Saturated soils
voids are filled completely with water
Dry soil
voids are filled completely with air
Fines
Clay and Silt
Sand
0.06 - 2 mm
Gravel
2 - 60 mm
Cobbles
60 - 200 mm
Boulders
> 200mm
Coefficient of Angularity
Fu = 4πA/l^2
where A = cross-sectional area
and l = perimeter
Roundness Coefficient
R = r/x
Plastic Limit
wPL: water content below which fine soil behaves brittle and crumbly
To determine wPL
- wPL is defined as the moisture content w when threads become brittle
Liquid Limit
wLL: water content above which fine soil behaves as a liquid
To determine wLL
BS: standard fall-cone tests
- usually carry out several tests at different w and draw a straight line between w and fall distance
US: use a Casagrande apparatus, cut V-shape in soil - count number of standard taps to cause the cut to disappear
- test requires more “judgement” than the fall - cone
Clays
- the higher the wLL, wPL and PL, the more plastic the clay (i.e. the more it will shrink, swell and change volume)
Non-plastic silts
-
Soil Classification
35% fines = “fine”
Static Compaction
Dynamic Compaction
Vibro-compaction
very deep compaction
Proctor Compaction Tests
laboratory method of experimentally determining the optimal moisture content at which a given soil type will become most dense and achieve its maximum dry density
Standard Proctor Test Method
Modified Proctor Test Method
Compaction
densification of soil by expulsion of air and the rearrangement of particles
Benefits of compaction