斯坦福大学老师课件
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4540353025
20751.2 1.1 1.00.90.80.750.70.650.60.550.550.50.450.40.35
0.30.250.20.15
(G = 2.68)0.50.450.40.350.30.250.20.15
8090100110120130140150
φ` Obtained from effective stress failure envelopes approximate correlation is for cohesionless materials without plastic fines
ML SM SP SW GP GW R e l a t i v e D e n s i t y 100%i n t h i s r a n g e a n d 025%50%75%Angle of Internal Friction Vs Density (For Coarse Grained Soils)
Adapted from NA VFAC DM-7.1 (5/82) p 7.1 - 149
Correlations Of Strength Characteristics For Granular Soils
Material Type A n g l e o f I n t e r n a l F r i c t i o n φ`(D e g r e e s ) Dry Unit Weight (γD
), PCF V oid Ratio, e
Porosity, n
Coefficient of Consolidation Vs Liquid Limit
Adapted from NA VFAC DM-7.1 (1982)
3
2
10-2
10-3
10-4
Liquid Limit (LL)
(C v ), F T 2/d a y C o e f f i c i e n t o f C o n s o l i d a t i o n (C v ), C m 2/s e c 8
8
654
3
2
654
8
6543
2
210.70.50.30.20.1
0.070.050.030.020.010.0070.00520406080100120140160Undisturbed Samples:C v in Range of Virgin Compression C v in Range of Recompression Lies Above this Lower Limit Completely Remolded Samples:C v Lies Below this Upper Limit 0.40
0.350.300.250.200.150102030
405060708090U n d r a i n e d S t r e n g t h R a t i o Plasticity Index, I p (percent)
Adapted from Ladd (1991), JGE, ASCE, 117(4) Comparison of field and laboratory undrained strength ratios for nonvarved sedimentary soils (OCR = 1 for laboratory CK o U testing)
Note: C u = S u Undrained shear strength for design (stability analyses)Note: Linear Regression Lines for Clay Data ********
*
Source of Strength Data A- Line Above Below Field c u /σp : Larsson (1980)Lab CK o U τave /σvc :Table 4Lab CK o UDSS τh /σvc : MIT *c u /σp τh /σvc τave /σvc
50403020
10
00204060801002004006001000
F r
i
c
t
i
o
n
A n
g
l
e
,
φ',
D e
g
r e
e
s Plasticity Index, I p , percent
Soft and Stiff Clays, and Shale Compositions
Clay Minerals
φ
' (oc) Data from
Table 3NC Values of Friction Angle φ' for Natural Clay Compositions NC For σ
p /σn Range of 10 to 20
For σ
p /σn Range of 2 to 5
σp = 4100 kPa
c c
30002000
1000
02000400060008000
S h
e
a r
S
t
r
e s
s
,
k P
a
σn = Effective Normal Stress, kPa
φPeak Strength against Effective Normal Stress Relationship of London Clay Sample from 35 m Depth (Data from Bishop et al. 1965)
10,000
10,00
100
101
0.110100100010,000100,000
c
p σ= 0.024
10 (Table1)
10
c
p σ= 0.10
c
,
k
P
a σp , kPa
Relationship between Cohesion Intercept and Preconsolidation
Pressure
Adapted from Mesri & Adel - Ghaffar (1993), JGE, ASCE, 119(8)
2 to 5
10 to 20
n σp σin /σn Range of