Prepared by: Dr. Hetty

13
Prepared by: Dr. Hetty

Transcript of Prepared by: Dr. Hetty

Page 1: Prepared by: Dr. Hetty

Prepared by:

Dr. Hetty

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STRESS

(kN/m2)= .z where:

= unit weight of soil (kN/m3)

z = depth / thickness from ground surface (m)

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TOTAL NORMAL STRESS

Generated by the mass in the soil body, calculated by sum up the unit weight of all the material (soil solids + water) multiplied by soil thickness or depth.

Denoted as , v, Po

The unit weight of soil is in natural condition and the water influence is ignored.

Total stress increases with depth and with unit weight: Vertical total stress at depth z

zt .

z = The depth of point

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EXAMPLE 1 : Total stress in multi-layered in soil

3 m

4 m

4 m

t,1 = 17 kN/m3

t,2 = 18 kN/m3

t,3 = 18 kN/m3

·A

·B

·C

·D

1 m

2 m

A = t,1 x 1 m

= 17 kN/m2

B = t,1 x 3 m

= 51 kN/m2

C = t,1 x 3 m + t,2 x 4 m

= 123 kN/m2

D = t,1 x 3 m + t,2 x 4 m + t,3 x 2 m

= 159 kN/m2

The total stress at depth z (i.e. Point D) is the sum of the weights of soil in each layer thickness above.

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Pore water pressure (u)

Under hydrostatic conditions (no water flow) the pore pressure at a given point is given

by the hydrostatic pressure:

u = w .hw

Where

w = unit weight of water (9.81kN/m3 10 kN/m3)

hw = depth below water table or overlying

water surface

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Negative pore pressure

- Below the water table, pore pressures are positive. - In dry soil, the pore pressure is zero. - Above the water table, when the soil is saturated, pore pressure will be negative.

u = -(w .hw)

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EFFECTIVE STRESS

Defined as soil stress which not influenced by water pressure in soil body.

Published first time by Terzaghi at 1923 base on the experimental result

Applied to saturated soil and has a relationship with two type of stress i.e.:

Total Normal Stress ()

Pore Water Pressure (u)

Effective stress formula

u'

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EFFECTIVE STRESS

u'

z.tz.u w

z'.z).(' wt

@

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EXAMPLE 2

MAT Sand

sat = 18.0 kN/m3

d = 13.1 kN/m3

Clay

sat = 19.80 kN/m3

h1 = 2 m

h2 = 2.5 m

h3 = 4.5 m

x

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EXAMPLE

Total Stress = d,1 . h1 + t,1 . h2 + t,2 . h3 = 13.1 . 2 + 18 . 2.5 + 19.8 . 4.5 = 160.3 kN/m2

Pore Water Pressure u = w . (h2+h3) u = 10 . 7 = 70 kN/m2

Effective Stress ’ = - u = 90.3 kN/m2

’ = d,1 . h1 + (t,2 - w) . h2 + (t,2 - w) . h3

’ = 13.1 . 2 + (18-10) . 2.5 + (19,8-10) . 4.5

= 90.3 kN/m2

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EXAMPLE

-2.0

-4.5

-9.0

26.2 kPa

71.2 kPa

160.3 kPa

25 kPa

70 kPa

26.2 kPa

46.2 kPa

90.3 kPa

Total Stress () Pore Water Pressure (u) Effective Stress (’)

Profile of Vertical Stress / Stress distribution Diagram

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EXAMPLE 3

1 m

0.5 m

2 m

d= 18 kN/m3

Dry sand

For the soil profile shown here, plot the stress distribution diagram including total stress, pore pressure and effective stress

d= 19 kN/m3

Silty sand

sat= 22 kN/m3

Clay

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EXAMPLE 3 (answer)

-1.0

-1.5

-3.5

18 kPa

27.5 kPa

71.5 kPa

0 kPa

19.62 kPa

18 kPa

27.5 kPa

51.88 kPa

Total Stress () Pore Water Pressure (u) Effective Stress (’)

Profile of Vertical Stress / Stress distribution Diagram