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1.3 Shear Strength of Clays.

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(1)

SNU Geotechnical and Geoenvironmental Engineering Lab.

1.3 Shear Strength of Clays.

(1) Drained Strength.

NC Clay OC Clay

drained

UU behavior UU behavior

τ

, '

n n

σ σ

su su

'

pc

8 . 0

(max. past pressure)

0

φ = φ =0

φ'

τ

, '

n n

σ σ

(2)

SNU Geotechnical and Geoenvironmental Engineering Lab.

“Fundamental Sear Strength Parameters”

- Hvoslev Parameter.

ce, φe

- Work based on lab tests of saturated remolded clays.

Physico-chemical Forces (Intrinsic Forces)

Attractive Forces, A.

1) Electrostatic attraction.

2) Van der Waal’s Force.

(3)

SNU Geotechnical and Geoenvironmental Engineering Lab.

Repulsive Forces, R.

1) Electrostatic repulsion.

- Factors affecting intrinsic forces.

1. Type of clay.

2. Particle spacing.

3. Geometric arrangement of particles.

4. Specific surface.

(4)

SNU Geotechnical and Geoenvironmental Engineering Lab.

- Effective stress equations.

R A u + −

= σ σ '

Sshear strength=Sgranular +Scohesive

e e

c c

g

c g

c g

c u

K R A K

K u

K R A u K

u S

S S

+

=

− + +

=

− +

− +

= +

=

φ σ

σ

σ σ

tan ) (

) (

) )(

(

) (

) (

Equivalent friction angle.

→material constant.

Equivalent cohesion.

(5)

SNU Geotechnical and Geoenvironmental Engineering Lab.

For NC Clay. (drained test)

f

f Mohr

Mohr Mohr

Mohr---Coulomb failure envelope-Coulomb failure envelopeCoulomb failure envelopeCoulomb failure envelope

e e e Hvorslev e

Hvorslev Hvorslev

Hvorslev failure envelopefailure envelopefailure envelopefailure envelope

(6)

SNU Geotechnical and Geoenvironmental Engineering Lab.

→ No longer 1 failure envelope, but a series of envelope for Hvorslev theory.

.

f

f Mohr

Mohr Mohr

Mohr----Coulomb failure envelopeCoulomb failure envelopeCoulomb failure envelopeCoulomb failure envelope

Hvorslev Hvorslev Hvorslev

Hvorslev failure envelopefailure envelopefailure envelopefailure envelope

(7)

SNU Geotechnical and Geoenvironmental Engineering Lab.

For O.C. Clay.

Ideal Soils → No ∆e during unloading.

In terms of Hvorslev parameters;

For any unloading (OCR > 1).

constant constant

=

=

e e

c φ

log P' log P' log P' log P'

e e e e

typical data typical datatypical data typical data

idealized data idealized data idealized data idealized data

σ’

(8)

SNU Geotechnical and Geoenvironmental Engineering Lab.

Practical decrease in strength due to increase in e during ‘actual’ unloading → So, Hvorslev ideal envelope (O.C. Clay) → upper bound strength.

Composite envelope (idealized)

ideal

practical τ

ce

σ'

φ'

φe

(9)

SNU Geotechnical and Geoenvironmental Engineering Lab.

Summary

An increase in effective stress has two effects on strength of clays.

1. Increase particle to particle contact forces.

→ increase in frictional resistance. → S =(σ −u) tanφe

increase 2. Decrease volume and void ratio, and increase (A-R) and ce.

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