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7/28/2019 16partiia.pdf
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.1
.1
1 2 4
Overconsolidation Ratio, OCR
Undrained strength ratio vs. OCR from Field Vane Tests
a) Boston Blue Clay, I-95 Saugus; MA
b) Connecticut Valley Varved Clay, Amherst, MA;
c) Organic Clay with Shells, Fore River, ME;
d) Jmaes Bay B-2 and B-6 marine Clays.
FieldValueStrength,
Cu
(FV)/v
o
'
6 8
.20.20 0.16
0.17
.4
Connecticut
valley varved clay
m = 0.93
.6
.8
1.0
1 2 4 6 8
James Bay
Marine Clay
B-2 1.18 = m
B-6 1.35
.20.165
0.74
.4
Boston Blue
Claym = 0.96
Fore River
Organic Clay
Mean
m = 0.83
.6
.8
1.0
00.4
0.6
0.8
1.0
1.2
1.4
20
Plasticity Index, PI (%)
Fields vane correction
factor vs. plasticity index derived
from embankment failures.
C
orrectionFactor,
40 60 80 100
Bjerrum's (1972)
Recommended Curve
cu (Field) = x cu (Vane)
120
Bjerrum (1972)
Milligan (1972)
Ladd & Foott (1974)
Flaate & Preber (1974)
LaRochelle et al. (1974)
# Layered & varved clays
Symbol Reference
#
#
Figure by MIT OCW.
Figure by MIT OCW.
Adapted from:
7/28/2019 16partiia.pdf
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0
CHANDLER ON UNDRAINED SHEAR STRENGTH OF CLAYS
(1988)
0.2
0.6
0.8
Empirical correlation
established from
embankment failures,
Estimated time
effect, R
Estimated effect of
anisotropy
Modified
Azzouz et al., 29
(1983)ASCE JGE
Plasticity Index, Ip, %
Factors Relating Field Vane and Field Failure Strengths
CorrectionFactor,
1.0
0.4
20 40 60 80 100 120
(cu)field = (cu)vane. A . R
0.20 0.2
"NC" = Young,
Aged & Cemented
B2
}7 m
11 m
B6SEBJ Data
OC = Mechanically
OC=
Field Vane Correction Factor
PROBLEMS WITH NEW NGI FV CORRECTION
0.4
cu(Fv) / vo
Ckouave
Su(FV)
'
Corr
ectionFactor,
0.6 0.8 1.0
0.4
0.6
0.8
1.0
1.2
0.4
0.60 20
Plasticity Index, %
R
40 60 80 100 120
0.8
1.0
1.2
0 20
A
Plasticity Index, %
Factor Rto Correct Field Value Strength for Strain-Rate Effects
CHANDLER ON UNDRAINED SHEAR STRENGTH OF CLAYS
(1988)
R
40 60 80 100 120
0.6
Roy & Leblanc2
Wiesel 18
Torstensson 16
Estimated effect, R, relating
vane strength to field failures
(tf= 10,000 mins), Bjerrum 190.8
1.0
1.2
B Field vane correction
factor, Rto give cu at
tf= 100 mins
For Ip = 1.05 - 0.04 (Ip)0.5R5% :>
For Ip = 1.05 - 0.03 (Ip)0.5R5% :>
Figure by MIT OCW.
Figures by MIT OCW.
Adapted from:
Adapted from:
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eL vj/fI...
7e
I -::: : ::: -:.. .. : .1:. ... .:1i.:. : .... ...
::. _: i.
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-. .,j1 .
-11
Candler /s8)6sr? SP /0/4
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N rrl SFY Bj4erra(N
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')
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i:7=
s;;. -7,,7Ns: : ! -..... ..i~i r :
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1.322lI ... .. _.. .... ... ... d... ....
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80 lid0 6020 lo
7/28/2019 16partiia.pdf
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14
10
Depth(m)
Measured Cone Resistance, (qc)
and Pore Pressure (u) (kPa)
Effect of Pore Pressure
on Cone Resistance in Emmerstad
Quick Clay
6
qT
qT
uA
qc uB
A
B
B
A
2
0 200 400 600
14
10
Depth(m)
Corrected Cone Resistance,
qT (kPa)
6
2
0 200 400 600
Piezocone A
Piezocone B
qc
60o
A
60o
B
Figures by MIT OCW.
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1000
5
10
15
20
25
20 30
Plasticity Index, Ip (%)
Example of NK- Ip Correlation
as Proposed by Different Workers
Data are Inconsistent since the different cones
used had different area ratios.
ConeFactor,
NK
40 50 60 70 80
Scandinavian sites
Sites in U.S.A.
Canadian Sites
Italian Sites
Other Clays
NK=qc - vocorr. su(Fv)
Figure by MIT OCW.
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1
31
2
0
10
20ConeFacto
r,Nkt
Nkt=
qct-
vo
cu
(Conv.orDSS)
30
40
50
60
70
2
Overconsolidation Ratio, OCR
Cone Factor vs. OCR. Collective Evaluation for Harrison Bay and Smith
Bay Arctic Silts. (In situ temp -1oC)~~
4 6 8 10 20 40
32
23
1
Mukluk Proximal
Smith Bay, Site T
Smith Bay, Site W
Ice Gouged
Note:
Numbers designate areas in
table 6.1
* Mainly lab UUC & Mv
** Via SHANSEP with well
defined OCR
Solid : Cu = Cu(conv.)*
Open : Cu = Cu(DSS)**
CL - Ip
ML- MH Ip
25%}}
~~
10-30%~~
CH
Figure by MIT OCW.
Adapted from:
7/28/2019 16partiia.pdf
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Yc /'/9it ,222 I1 __-Su/ptnt Secor, 2.4
,Gs4X7 ,oK) t/ Aast Jpono~rcrcedfs on;8/~Sm/~wcwan ru~oeql ScXngves 4t /n/ftptfafiaof /n sA.e onen fion'" lfi , , coh~wr sodrtby hiLhn/Xfa I naectmy evti/usQz of d/tv4.lnize. 4 dS wY// pf .r#rntfro f6?mC. 6ony PrD thuis (/7O2)
Pt-2 Echmcfnt4c of SBp$?17 fOPrT /Pi/'T* -3 Sacrndlis 4m S /4//irnm PzPfMS /idto/S I*,*P1i-4 Pfccktn p ion CrrV(4 Qf- i of
oranof ctwio64aCe far OCE- /C~5PA-S Pr~dhtfdc s.fnts6rct expcnsxon 4xevacit ,C- c+ seC
,t6 Pr@/c/ccl s4/c o fimc7$anof Q ,Anf #ofc/Isnirbr ce or Ace / Ai6C.
btr Prec//4tconJ'ng 84//g~ (//5)*d;,4z PafZ* 4'odA/h/anclIft/ ;a,l7}/ 1etlu-h Ot node/
C. r ACg , ..............*in hu{,15 d co& o La) AAAW S ple
I~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~
f_z~;
Ic
- I
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Drilling Mud
Drill Pipe
Open Hole Drag Bit
Adiprene Membrane
Protective Strips
Cutting Shoe
Pressuremeter Head
Spacer
Pressure Developer
Figure by MIT OCW.
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Electro/Hydraulic Hose
Controle Unit
+ Read out
Push Head
Cone rods conducting hose
Standard cone rod
Cone rod adaptor
Amplifier housing
Contraction ring
Pressuremeter module
Contraction ring
Cone sapper
Dummy cone
400
705
720
Full Displacement or Cone Pressuremeter
Figure by MIT OCW.
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Spring
Feeler
Rubber Membrane
Fine Thread
Pore Pressure Cell
Clamp
Gas Return LineCable and Gas
Pressure Tube
Slurried water and soil
Flushing Water
Camkometer
Figure by MIT OCW.
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Inner SoilInner Soil
Outer SoilOuter
Soil
Cutter Location
Extracted
Soil
1
1
-1 -1
1
1 1
1
2
2
2
2
2 2
2
2
10
10
20 20
E = 5%
E =
5%
Ce
nterline
Centerline
5
1
0
0 0
0
t
B/2t
B/2
z/R
z/R
Push-in pressuremeter Ideal self-boring pressuremeter
r/R r/R
Figure by MIT OCW.
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0.001 0.01 0.1 1 10 1000.0
0.5
1.0
1.5
2.0
Volumetric strain, V/V (%)
Mem
braneexpansionpressure,
(p-u0
)/'
2
120.040
0.875
1.0
FDPMTPIPMT
INTACT
Ideal
SBPMT
MIT - E3 Predictions
BBC: OCR = 1.0
Aspect ratioExtraction ratio
B/tf
Figure by MIT OCW.
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0.00.01
Equivalent Volumetric Strain, V/V = {(1+0)2 -1}/(1+0)
2 (%)
M
embraneExpansionPressure,
(p-u0)v0'
0.1 1 10 100
1.0
2.0
3.0
4.0
5.0
f=0
f=1
Intact
Measured Data South Boston Test Site
(Ladd, 1991)
Measured
Arm 1 1.35Arm 2 0.68
Arm 3 0.68
'su/v0
Predicted
PIPMT (f = 0) 0.65SBPMT (f = 1) 1.01Intact 0.66
'su/v0
Figure by MIT OCW.
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1 10 500.0
0.1
0.2
0.3
0.4
0.0
0.1
0.2
0.3
0.4
PSA
PM
TE
PSA
PM
TE
0.0 0.2 0.4 0.6 0.8 1.0 1.2
Aspect ratio, B/t Extraction ratio, f
FDPMT PIPMT PIPMT SBPMT OvercuttingUndercuttingIdeal
Undrainedstreng
thratio.su/'v
o
OCR =1OCR =1
su
/'v
o
Peak Undrained shear strength
Expansion test = PMT
Contraction testHoulsby
Figure by MIT OCW.