Stresses and Strains in flexible Pavements

29
Stresses and Strains in flexible Pavements

Transcript of Stresses and Strains in flexible Pavements

Page 1: Stresses and Strains in flexible Pavements

Stresses and Strains in

flexible Pavements

Page 2: Stresses and Strains in flexible Pavements

Multi Layered Elastic System

Page 3: Stresses and Strains in flexible Pavements

Assumptions in Multi Layered

Elastic Systems

• The material properties of each layer are homogeneous – property at point Ai is the same at Bi

• Each layer has a finite thickness except for the lower layer, and all are infinite in lateral directions.

• Each layer is isotropic, that is, the property at a specific point such as Ai is the same in every direction or orientation.

• Full friction is developed between layers at each interface.

• Surface shearing forces are not present at the surface.

• The stress solutions are characterized by two material properties for each layer, i.e., (µ, E).

Page 4: Stresses and Strains in flexible Pavements

Stresses in Layered Systems

• At any point, 9 stresses exist. They are 3 normal

stresses (σz, σr, σt) and 6 shearing stresses

(τrz =τzr; τrt =τtr; τtz =τzt)

• At each point in the system there exists a certain

orientation of the element such that the shearing

stresses acting on each face are zero.

– The normal stresses under this condition are principal

stresses and are denoted by σ1(major), σ2

(intermediate) and σ3 (minor).

Page 5: Stresses and Strains in flexible Pavements

Computation of Strains

( ))(1

trzzE

σσµσε +−=

( ))(1

ztrrE

σσµσε +−=

( ))(1

zrttE

σσµσε +−=

Page 6: Stresses and Strains in flexible Pavements

One –Layer Systems• If, one-layer system is assumed as a homogeneous half space,

Boussinesq equations can be applied.

• Half space is an infinite large area with infinite depth with a top plane on which loads are applied.

• Boussinesq equations are developed for computing stresses in a homogeneous, isotropic and elastic media due to a point load at the surface.

– Stress is independent of the properties of the transmitting medium.

– Maximum stress occurs on the vertical plane passing through the point of load application, on a particular horizontal plane.

– Pressure is maximum at shallow depths, theoretically becoming zero at infinite depth. But, for all practical purposes, σz is taken as zero when z is sufficiently large.

2z

PKz =σ

( )[ ] 2521

1

2

3

zrK

+=

π

σzz

r

P

Page 7: Stresses and Strains in flexible Pavements

• Load is not a point load – it is distributed over an elliptical area. This contact area can be approximated to a circular shape.

• Variation of stress follows the same general pattern

• Vertical stress resulting from uniformly distributed circular load may be obtained by integration of Boussinesq equation.

• Love has obtained the following closed from equation for the vertical stress beneath the centre of the loaded area:

• Newmark has developed charts for foundation work for computing stresses

( )

+−=

2322

3

1za

zpzσ

One –Layer Systems

Page 8: Stresses and Strains in flexible Pavements

• Foster and Ahlvin (1954) developed charts for computing vertical, tangential and radial stresses. The charts were developed for µ = 0.5.

• This work was subsequently refined by Ahlvin and Ulery (1962) allowing for evaluation of stresses and strains at any point in the homogenous mass for any µ.

• Due to axis symmetry, there are only three normal stresses, σz, σr and σt and one shear stress τrz.

• One-layer theory can be applied as an approximation for a conventional flexible pavement with granular base/subbase with a thin asphaltic layer on a stiff subgrade comparable to the base/subbase. (i.e., E1/E2 ≅ 1)

• The deflection that occurs within the pavement (∆p) is neglected and therefore, the pavement surface deflection (∆T) is equal to the deflection on the top of subgrade (∆s)

∆T = ∆s + ∆p

∆p = 0

Therefore, ∆T = ∆s

E1, µ1, h1

E2, µ2, h2=α

∆T

∆p

∆s

One –Layer Systems

Page 9: Stresses and Strains in flexible Pavements

Charts for One-layer Solutions

by Foster and Ahlvin (1954)

These are applicable for µ = 0.5

Page 10: Stresses and Strains in flexible Pavements
Page 11: Stresses and Strains in flexible Pavements
Page 12: Stresses and Strains in flexible Pavements
Page 13: Stresses and Strains in flexible Pavements
Page 14: Stresses and Strains in flexible Pavements
Page 15: Stresses and Strains in flexible Pavements

Tables for One-layer Solutions

by Ahlvin and Ulery (1962)

Page 16: Stresses and Strains in flexible Pavements
Page 17: Stresses and Strains in flexible Pavements

Tables for Functions A to H

(after Ahlvin and Ulery)

Page 18: Stresses and Strains in flexible Pavements

Example problems on One-layer Systems

1. A homogeneous half space is subjected to a circular load, 254 mm in diameter. The pressure on the circular area is 345 kPa. The half space has an elastic modulus of 69 MPa and a Poisson's ratio of 0.5. Determine the vertical stress, strain and deflection at point A, which is located 254 mm below and 508 mm away from the centre.

2. A homogeneous half space is subjected to two circular loads, each 254 mm in diameter and spaced at 508 mm on centres. The pressure on the circular area is 345 kPa. The half space has an elastic modulus of 69 MPa and a Poisson's ratio of 0.5. Determine the vertical stress, strain and deflection at point A, which is located 254 mm below the centre of one of the wheels.

Page 19: Stresses and Strains in flexible Pavements

Example Problems Continued

3. Given the following data for the pavement shown in the figure,

compute the deflection at point m, σz and εr at point o and σ1,2,3 and τmax at point p.

a= 152 mm; p = 552 kPa

h1=254 mm; E1 = 173 MPa; µ1 = 0.35

E2 = 110 MPa; µ2 = 0.4

Coordinates of points:

m: (z=0, r=0)

o: (z=457, r=305)

p: (z=457, r=0)

E1, µ1, h1

E2, µ2, h2=α

Page 20: Stresses and Strains in flexible Pavements

Solutions at Axis of Symmetry

Page 21: Stresses and Strains in flexible Pavements

Deflection of Flexible Plate

Deflection Profile

Ground Reaction

Page 22: Stresses and Strains in flexible Pavements

Solutions at Axis of Symmetry –

Flexible Plate

( )

+−=

2322

3

1za

zpzσ

++

+

+−+=

2322

3

5.022

2

)()(

)1(221

2 za

z

za

pr

µµσ

( ))(1

trzzE

σσµσε +−=

( ))(1

ztrrE

σσµσε +−=

( ))(1

zrttE

σσµσε +−=

Normal stress at axis symmetry:

Radial stress at axis symmetry:

Strains can be computed from the following equations:

At the axis of symmetry, τrz =0 and σr = σt

Page 23: Stresses and Strains in flexible Pavements

∫∞

=∆

z

zz dzε

5.022

2

)(2

3

zaE

paz

+=∆

[ ]

−+−

++

+=∆ zza

aza

a

E

paz

5.022

5.022)(

21

)(

)1( µµ

Vertical deflection ∆z can be determined by

εzdz

z

E

paz

)1(22µ−

=∆

E

paz

5.1=∆

For µ = 0.5,

At z = 0,

At z = 0 and µ = 0.5,

Solutions at Axis of Symmetry –

Flexible Plate

Page 24: Stresses and Strains in flexible Pavements

Deflection of Rigid Plate

5.022)(2

)(ra

parp

−=

E

pao

2

)1(2µπ −

=∆

Deflection Profile

Ground Reaction

SteelUllidtz (1987) gave the

distribution of pressure under

a rigid plate as:

By integrating a point load

over the contact area of the

plate it can be shown that

E

pao

18.1=∆If µ = 0.5, then,

Page 25: Stresses and Strains in flexible Pavements

Two-layer Systems

• The effect of layers above subgrade is to reduce the stress and deflections in the subgrade.

• Burmister (1958) obtained solutions for two-layer problem by using strain continuity equations.

• Vertical stress depends on the modular ratio (i.e., E1/E2)

• Vertical stress decreases considerably with increase in modular ratio.

• For example,

for a/h1=1 and E1/E2 = 1, σz at interface = 65% of contact pressure

for a/h1=1 and E1/E2 = 100, σz at interface = 8% of contact pressure

Page 26: Stresses and Strains in flexible Pavements

Variation of Subgrade Stress with

Modular Ratio

Page 27: Stresses and Strains in flexible Pavements

Vertical Stress in a Two-layer System

Page 28: Stresses and Strains in flexible Pavements

Vertical Surface Deflection in a Two-

layer System

• Burmister (1958) dveloped a chart for computing vertical surface deflection in a two-layer system.

• The deflection factor, F2, is obtained from the chart based on the values of a/h1 and E1/E2.

• Then the deflection is computed from the following equations:

– Deflection under a flexible Plate =

– Deflection under a rigid Plate =

2

2

5.1F

E

paT =∆

2

2

18.1F

E

paT =∆

Page 29: Stresses and Strains in flexible Pavements

Vertical Surface Deflections for Two Layer Systems (Burmister, 1958)