2.3. Plasticity and Structure of Soil (Shrinkage Limit) Flashcards
the moisture content, in percent, at which the volume of the soil mass ceases to change
Shrinkage Limit
T or F. Soil shrinks as moisture is gradually lost from it. With continuing loss of moisture, a stage of equilibrium is reached at which more loss of moisture will result in no further volume change.
True
Shrinkage Limit: 8.5 - 15
Montmorillonite
Shrinkage Limit: 15 - 17
Illite
Shrinkage Limit: 25 - 29
Kaolinite
the moisture content, in percent, at which the volume of a soil mass ceases to change as it gradually loses moisture
Shrinkage Limit (SL) (ASTM D-427, ASTM D-4943)
the moisture content, in percent, at which the volume of the soil mass ceases to change
Shrinkage Limit
T or F. Soil shrinks as moisture is gradually lost from it. With continuing loss of moisture, a stage of equilibrium is reached at which more loss of moisture will result in no further volume change.
True
Shrinkage Limit: 8.5-15
Montmorillonite
Shrinkage Limit: 15-17
Illite