Soils and Materials Flashcards
Moisture content calculation
((wet - dry weight)/wet) x 100
Calculating liquid limit
The liquid limit is defined as the
water content at which the groove
cut into the soil will close over a
distance of 13 mm following 25
blows.
parameters gained from shear test
Cohesion
angle of internal friction
Soil description order
Strength
Colour
Structure
Soil type
Additional info
Determination of Liquid Limit tests (atterberg limits)
One-point Casagrande method (line in soil closing 13mm after 25 blows)
Cone penetrometer method (moisture content at which a standard cone will
penetrate a distance of 20 mm in 5 seconds)
Atterberg Limits
basic measure of the critical water contents of a fine-grained soil
L– for low plasticity soil (liquid limit < 50)
H– for high plasticity soil (liquid limit > 50)
Liquid limit
Plastic limit PI=0.73(LL-20)
Shrinkage limit
What is Cohesion
property of like molecules (of the same substance) to stick
to each other due to mutual attraction (e.g. soil particles).
what is Adhesion
the property of different molecules or surfaces to cling to each
other (e.g. soil & water).
What is the proctor test and how is it performed
used to obtain the maximum dry density of compaction and the optimum moisture content
The soil is mixed with varying amounts of water, then compacted in 3 equal layers in a standard mould using a 2.5kg rammer
Parameters gained:
The maximum dry density and optimum moisture content is
determined from the results of the test.
what is Compaction
process of increasing the bulk density of a soil or aggregate by removing the air voids trapped within. The density achieved is very much dependent on the moisture content
Importance of the proctor test
- It gives density that must be achieved in the field.
- Provides the moisture range that allows for minimum compaction
effort to achieve density. - Provides data on the behaviour of the material in relation to various
moisture contents. - It is not possible the determine if a soil density test passes or fails
without it.
Determination of coefficient of permeability, (k) tests
The constant-head test (For permeable soils (k>10-3 mm/sec)) FOR MEDIUM TO COURSE SOILS
The falling-head test (variable-head), (For less permeable soils (k<10-3
mm/sec)) FOR SAND
Unit weight of water
1000 kg/m3
Specific gravity of soil
Gs = Density soil / Density of water
typically varies between 2.6 and 2.8
enables the volume of solid particles to be
calculated from mass or weight.
coefficient of permeability calculation
From Darcy Law
𝑘 =𝑞/𝐴i
q = flow rate = mm3 of liquid / time in seconds
A = cross sectional area of sample
i = h/L = change in head height mm/length of sample mm