3.1 Origin and classification of rocks and soils Flashcards
Define soil for geological engineering
Soil is any uncemented or weakly cemented accumulation of particles formed by the weathering of rocks and the void space between the particles containing water or air.
Types of weathering
- Mechanical (physical): Results in rock being broken down into smaller particles that have the same mineralogical composition as the parent rock
- Chemical: caused by rainwater reacting with the mineral grains in rocks
Two types of soils
Residual soils: formed by weathered products at their place of origin
Transported soils: moved from place of origin (more common)
Why are clays different that sands or gravel?
They are not just very small rocks
Clay mineralogy
Is what the clay is composed of on a molecular scale
Explain two ways to determine particle size distribution
Mechanical analysis: coarse grains - % Gravel, Sand, Fines
Hydrometer analysis - % Silt vs Clay
Dispersive soils
high erosion potential
Well graded vs poorly graded
Well graded: means poorly sorted
Poorly graded: Very well sorted
Mechanical weathering mechanisms and soils
Alluvial soils: Moved or transported by running waters
Glacial soils: Moved or transported by glaciers
Lacustrine soils: Deposited in lakes
Marine soils: Deposited in the ocean
Aeolian soils: Deposited by wind
Colluvial soils: deposited or transported by rock fall or gravity
Atterberg limits
How does soil behave under different moisture contents
Types of Atterberg limits
Shrinkage limit (SL)
Plastic Limit (PL)
Liquid Limit (LL)
Plasticity Index (PI)