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CT2 Study Notes
Course: Construction Technology 2 (Substructure) (300721)
18 Documents
Students shared 18 documents in this course
University: Western Sydney University
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CT2 STUDY NOTES 2012 MODULE 1-6
Module 1:
The strength of foundations
Foundation Soils are fairly incompressible. Footings and retaining walls mainly fail when the soil
particles are shifted sideways and upwards. Buildings can be designed to float on poor foundation
soil. The soil shears when it moves sideways. One layer of soil moves to the side in relation to the
main bulk of the soil. This behaviour occurs ground coupled construction systems, including footing
beams, slabs and retaining walls.
Shearing Strips
A building cannot fail by compression of the soil, therefore the shear capacity of the soil determines
the load-carrying capacity of the footing. The ability to resist shear is important for soil.
Prediction of Shear Strength
Two mechanisms, soil resist loads by cohesion and friction between the soil particles.
Cohesion is important in clayey soils
It results from, chemical bonding amongst soil particles and between the soil particles and water in the
pores. The type of chemical bonding depends on the moisture content, electrolyte concentration and
the compaction of the soil.
Flocculent Clay Structure
Capillary forces within the soil pores. Menisci develop within the soil voids that are capable of binding
the soil together. Capillary forces are optimised at a particular moisture content. The meniscus is an
example of surface tension
Apparent cohesion in soil
Meniscus will spread the forces like an arch, moisture content is to high then the pore is overwhelmed
and cannot develop and if it's to low it cannot develop as well. Friction is caused by the physical
interlock of soil particles, frictional resistance is more important in sandy or granular soils, larger sized
particles soils usually possess greater frictional properties. Clay particles are smooth and are platelets
Dispersed clay structure
FF are important in sandy soils, sand particles are rougher then sand :S, less chance of slippage
between particles also known as cohesion less soils.
Theories of shear strength
There are two types of shear resistance have been developed in two theories.
The Coulomb Theory
Failure occurs when the supported weight exceeds the shear capacity of soil. The weight on the soil
has reached a limit that is related to the bonding within the soil. Work done with an excavated depth
greater than 1.5 metres is classified as high risk construction work and a MSDS is required.
The Mohr Theory