Chapter II Deformation Analysis

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Advanced Soil Mechanics I SNU Geotechnical and Geoenvironmental Engineering Lab. Chapter II Deformation Analysis 2.1 Stress Distribution in Soil ex) What is settlement caused by embankment loading? σ Δ (Applied Stress) γ = h v σ Δ = ( stress induced by σ Δ ) 1-D loading If NC clays, consolidation settlement, 0 0 0 ' ' log 1 v v c c H e C S σ σ σ Δ + + = B Δσ=γh NC clay Sand v σ Δ 0 ' v σ H

Transcript of Chapter II Deformation Analysis

Advanced Soil Mechanics I

SNU Geotechnical and Geoenvironmental Engineering Lab.

2-1 Chapter II

Deformation Analysis

2.1 Stress Distribution in Soil

ex) What is settlement caused by embankment loading?

σ∆ ≡ (Applied Stress) γ= h

vσ∆= ( ≡stress induced by σ∆ )

→ 1-D loading

If NC clays, consolidation settlement,

0

0

0 '

'log

1 v

vc

c He

CS

σσσ ∆+

+=

B

∆σ=γh

NC clay

Sand

vσ∆

0'vσ

H

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2-2 When B/H ≥ 1, then 1-D loading (under center of structure) is valid.( vσ σ∆ = ∆ )

When B/H<1, then we must calculate stress distribution throughout soil mass.(∆σ ≠∆σv)

P

vσ∆ A

Sand

Clay

AP /=∆σ

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2-3 � Notes

- In case that 1-D loading condition is no longer valid,

ⅰ) σσ ∆≠∆ v

ⅱ) vu σ∆≠∆

ⅲ) 0≠ε∆ h

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2-4 � Use elasticity to calculate the stress distribution.

⇒ Boussinesq approach.

Assumptions

1. Soil is homogeneous and isotropic.

2. Soil is linear elastic.

3. Semi-infinite soil mass (No rigid base nearby).

4. Perfectly flexible footing.

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2-5 Can get

1. good estimate of vσ∆ .

2. but poor estimate of hσ∆ (unless plane strain condition)

L/B ≥ 5

( → Generally consolidation settlement is estimated by vu σ∆=∆ and 0hε = )

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2-6 � Stress Distributions

- Point load : depth ≥ 3 times of width(diameter) of square ft (circular ft).

- Line load : depth ≥ 3 times of width of strip ft.

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2-7 1. DM 7.1-165, Formulas for stresses

Figure 2. Formulas for Stresses in Semi-Infinite Elastic Foundation 7.1-165

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2-8

Figure 2(continued)Formulas for Stresses in Semi-Infinite Elastic Foundation 7.1-165

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2-9 2. DM 7.1-167, Difference between square and strip footings

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2-10- PIz ×=σ

3. DM 7.1-168, Vertical stress beneath a corner of a uniformly loaded rectangular area

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2-116. DM 7.1-169, Vertical stress under uniformly loaded circular area

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2-125. DM 7.1-170, Vertical stress under embankment load of infinite length

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2-136. DM 7.1-171, Vertical stress under corner of triangular load

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2-14- Comments on charts

i) Stresses penetrate further for larger loads.

ii) If the size of footing increases, stresses penetrate further.

iii) Stresses for strip footing penetrate further than stresses for square or circular footing.

iv)For square or rectangular footing, stresses other than corner can be found by

superposition.

at

center 4×=∆ PIcenter σ

at corner

PIPI BCDGABCDEFc −=∆σ

A B

C

F

G D

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2-15- Rule of thumb to find critical depth

critical depth : depth at which soil compression contributes significantly to surface

settlements

i) Sands Depth at which vσ∆ is 20% of the in situ, effective stresses( vo

'σ )

ii) Clays ≥∆ vσ 10% of vo

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2-16� Newmark charts (�useful for irregular loaded area)

1. Determine location and depth(z), where stress increment is desired to obtain.

2. Adopt a scale such that the distance OQ(=1 inch) in Fig. is equal to the depth z.

(i.e. if z=30ft, scale is 30ft)

3. Draw the plane of loaded area to scale determined in (2).

4. Place the plane on Newmark chart with point under consideration over the center.

5. Count the number of blocks, N, of the influence chart which fall inside the plane.

6. Calculate vσ∆ as qFNv =∆σ

where, q = applied stress and,

F = influence value of charts (=0.001)

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2-17

Fig. 3.50 Influence chart for vertical stress σz(=∆σv) (Newmark, 1942)

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2-18•••• Comments on Stress Distributions

1. Use superposition for areas with different applied pressures.

2. For embedded structures,

�Conservative (i.e. higher loads), because shear resistance of soil at boundary between

embedded structure and soil is neglected.

→ Use this to get ∆σv

� superposition

-(∆σv)1

+(∆σv) 2

∆σv = (∆σv) 2 - (∆σv) 1

D γ P

� Vertical load

at depth, D is (P- γD)

or

γD + P

At ground

surface

At depth, D

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3. Vertical stresses are affected by layering, if soils have much different E values.

4. Stiff layer at ground surface dissipates the induced stresses rapidly.

(Hand out Fig 6-4 in p2-15, 7.1-179 in p2-16)

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2-20

Figure 6-4. Basic pattern of Burmister Two-Layer Stress Influence Curves

(Strip footing)

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7.1-179