Top Banner
41

The material properties of each layer are homogeneous Each layer has a finite thickness except for the lower layer, and all are infinite in.

Dec 16, 2015

Download

Documents

Hilary Wilkins
Welcome message from author
This document is posted to help you gain knowledge. Please leave a comment to let me know what you think about it! Share it to your friends and learn new things together.
Transcript
Page 1: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.
Page 2: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.
Page 3: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.
Page 4: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.

• The material properties of each layer are homogeneous • 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 5: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.

At any point, 9 stresses exist. They are 3 normal stresses (sz, sr, st) and 6 shearing stresses ( trz

=tzr; tr t = ttr; ttz =tzt) • 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 s1(major), s2 (intermediate) and s3 (minor).

Page 6: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.
Page 7: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.

Boussinseq assumptions: 1.soil is ideal mass; 2.soil are homogenous; 3.possion`s ratio is constant in all

directions, and E is constant; 4.soil is isotropic , that mean x =

Page 8: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.

One –Layer Systems

Page 9: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.

Vertical stress beneath the centre of the loaded area:

Page 10: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.
Page 11: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.
Page 12: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.
Page 13: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.
Page 14: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.
Page 15: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.
Page 16: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.
Page 17: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.
Page 18: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.
Page 19: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.
Page 20: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.
Page 21: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.
Page 22: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.
Page 23: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.
Page 24: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.
Page 25: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.
Page 26: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.
Page 27: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.
Page 28: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.
Page 29: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.

Pavement stresses , strains and deflections are caused by:

1.traffic loading, 2.daily or seasonal temperature

and moisture changes; 3.changes in the conditions of

pavement support.

Page 30: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.

The general assumptions of the multi-layer theory are:

1.Materials used in each layer is homogenous; 2.Finite thickness of layer; 3.Infinite lateral dimensions; 4. Isotropic properties; 5. Full friction at layer interfaces; 6 .Shear forces at surface =0; 7 .Each layer’s material is characterized by

Poisson’s ratio (u) and elastic modules (E).

Page 31: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.

Equivalent single wheel load (ESWL)

ESWL defined as the load on a single tire that will cause an equal magnitude of pre-selected parameter (stress, strain, def.), to that resulting from a multiple wheel load at the same location from the pavement.

There are two methods for determination the ESWL , based on equal stress and equal deflection.

Page 32: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.
Page 33: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.

Solution (1) For dual system a = (Q/ p)0.5 = (9000/3.14 x90)0.5 =

5.64 in. Max. stress at point (a) = 1 + 2 Load (1): z/a = 30/5.64 =5.32, r/a =0.0 From z influence curve (Fig.58) stress ratio = 5.1/ 90 1 =Pt x stress ratio = 90 x(5.1/90) =5.1

psi.

Page 34: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.

load (2): z/a = 5.32, r/a =5.32 2 = pt x stress ratio = 90x(0.95/90)

=0.95 psi. Total = 5.1 + 0.95 = 6.05 psi b) For ESWL max. = Pt x stress ratio = 6.05 stress ratio = 6.05 / Pt = 6.05 / 90 = 0.067 By using the chart: r/a = 0.0 , stress ratio = 0.067 x 90 = 6.05 z/a = 5 = 30 / a a = 6.0 in. PE = .Pt. a2 = 3.14x 90x 6x6 = 10.174 Ib.

Page 35: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.
Page 36: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.
Page 37: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.

The design methods are classified to three main groups as follows:

1. Theoretical methods; 2. Empirical methods; 3. Empirical-theoretical

methods.

Page 38: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.

These methods can be classified into three groups:

1-Methods based on soil classification tests , as example group index method.

2-Methods based on soil strength tests as CBR-, asphalt institute-and national crushed stone association method.

3-Methods based on the results of road tests as AASHO and road test method.

Page 39: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.

Fig.69 shows an approximation of desirable total permanent th. based on truck traffic volume and the group index of the subgrade. This method is simple, but has many limitations and it could be lead to an over -or under designed pavement.

Page 40: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.

Modified CBR method or asphalt institute method is shown in Fig.71. By using this method , pavement thickness depends upon traffic classification . Tab.27 shows the determination of each class . The relation between traffic classification and wearing surface thickness is in Tab.28.

Page 41: The material properties of each layer are homogeneous  Each layer has a finite thickness except for the lower  layer, and all are infinite in.