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CE 261 Consultation

This document outlines the key concepts covered in 5 modules for a soil mechanics course. It discusses graphical methods for visualizing soil stresses including Mohr's circle and different shear strength tests. It also covers stress-strain behavior of soils under drained and undrained conditions, stress paths for triaxial tests, critical state soil mechanics concepts, and Taylor's method for computing friction angle from triaxial test data using finite differences.
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0% found this document useful (0 votes)
41 views11 pages

CE 261 Consultation

This document outlines the key concepts covered in 5 modules for a soil mechanics course. It discusses graphical methods for visualizing soil stresses including Mohr's circle and different shear strength tests. It also covers stress-strain behavior of soils under drained and undrained conditions, stress paths for triaxial tests, critical state soil mechanics concepts, and Taylor's method for computing friction angle from triaxial test data using finite differences.
Copyright
© © All Rights Reserved
We take content rights seriously. If you suspect this is your content, claim it here.
Available Formats
Download as PPTX, PDF, TXT or read online on Scribd
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CE 261

2nd Semester 2020-2021


Module 1
• Mohr Circle and the Pole Method are graphical methods whose main
purpose to help visualize the magnitudes and direction of stresses for
a given plane, as well as independently check computations made
using the formulas/expressions for computing stresses along a given
reference frame.
• Be familiar with initial and final Mohr Circles associated with different
shear strength tests.
• For undrained tests, there is an total and effective stress Mohr Circle.
Module 2
• Be familiar with the standard plots associated with different basic
tests.
• Test results within a test series a plotted together within a single
graphs.
• Some graphs with a common ordinate (independent variable) are
normally plotted one on top of another.
• There are three different failure criteria for triaxial tests
• Maximum principal stress ratio
• Maximum deviator stress
• Maximum strain
Module 3
•  Skempton’s Pore pressure parameters: and


• There are two conventions for stress paths:
• MIT: , , and
• Cambridge: , , and where .
Module 3
• For triaxial test (CL):
• Drained stress path is a 1H:1V (MIT)/ 1H:3V (Cambridge) straight line.
• Horizontal distance between corresponding points on the TSP and ESP
is equal to the pore pressure at the point in the test.
• A 1H:1V line drawn tangent to the (MIT) ESP corresponds to point of
maximum pore pressure.
• For soils with no cohesion, a line tangent to the ESP passing through
the origin corresponds to the point of maximum PSR.
Module 4
• There are four sources of friction in coarse grained soil (assuming
samples if fully saturated):
• Particle sliding
• Expansion/Dilation
• Particle rearrangement/reorientation
• Particle crushing
• Dense versus loose behavior are differentiated by:
• Dilation versus contraction, as well as the presence or absence of strain
softening under drained loading.
• Negative versus positive pore pressures during undrained loading.
Module 4
•  The dense versus loose behavior is dependent on the combination of
the initial void ratio and the confining pressure.
• Consequently, is not dependent only on void ratio, but also on the
confining pressure.
Module 5
•  Taylor’s method requires the computation of the from test data. In
the program ds_taylor.exe, the derivative is computed using finite
difference approximation.
• First point:
• Last point:
• All other points:
Module 5
•  A similar approach is used for subsequent methods for drained triaxial
tests.
• The correction is not applied if the sample undergoes a contraction
instead of a dilation.
• For samples undergoing strain softening, there is a peak angle of
internal friction and a residual angle of internal friction . For a given
confining pressure, the peak angle of internal friction varies with the
initial void ratio. However, the residual angle of internal friction is
independent of the initial void ratio.
Module 5
•  For a given confining pressure , a dense sample dilates and a loose
sample contracts until it reaches the critical void ratio . The
relationship between is referred to a the critical state line.
• In theory, samples shear without undergoing any volumetric strain in
the critical state .
• Experimentally, there are very slight differences from the state when
the sample shears within any volumetric strain (constant volume),
and the residual state .
Module 5
•  Taylor’s method requires the computation of the from test data. In
the program ds_taylor.exe, the derivative is computed using finite
difference approximation.
• First point:
• Last point:
• All other points:

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