๐ Oedometer is used to find the consolidation characteristic of soil.
๐ Hydrometer is used to determine grain size distribution
๐ Plate load test is used to determine safe bearing capacity of soil.
๐Pycnometer method is the laboratory method for determining specific gravity as well as water content of soil sample
๐Permeameter is used to find hydraulic conductivity and permeability of soil sample.
๐Core cutter is a field method to compute bulk density of soil.
๐ Increasing order of their grain size:
Montmorillonite < Illite < Kaolinite
๐Sequence of plasticity index
Montmorillonite > Illite > Kaolinite
๐ Relative compaction: Degree of compaction achieved as a percentage of the laboratory compaction
Relative compaction = dry density in field/ maximum dry density from the proctor test
๐Relative density can be zero but relative compaction can never be zero.
๐with increase in temperature, viscosity decreases and permeability increases.
k ∝ Unit weight/ Viscosity
๐Effective stress increases, void ratio decreases and permeability decreases.
๐Organic matter has the tendency to move towards flow channel and choke them, thus reduces permeability
๐ Entrapped air decreases the permeability of soil.