soil shear strength_lecture
TRANSCRIPT
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PBWN302
CEM/WEE/STE
Dr.Asmaa
Moddather
SoilMechanicsandFoundations
FacultyofEngineering CairoUniversity
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Soil fail in shear.
Shear strength of soil is the internal resistance that the
soil mass offer to resist failure/sliding along any plane
.
ear a ure w occur at po nts w ere s ear stresses exceeds soils shear stren th S .
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Shear stresses are generated into the soil mass due to
.
The engineer needs to know the nature of shearing
o bearing capacity of foundations.
o stability of slopes.
o lateral pressure on retaining walls.
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FailuresurfaceStablemass
Bearing
capacity
of
Foundation
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Failuresurface
Stablemass
ta ty o s opes
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Directionofmovement
Failuresurface
Stablemass
lateral ressureonretainin walls
Failuresurface
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1. oca a ure ta es p ace at po nts w ere s ear stresses() > shear strength (S).
2. When local failure occurs at sufficiently large numberof oints within the soil mass a eneral failure takesplace.
3. a ure a es e orm o s ng o a so oc over aFailure/Sliding/Slip surface within the soil mass.
To study shear failure at a point, we need to calculate:
1. Stresses (, ) on any plane through this point
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2. Shear resistance S at this point
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ons er ng a certa n po nt ns ethe soil mass and knowing the
y
norma an s ear s ressesacting on two planes at this point:xy
x
o What is the maximum and
minimum normal stresses
xx
xy
magnitude and direction ?
o What is the maximum shear
xy
stresses (magnitude anddirection)?
y
o What is the normal () and shear
stresses actin on an lane?
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t s a grap ca met o to presentthe state of stress along any plane
pass ng roug any po n w n esoil mass. y
Need to define and signxy
x
o For :
xx
xy
Compression
+ve sign
Tension ve signxy
o For :
Rotation clockwiseve si n
y
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Rotation anticlockwise +ve sign
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y
ane
tressesonp anea: x,xy
Stressesonplaneb:( , x )
xy
xy
ane a
xx
xyMohrs circle
xy
y
a
o
yxy
bxy
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Mohrs circle
x
yxy
xy
Plane a
xy
xy
a
y
ox
yxy
Every point on the circle represents the state of stress acting on a
plane passing through the soil element.
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There are infinite number of planes passing through the element.
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Plane b
maxc
xx
xyxy
Plane a
aMinor principal
plane (3, 0)Major principal
plane (1, 0)xy
xy
b
y
mind
Maximumandminimumnormalstresses:
o Majorprincipalplane(1,0)
3,
Maximumandminimumshearstresses:
o Planec
+ /2
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o Planed((1+3)/2,min)
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Plane b
xx
xyxy
Plane a
a xyxy
,
b
y
Pole
Define: Pole
parallel to any plane, the line will intersect the circle at a point
whose coordinates are and actin on this lane.
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Plane b
xx
xyxy
Plane a
axy
xy
plane
by
Poleorizonta
plane
HowtofindthePole?
Needtoknowthefollowingaboutasingleplane:
o Stateofstress( and)
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o Directionofplane
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Plane b
maxc
xx
xyxy
Plane a
aMinor principal
plane (3, 0)Major principal
plane (1, 0)xy
xy
1
b
y
Pole
23
mind
Knowingthelocationofthepole,determinethedirectionof:
1, ,
o Minorprincipalplane(2,withhorizontal,clockwise)
o
Plane
with
maximum
shear
stress
( ,
with
horizontal,
clockwise)
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o Planewithminimumshearstress(4,withhorizontal,anticlockwise)
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estateo stresson2perpen cu ar
laneswithinasoilelementisshownin2 t/m2
theoppositefigure.DrawMohrscircle, 1.5 t/m2
anddetermine:
5 t/m25 t/m
.
whichtheyact. 2
ii.Maximum
shear
stress
and
the
Soil Element
.
iii.Thestateofstressonaplaneinclined
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20o anticlockwisewithhorizontal.
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22 t/m
2
2Plane b
, .
Stresses on plane b: (+2, +1.5) t/m25 t/m2
5 t/m2
Plane a
2 t/m2Note: horizontal
and
vertical
axes
MUST
be
drawn
withthesamescale 2
b Pole
o (t/m2)
a
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t/m2
max
b3 Pole
o 1
3
2
(t/m2)
a
i.Principle stresses ( = 0):
1: Major principle stress = 5.62 t/m2, 1 = 68
o clockwise, with horizontal
3: Minor principle stress =1.37 t/m2, 2 = 158
o clockwise, with horizontal
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Maximum shear stress: max = 2.12 t/m2, 3 = 23
o anticlockwise, with horizontal
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t/m2
b20
Pole
(t/m2)
(1.39, 0.18)
(t/m2)
a
iii.
State of stress at plane inclined 20o anticlockwise with horizontal:
= 1.39 t/m
2
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= 0.18 t/m2
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o Frictionandinterlockingbetweensoilparticles Friction
componento Interparticleattractionforces(duetoelectrochemicaleffects)
Cohesioncomponent
function of the effective normal stress () acting on plane of
failure: ''' tancS +=
where, c and are the shear strength parameters
c: effective cohesion
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: effective angle of shearing resistance
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Mohr-Coulomb shear strength
failure envelope
c
'''
f tancS +==
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Shear strength
failure envelope
(f, f)
c
Elastic equilibrium
ast c equ r um
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,
between particles ():
v.loose
versus
v.
dense
o Gradation:
poor ygra e versuswe gra e
small large
o
Particle
shape:roundedversusangular
small large
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o Particlesurface
roughness
(as
roughness
increases,increases)
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orcoarsegra ne so :
o
ranges
rom
27o
to
45o
dry wet
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Forfine
rained
soils,
S
de ends
on
friction
and
interlockin
o Stresshistor overconsolidation ratio :
betweenparticles()aswellascohesion(c):
asOCR
increases,
S
increases
,
floculated hashigherS
:
asdisturbanceincreases,Sdecreases
o Soi permea i ity water rainage :
Shearstrength
of
soil
loaded
under
drained
conditions(slowly)isdifferentfromthat
c
loadedunderundrained conditions(quickly)
Drainedshearstrengthversusundrained shear
stren th
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Shear strength parameters for a particular soil are
determined by means of laboratory tests on specimens
sampled from insitu soil.
Great care is required in sampling, storage, and handling
o samp es pr or o es ng, espec a y n case o
undisturbed samples where it is necessary to preserve the
in
situ structure and water content of soil.
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Shearboxapparatus.
ProvingringShearbox
Vertica isp acement ia gage
Motor,applieshorizontal
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Weightstoapplynormalload
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s a ev ce use to measure orce. t cons sts
of an elastic ring of known diameter with a
measuring device located in the center of the
r ng t at measures ts e ect on.
,
by which we convert the readings of the
measuring device (deflection) into force.
Force = proving ring reading x calibration
constant.
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c e m a co s ear oxappara us:
oa ngp a e
Samplemaybecircularorsquare
~
2
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Boxissplitinto2halves
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1. ssem e eappara us samp e,porouss ones, erpaperneeded),shearboxparts)andfillshearboxwithwaterifneeded.
2. pp y
norma
orce
on
top
o
s ear
ox
1 .3. Shearforceisappliedtospecimenbymovingonehalfofthebox
relativetotheothertocausefailureinthesoilspecimen.Shearingforceismeasuredbyprovingringorloadcell.
Pictureofsampleafterfailure
4. ert ca v an or zonta h sp acementsaremon tore duringthetest.
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5. Repeatsteps
2,
3,
and
4
for
different
normal
forces
(N2,N3).
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1. Foreach
test,
calculate:
Normalstress()=normalforce/areaofsample
Shearstress()=shearforce/areaofsample
2. Plot:
Peak
ress,
Densesand
shearstrength
Densesandec
imen,
v
nsion
Shearst
f heightofsp
Expa
ion Sheardisplacement,h
sandf
==constantLoosesand
Chang
ein
Com
pres
Loosesandandnormallyconsolidatedclayresultinsimilar(h andvh
Sheardisplacement,h
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Densesandandoverconsolidated clayresultinsimilar(h andvhrelationships)
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3. or es 1,ge 1 an max1=f1.
Fortest2,get2 andmax2=f2.
, 3 max3= f3.
4. Plot:
Test (2)
Test (3)
(3, f3)
Test (1)
(1,f1)
, ote: or zonta an vert ca
axesMUST
be
drawn
with
the
samescale
c
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1. enera y, rec s ear es s are con uc e on ry san , sa ura e san ,
and saturated clay.
2. For sands, soil has high permeability, water drains instantaneously
ur ng e es , u = 0 ur ng s ear ng, ere ore, = roug ou
the test.
3. For clays, to maintain = throughout the test (similar to sands), the
es s con uc e s ow y so excess pore wa er pressure u can ra n
during shearing.
4. Measured shear strength parameters: c, called drained/effective
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s ear strengt parameters.
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oreac es ,we now an f on a urep ane,w c s or zon a .
(,f) Pole
cMinor principal
plane (3, 0)Major principalplane (1, 0)
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s ear ox test carr e out on a s ty c ay so , gave t e
followin results:
235.6176.6117.758.9Verticalload(N)
8..1..2Provin
rin
dial
au ereadin
mm
If the shear box area is 36 cm2 and the proving ring
,
and the angle of shearing resistance.
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xamp examp e
235.6176.6117.758.9Verticalload(kg)
8.97.15.33.2rov ngr ng a gaugerea ng
(mm)
132.75105.7578.75
=3.2x15
Horizontalforce, H
(kg) =47.25
=6.544.913.27
.
=1.64 (kg/cm2)
3.692.942.19=47.25/36
=
(kg/cm2)
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xamp examp e4.00
3.50
2.50
.
(kg/cm
2)
1.50
2.00
arStress,
1.00Sh
0.00
.
0.00 0. 0 1.00 1. 0 2.00 2. 0 .00 . 0 .00 . 0 .00 . 0 6.00 6. 0 .00
c
Normalstress, (kg/cm2)c = 0.60 kg/cm2
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= 25o
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1. Simple
2. Not expensive
Disadvantages:
. ,weakest plane (might overestimate strength).
. , ,
are adjusted such that u = 0..
specimen is not uniform (stress concentration at corners).
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Provingring
Test
specimen
Dialgageforvertical
displacementTriaxialcell
Triaxialcell
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Filterpaper
Rubbermembrane
OringsTop/bottom
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Porousstones
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Verticalload
Transparentcylinder
Orings
Confiningpressure
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Air is released SamplePlacement
Open valve
Air release valve
Top drainage
Loading ram
Transparent cylinder
Porous stone
Specimen
Porous stone
Membrane
Open valve
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All around
Pressure supply
o om ra nage
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SamplePlacement:
1. Trim
sample
to
required
dimensions
(h/d
~ 2).
2. P acesamp eon ottom i terpaperan porousstone.
3. ace
op
er
paper,
porous
s one,
an
oa ng
cap.
. .
6. Lowerloadin bar usttorestonloadin ca .
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oa ng ages:
o Sta eI
l in confinin ressure( )
Openvalve
Open/closedvalve
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aroun
Pressuresupply
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Applyingaxialload(N)
Deviatorstress
(d)
oa ng ages:
o Sta eII
l in confinin ressure( )
Openvalve
Open/closedvalve
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aroun
Pressuresupply
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o Stage1:
Apply
confining
pressure
(c)
= cell
pressure.o Sta e2:
Increaseaxialload(N)uptofailure.Axialload/areaofspecimen
iscalled
deviator
stress
.
c c+df
cc cc
+
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Stage(1) Stage(2)
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ra nage con ons ur ng s ages 1 an 2 are se accor ng orequired type of test.
c c + df
cc cc
Valve (open/closed) Valve (open/closed)
c
c + df
Valve opened
Valve closed
Valve opened
Valve closed
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Consolidated, C
Unconsolidated, U
Drained, D
Undrained, U
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c c +df
cc cc
Valve (open/closed) Valve (open/closed)
Stage (1)
cStage (2)
c + df
Consolidated, C Unconsolidated, U Drained, D Undrained, U
Stage 1 Stage 2 Test Type
-
C U Consolidated-Undrained (CU)
U U Unconsolidated-Undrained UU
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U D Unconsolidated-Drained (UD) ever one
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c c df
cc cc
c
c+df
Note:
Stage 2
c 3
c
+df
=1Stage 1
Minor principal plane Major principal plane
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Pole(c, 0) (c+df, 0)
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c c + df
cc cc
Valve (open) Valve (open)
Stage (1)
cStage (2)
c + df
Consolidated, C Drained, D
= =
c c + df1 =
1 =
3 = 3
3 = 3
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1 1 1 1
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StressstrainRelationships:
s,d
OCC
OCCecimen,
V
nsion
e
viatorStre
NCC
df
v
olumeofs
Expa
sion Axial Strain, v
D
NCCChangein
Compres
Axial Strain, v
d v V v
relationships)
Dr.Asmaa Moddather PBWN302 Fall2012
oosesan
an
norma y
conso a e
c ay
resu
n
s m ar
d
van
Vv
relationships)
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Mohr circle at failure
dStage I
tage
1fdf3
1
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1f(2) 3(2)1f(1)3(1)c=0
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OCC NCC
pc
c1
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c c + df
cc cc
Valve (open) Valve (closed)
Stage (1)
cStage (2)
c + df
Consolidated, C Undrained, U
= =3 c c
c c + df1 =
1 =u =
3 = 3
u = va ue measure uring test
3 = 3 - u
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1 = 1 1 = 1 - u
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StressstrainRelationships:
s,d OCC
OCCressure
,u
ve
e
viatorStre
NCC
df
p
orewater
Axial Strain, v
D
NCCChangein
+ve
Axial Strain, v
Dense sand and overconsolidated cla result in similar ( and u
relationships)
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v v
relationships)
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u = +ve =
1 = 1u decreases
Same diameter
Mohr circle at failure
Mohr circle at failure
(Total stresses, measured)
ective stresses, ca cu ate
'c=0
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u u
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= -c c, ,
3 = 3u increases
1 = 1u increases
o Ifc>pc, soil behaves as NCC, u = +ve
3 = 3u decreases
=
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Overconsolidated Cla (OCC)
Mohr circle at failure
Mohr circle at failure
OCC
ect ve stresses, ca cu ate(Total stresses, measured)
2
c1
pc
u1 u2
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3 4u=-veu=+ve
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Drainage conditions during stages 1 and 2 are set according to
re uired t e of test.
c
c
+ df
cc cc
Valve (open/closed) Valve (open/closed)
c
c + df
Valve opened
Draina e allowed
Valve closed
Draina e not allowed
Valve opened
Draina e allowed
Valve closed
Draina e not allowed
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Consolidated, C Unconsolidated, U Drained, D Undrained, U
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c c + df
cc cc
Valve (closed) Valve (closed)
Stage (1)
cStage (2)
c + df
Unconsolidated, U Undrained, U
= =
c c + df1 =
1 =d . . dc . . c
Measured u during shearing = uc + ud +ve (NCC), -ve (OCC)
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One effective stress circle to all
total stress circles calculatedSame diameter
Mohr circle at failure
Total stresses measured
u= 0
1
'3 1(1)3(1)
cu
3(2) 1(2)
u(1) (-ve)
u(2) (+ve)c =undrained shearstren th
Note: increasingc doesntresultinanyincreasein3
Dr.Asmaa Moddather PBWN302 Fall2012
Sinceall
3
prior
to
shearing
is
the
same
in
all
samples,
the
strength
of
the
sampleswhenshearedwillbethesame.
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Loadingframe
Provingring
(measuresaxialdisplacement)
Sample
SpecialcaseofUUtest
o c =0
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o Verysimple
and
quick
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amp e acemen :
. ~ .
. .
as drying will alter samples characteristics considerably.
3. Lower loading piston until it contacts specimen.
4. Begin the test, continue until load values decrease or until20 strain is reac e .
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Ao A
Bulging
H
Ho H
ConstantV =
HAAH oo
testbeforeafter test
=
AAHA oooo
ooo
===
=
%
AA o=
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)(1)HH(1H)(H
o
o 100
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Readings:Load(F),verticaldisplacement(H)
Data
Reduction: a o
o where: Ho =initialsampleheight
o Stress: =F/Ac
c o a
Ao =initial
x
sectional
area
of
the
sample
DataPlotting:
Dr.Asmaa Moddather PBWN302 Fall2012
o Plotstress
() versus
axial
strain
(a)
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Stress,
qu
Strain, (%)
a,f
qu =unconfinedstrength
Dr.Asmaa Moddather PBWN302 Fall2012
cu =undrained shear
strength
=
qu/2
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qu
c
= 0 c = 0
u = 0
cu
qu0.0
u
3
1
=
= qu
0
qu =unconfinedstrength
Dr.Asmaa Moddather PBWN302 Fall2012
cu =undrained shear
strength
=
qu/2
UnconsolidatedUnconsolidatedUndrainedUndrained (UU Test(UU Test
versusUnconfinedCompressionTestversusUnconfinedCompressionTest
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pp
One effective stress circle to all
total stress circles (calculated)Same diameter
Mohr circle at failure(Total stresses, measured)
c = 3 = 0
u= 0
1 '3 1(1)3(1)
u
3(2) 1(2)
u(UC)u(UU1)
u(UU2)
=
Dr.Asmaa Moddather PBWN302 Fall2012
u
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ra ne
s ear
s reng
parame ers:
o c' OCC
o : NCC,sand
Theseparametersareobtainedfrom:
o CDTest
o Usedtodesignstructuresforlongtermcondition Drained.
Dr.Asmaa Moddather PBWN302 Fall2012
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Undrained shearstrengthparameters:
o cu, u=0 ,
eseparametersareo ta ne rom:
o
es
Dr.Asmaa Moddather PBWN302 Fall2012
Undrained.
xamp examp e 11
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The following results were obtained at failure in a series of
.
i. Determine the shear strength parameters of this soil.
ii. If a specimen is subjected to a confining pressure of 150 kPa
, .
on n ngpressure
(kN/m2)
ev a ors ress
(kN/m2)Test
1003501
210102
Dr.Asmaa Moddather PBWN302 Fall2012
xamp examp e 11
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1= c+df3= cc
2
df2
Test
4501001003501
6202102104102
' .
c'=119kN/m2
620c'
'=12o
450100 210
Note: sincec>0,thisclayis
Dr.Asmaa Moddather PBWN302 Fall2012
OCC,and
pc >210kN/m2
xamp examp e 11
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ii. If a specimen is subjected to a confining pressure of 150 kPa and a
deviator stress of 200 kPa would it fail? Comment.
350150
c
Elastic equilibrium
Dr.Asmaa Moddather PBWN302 Fall2012
xamp examp e 22
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Aclayspecimenfailedatunconfinedstrengthvalueof400kN/m2
when lacedinanunconfinedtesta aratuswhatwouldbethe
undrained shearstrength
for
the
tested
specimen?
u =0
Undrained Shearstrength:
0.0
400
u
cu =
qu/2
=
400/2
=
200
kN/m2
Dr.Asmaa Moddather PBWN302 Fall2012
xamp examp e 33
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,
(sampleheight=10.4cm,samplediameter=4.2cm),Findtheunconfined
strengthandtheundrained shearstrengthforthetestedsample.(Ao =13.85
cm2,Ho =10.4cm).
1112171613940Load(kg)
0.3500.3000.1110.0 00.0530.0340.0130.0
3.3652.8851.0670.7690.5100.327=0.013x100/10.40.0 =H/Ho (%)
=0.125
14.3414.2714.0013.9613.9213.9013.85A
(cm2
)0.125
13.85=A
=13.87
100
)100
(%)(1
=
Dr.Asmaa Moddather PBWN302 Fall20120.770.841.211.150.930.65
=0.290Stress(kg/cm2) 87.13
4.0=
xamp examp e 33
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1.20
1.40
qu
1.00
(kg/cm
2)
0.60
.
ialStress,
0.20
.Ax
0.00
0.00 0.50 1.00 1.50 2.00 2.50 3.00 3.50 4.00
Axial Strain, a (%)
Unconfinedstrength:qu =1.21kg/cm2
Dr.Asmaa Moddather PBWN302 Fall2012
Un raine S earstrengt :
cu =
qu/2
=
0.61
g/cm
2