Geotechnology Fundamental Theories of Rock and Soil Mechanics.

88
Geotechnology Fundamental Theories of Rock and Soil Mechanics

Transcript of Geotechnology Fundamental Theories of Rock and Soil Mechanics.

Page 1: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

GeotechnologyFundamental Theories of Rock and Soil Mechanics

Page 2: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

GeotechnologyI. Theory of Rock and Soil Mechanics

A. Stress

1. Concept

Stress = Pressure = ???

Page 3: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

GeotechnologyI. Theory of Rock and Soil Mechanics

A. Stress

1. Concept

Stress = Pressure = Force Area

Page 5: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

A. Stress

2. Primary Forces (natural)

Page 6: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

A. Stress

2. Primary Forces (natural)

a. Gravitational Forces (overlying

materials and upslope activity)

Page 7: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

A. Stress

2. Primary Forces (natural)

b. Tectonic Forces

“Important for Virginia and the Eastern Seaboard?”

Page 8: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

A. Stress

2. Primary Forces (natural)

c. Fluid Pressures (‘quick conditions’)

Page 9: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

GeotechnologyI. Theory of Rock and Soil Mechanics

A. Stress

3. Secondary Forces (Human Induced)

Page 10: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

Geotechnology3. Secondary Forces (Human Induced)

a. Excavation and Mining

Page 11: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

Geotechnology3. Secondary Forces (Human Induced)

b. Loading

Page 12: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

Geotechnology3. Secondary Forces (Human Induced)

c. Other

* Blasting

* Tunneling

* Pumping of Fluids

Page 13: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

4. Stress (σn ) on a plane normal to Force

σn = Force / AreaWhere n = ‘normal’, or stress perpendicular To the cross sectional area

Page 14: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

5. Stress on an inclined plane to Force

σ = Force / Area

Θ = angle to normal

Where inclined area = A = An/cos Θ

Page 15: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

5. Stress on an inclined plane to Force

σ = Force / Area

Where is 1)Normal Force and 2)Shear Force = ??

Page 16: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

5. Stress on an inclined plane to Force

σ = Force / Area

Where Normal Force and Shear Force = ??

cos Θ = a h

sin Θ = o h

Page 17: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

5. Stress on an inclined plane to Force

σ = Force / Area

Where Normal Force and Shear Force = ??

cos Θ = a = Fn h = F

sin Θ = o = Fs h = F

Page 18: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

5. Stress on an inclined plane to Force

σ = Force / Area

Where Normal Force and Shear Force = ??

Fn = F cos ΘFs = F sin Θ

cos Θ = a = Fn h = F

sin Θ = o = Fs h = F

Page 19: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

5. Stress on an inclined plane to Force

A reminder…

Fn = F cos ΘFs = F sin Θ A = An/cos Θ

Page 20: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

5. Stress on an inclined plane to Force

Stress Normal = Force Normal / Areaσn = {F cos Θ} / {An/cos Θ}

Stress Shear = Force Shear / Areaτ = {F sin Θ} / {An/cos Θ}

A reminder…

Fn = F cos ΘFs = F sin Θ A = An/cos Θ

Page 21: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

5. Limits:(max) σn when Θ = 0(min) σn when Θ = 90

(max) τ when Θ = 45(min) τ when Θ = 0 or 90

Page 22: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

Example Problem Given: Force = 10 lbs, Area (normal) = 5 in2

Determine σn and τ when Θ = 0 °, Θ = 30°, Θ = 45°, and Θ = 60°

Page 23: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

Example Problem Given: Force = 10 lbs, Area (normal) = 5 in2

Determine σn and τ when Θ = 0 °, and Θ = 30°

σn = {F cos Θ} / {An/cos Θ} = (10 lbs * cos 0)/(5 in2/cos 0) =

τ = {F sin Θ} / {An/cos Θ} = (10 lbs * sin 0)/(5 in2/cos 0) =

Page 24: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

Example Problem Given: Force = 10 lbs, Area (normal) = 5 in2

Determine σn and τ when Θ = 0 °, and Θ = 30°

σn = {F cos Θ} / {An/cos Θ} = (10 lbs * cos 0)/(5 in2/cos 0) = 2 lbs/in2

τ = {F sin Θ} / {An/cos Θ} = (10 lbs * sin 0)/(5 in2/cos 0) = 0 lbs/in2

Page 25: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

Example Problem Given: Force = 10 lbs, Area (normal) = 5 in2

Determine σn and τ when Θ = 0 °, and Θ = 30°

σn = {F cos Θ} / {An/cos Θ} = (10 lbs * cos 30)/(5 in2/cos 30) = lbs/in2

τ = {F sin Θ} / {An/cos Θ} = (10 lbs * sin 30)/(5 in2/cos 30) = lbs/in2

Page 26: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

Example Problem Given: Force = 10 lbs, Area (normal) = 5 in2

Determine σn and τ when Θ = 0 °, and Θ = 30°

σn = {F cos Θ} / {An/cos Θ} = (10 lbs * cos 30)/(5 in2/cos 30) = 1.50 lbs/in2

τ = {F sin Θ} / {An/cos Θ} = (10 lbs * sin 30)/(5 in2/cos 30) = 0.87 lbs/in2

Page 27: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

Example Problem Given: Force = 10 lbs, Area (normal) = 5 in2

Determine σn and τ when Θ = 0 °, and Θ = 45°

σn = {F cos Θ} / {An/cos Θ} = (10 lbs * cos 45)/(5 in2/cos 45) =

τ = {F sin Θ} / {An/cos Θ} = (10 lbs * sin 45)/(5 in2/cos 45) =

Page 28: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

Example Problem Given: Force = 10 lbs, Area (normal) = 5 in2

Determine σn and τ when Θ = 0 °, and Θ = 45°

σn = {F cos Θ} / {An/cos Θ} = (10 lbs * cos 45)/(5 in2/cos 45) = 1.00 lbs/in2

τ = {F sin Θ} / {An/cos Θ} = (10 lbs * sin 45)/(5 in2/cos 45) = 1.00 lbs/in2

Page 29: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

Example Problem Given: Force = 10 lbs, Area (normal) = 5 in2

Determine σn and τ when Θ = 0 °, and Θ = 60°

σn = {F cos Θ} / {An/cos Θ} = (10 lbs * cos 60)/(5 in2/cos 60) = 0.5 lbs/in2

τ = {F sin Θ} / {An/cos Θ} = (10 lbs * sin 60)/(5 in2/cos 60) = 0.87 lbs/in2

Page 30: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

5. Limits:(max) σn when Θ = 0(min) σn when Θ = 90

(max) τ when Θ = 45(min) τ when Θ = 0 or 90

Do your answers conform to the trends shown here?

Page 31: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

6. Stress (σ) in 3 dimensions

Stress at any point can be ‘resolved’ via3 mutually perpendicular stresses:

σ1 , σ2 , σ3

Where σ1 > σ2 > σ3

Page 32: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

B. Strain

“your ideas??”

Page 33: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

B. Strain

1. Strain Effects

Page 34: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

B. Strain 1. Strain Effects a. Stress produces deformation

Strain = dL L

Page 35: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

B. Strain 1. Strain Effects a. Stress produces deformation

“phi”

Page 36: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

B. Strain 1. Strain Effects a. Strain Ellipse

Maximum Shear Stress:Where σ1 - σ3

2

Page 37: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

2. Stress – Strain Diagrams

σ

ε“which material is stronger?”

Page 38: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

II. Elastic Response A. Young’s Modulus (E) “best shown in rocks”

E = stress σ strain ε

“The greater E is, ……?

“elastic limit”

Page 39: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

II. Elastic Response A. Young’s Modulus (E) “best shown in rocks”

E = stress σ strain ε

“The greater E is, the less deformation per unit stressOR“the stronger the material”

Page 40: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

An Example:

Page 41: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

II. Elastic Response B. Poisson’s Ratio (ν)

ν = lateral strain length strain

In compression

In tension

Page 42: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

II. Elastic Response C. Ideal Elastic Behavior

Page 43: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

II. Elastic Response D. Non-Ideal Elastic Behavior

Strainhardening

Page 44: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

“under repeated loads”

II. Elastic Response

E. Hysteresis

Soft Rock

Hard Rock

‘delayed feedback’

Page 45: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

II. Elastic Response

F. Stress-Strain in Soils

Limits of Proportionality (how much of the strain is Elastic?)

AssumesOM, MD

Page 46: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

“under repeated loads”

II. Elastic Response

G. Repeated Loading of Soils (when rolled)

Increment of permanent strain decreases (densification)

Page 47: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

III. Time-Dependent Behavior – Strain

A. Creep – under static loads

Elastic response occurs instantaneously

Page 48: Geotechnology Fundamental Theories of Rock and Soil Mechanics.
Page 49: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

Collapsed Culvert, Cincinnati, OH

Page 50: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

III. Time-Dependent Behavior – Strain A. Creep – under static loads

Page 51: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

III. Time-Dependent Behavior – Strain

B. Specific Rocks

Page 52: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

III. Time-Dependent Behavior – Strain

C. Griggs Relationship

Page 53: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

III. Time-Dependent Behavior – Strain

D1. Pavements

“The Benkelman Beam measures the deflection of a flexible pavement under moving wheel loads.”

Page 54: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

III. Time-Dependent Behavior – Strain

D2. Mines

compression

tension

Steel is strong in tension;Transfer Load to more confined(stronger) rocks.

Page 55: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

III. Time-Dependent Behavior – Strain

D. Mines

compression

tension

Steel is strong in tension;Transfer Load to more confined(stronger) rocks.

Page 56: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

“One of the most important engineering properties of soil is their shearing strength,or its ability to resist sliding along internal surfaces within a mass.”

IV. Shearing Resistance and StrengthA. Introduction

•Internal Friction•Cohesion

Page 57: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

“One of the most important engineering properties of soil is their shearing strength,or its ability to resist sliding along internal surfaces within a mass.”

IV. Shearing Resistance and StrengthA. Introduction

•Internal Friction•Cohesion

“One of the most important engineering properties of soil is their shearing strength,or its ability to resist sliding along internal surfaces within a mass.”

Page 58: Geotechnology Fundamental Theories of Rock and Soil Mechanics.
Page 59: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

An example of basic principles of friction between two bodies….

Φ

Φ

Page 60: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

An example of basic principles of friction between two bodies….

Φ

Φ

Φ

Page 61: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

An example of basic principles of friction between two bodies….

Φ

Φ

Φtan Φ = τ / σnormal

Page 62: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

Φ

ϴ

Page 63: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

Our governing equations…..

Φ

Φ

ϴ

Page 64: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

Φ

Φ

ϴ

(cosΘ)*(cosΘ)

Page 65: Geotechnology Fundamental Theories of Rock and Soil Mechanics.
Page 66: Geotechnology Fundamental Theories of Rock and Soil Mechanics.
Page 67: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

IV. Shearing Resistance and StrengthB. Triaxial Test for Soils & Mohrs Circles

“Strength of material ~ cohesion and angle of internal friction”

τ = c + σnormal * tanΦ

τ = shear stress on failure planec = cohesionσnormal = stress normal on failure planeΦ = angle of internal friction

Page 68: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

σ3

σ1

0 10 20 30 40

10

0

stress(lbs/in2)

stress(lbs/in2)

Mohrs Circles

8 lbs/in2

33 lbs/in2

Page 69: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

ϕ ϴ

Φ = angle of internal frictionϴ = angle between σ3 and

horizontal plane

OB = σ1

OA = σ3

OE = σnormal DE = τ (shear stress)

Φ

τ (s

hear

str

ess)

σ1σ3

Page 70: Geotechnology Fundamental Theories of Rock and Soil Mechanics.
Page 71: Geotechnology Fundamental Theories of Rock and Soil Mechanics.
Page 72: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

An example……

Page 73: Geotechnology Fundamental Theories of Rock and Soil Mechanics.
Page 74: Geotechnology Fundamental Theories of Rock and Soil Mechanics.
Page 75: Geotechnology Fundamental Theories of Rock and Soil Mechanics.
Page 76: Geotechnology Fundamental Theories of Rock and Soil Mechanics.
Page 77: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

An Example Problem:

The following Triaxial tests were performedon multiple samples of the same soil:

Test σ3 (psi) σ1 (psi)A 7 32B 17 61C 23 76D 31 92

IF: A minimum confining load (σ3) is required to stabilize a vertical load of 70 psi

DETERMINE:• σn• τ• angle of internal friction• cohesion

An example to get you started…

Page 78: Geotechnology Fundamental Theories of Rock and Soil Mechanics.

The slides that follow are extra material for your review as needed…..

Page 79: Geotechnology Fundamental Theories of Rock and Soil Mechanics.
Page 80: Geotechnology Fundamental Theories of Rock and Soil Mechanics.
Page 81: Geotechnology Fundamental Theories of Rock and Soil Mechanics.
Page 82: Geotechnology Fundamental Theories of Rock and Soil Mechanics.
Page 83: Geotechnology Fundamental Theories of Rock and Soil Mechanics.
Page 84: Geotechnology Fundamental Theories of Rock and Soil Mechanics.
Page 85: Geotechnology Fundamental Theories of Rock and Soil Mechanics.
Page 86: Geotechnology Fundamental Theories of Rock and Soil Mechanics.
Page 87: Geotechnology Fundamental Theories of Rock and Soil Mechanics.
Page 88: Geotechnology Fundamental Theories of Rock and Soil Mechanics.