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Basic Definitions and Terminology
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Page 1: Soil mechanics a[1].ppt

Basic Definitions and Terminology

Page 2: Soil mechanics a[1].ppt

• Soil is generally a three phase material• Contains solid particles and voids• Voids can contain liquid and gas phases

Solid

Water

Air Vs

Vw

Va

Page 3: Soil mechanics a[1].ppt

• Soil is generally a three phase material• Contains solid particles and voids• Voids can contain liquid and gas phases

Solid

Water

Air Vs

Vw

Va

Page 4: Soil mechanics a[1].ppt

• Soil is generally a three phase material• Contains solid particles and voids• Voids can contain liquid and gas phases

Solid

Water

Air

Phase Volume Mass Weight

Air Va 0 0

Water Vw Mw Ww

Solid Vs Ms Ws

Vs

Vw

Va

Page 5: Soil mechanics a[1].ppt

Units

• Length metres• Mass tonnes (1 tonne = 103 kg)• Density t/m3

• Weight kilonewtons (kN)• Stress kilopascals (kPa) 1 kPa= 1 kN/m2

• Unit weight kN/m3

• Accuracy Density of water, w = 1 t/m3

Stress/Strength to 0.1 kPa

Page 6: Soil mechanics a[1].ppt

Weight and Unit weight

• Force due to mass (weight) more important than mass• W = M g

• Unit weight

Page 7: Soil mechanics a[1].ppt

Weight and Unit weight

• Force due to mass (weight) more important than mass• W = M g

• Unit weight

= g

Page 8: Soil mechanics a[1].ppt

Weight and Unit weight

• Force due to mass (weight) more important than mass• W = M g

• Unit weight

= g

vz v = g z

v = z

Page 9: Soil mechanics a[1].ppt

Specific Gravity

• Gs 2.65 for most soils

• Gs is useful because it enables the volume of solid particles to be calculated from mass or weight

GD e n s i t y o f M a t e r i a l

D e n s i t y o f W a t e r w

GU n i t W e i g h t o f M a t e r i a l

U n i t W e i g h t o f W a t e r w

This is defined by

Page 10: Soil mechanics a[1].ppt

Specific Gravity

• Gs 2.65 for most soils

• Gs is useful because it enables the volume of solid particles to be calculated from mass or weight

GD e n s i t y o f M a t e r i a l

D e n s i t y o f W a t e r w

GU n i t W e i g h t o f M a t e r i a l

U n i t W e i g h t o f W a t e r w

This is defined by

VM M

G

W W

Gs

s

s

s

s w

s

s

s

s w

Page 11: Soil mechanics a[1].ppt

Voids ratio• It is not the actual volumes that are important but rather the

ratios between the volumes of the different phases. This is described by the voids ratio, e, or porosity, n, and the degree of saturation, S.

Page 12: Soil mechanics a[1].ppt

Voids ratio• It is not the actual volumes that are important but rather the

ratios between the volumes of the different phases. This is described by the voids ratio, e, or porosity, n, and the degree of saturation, S.

• The voids ratio is defined as

Page 13: Soil mechanics a[1].ppt

Voids ratio• It is not the actual volumes that are important but rather the

ratios between the volumes of the different phases. This is described by the voids ratio, e, or porosity, n, and the degree of saturation, S.

• The voids ratio is defined as

• and the porosity as

Page 14: Soil mechanics a[1].ppt

Voids ratio• It is not the actual volumes that are important but rather the

ratios between the volumes of the different phases. This is described by the voids ratio, e, or porosity, n, and the degree of saturation, S.

• The voids ratio is defined as

• and the porosity as

The relation between these quantities can be simply determined as follows

Vs = V - Vv = (1 - n) V

Page 15: Soil mechanics a[1].ppt

Voids ratio• It is not the actual volumes that are important but rather the

ratios between the volumes of the different phases. This is described by the voids ratio, e, or porosity, n, and the degree of saturation, S.

• The voids ratio is defined as

• and the porosity as

The relation between these quantities can be simply determined as follows

Vs = V - Vv = (1 - n) V

Hence

Page 16: Soil mechanics a[1].ppt

Degree of Saturation• The degree of saturation, S, has an important influence on soil

behaviour• It is defined as

Page 17: Soil mechanics a[1].ppt

Degree of Saturation• The degree of saturation, S, has an important influence on soil

behaviour• It is defined as

• The phase volumes may now be expressed in terms of e, S and Vs

• Vw = e S Vs Va = Vv - Vw = e Vs (1 - S)

Page 18: Soil mechanics a[1].ppt

Degree of Saturation• The degree of saturation, S, has an important influence on soil

behaviour• It is defined as

• The phase volumes may now be expressed in terms of e, S and Vs

• Vw = e S Vs Va = Vv - Vw = e Vs (1 - S)

Assuming Vs = 1 m3, the following table can be produced

Phase Volume Mass Weight

Air e (1 - S) 0 0

Water e S e S w e S w

Solid 1 G s w G s w

Page 19: Soil mechanics a[1].ppt

Unit Weights

• The bulk unit weight

Page 20: Soil mechanics a[1].ppt

Unit Weights

• The bulk unit weight

• The saturated unit weight (S = 1)

Page 21: Soil mechanics a[1].ppt

Unit Weights

• The bulk unit weight

• The saturated unit weight (S = 1)

• The dry unit weight (S = 0)

Page 22: Soil mechanics a[1].ppt

Unit Weights

• The bulk unit weight

• The saturated unit weight (S = 1)

• The dry unit weight (S = 0)

• The submerged unit weight

Page 23: Soil mechanics a[1].ppt

Moisture Content

• The moisture content, m, is defined as

Page 24: Soil mechanics a[1].ppt

Moisture Content

• The moisture content, m, is defined as

In terms of e, S, Gs and w

Ww = wVw = we S Vs

Ws = s Vs = w Gs Vs

Page 25: Soil mechanics a[1].ppt

Moisture Content

• The moisture content, m, is defined as

In terms of e, S, Gs and w

Ww = wVw = we S Vs

Ws = s Vs = w Gs Vs

hence

Page 26: Soil mechanics a[1].ppt

Example 1

Phase Trimmings Mass

(g)

Sample Mass, M

(g)

Sample Weight, Mg

(kN)

Total 55 290 2845 10-6

Solid 45 237.3 2327.9 10-6

Water 10 52.7 517 10-6

• Distribution by mass and weight

Page 27: Soil mechanics a[1].ppt

Example 1

Phase Trimmings Mass

(g)

Sample Mass, M

(g)

Sample Weight, Mg

(kN)

Total 55 290 2845 10-6

Solid 45 237.3 2327.9 10-6

Water 10 52.7 517 10-6

• Distribution by mass and weight

• Distribution by volume (assume Gs = 2.65)

Total Volume V = r2 l

Page 28: Soil mechanics a[1].ppt

Example 1

Phase Trimmings Mass

(g)

Sample Mass, M

(g)

Sample Weight, Mg

(kN)

Total 55 290 2845 10-6

Solid 45 237.3 2327.9 10-6

Water 10 52.7 517 10-6

• Distribution by mass and weight

• Distribution by volume (assume Gs = 2.65)

Total Volume V = r2 l

Water Volume

Page 29: Soil mechanics a[1].ppt

Example 1

Phase Trimmings Mass

(g)

Sample Mass, M

(g)

Sample Weight, Mg

(kN)

Total 55 290 2845 10-6

Solid 45 237.3 2327.9 10-6

Water 10 52.7 517 10-6

• Distribution by mass and weight

• Distribution by volume (assume Gs = 2.65)

Total Volume V = r2 l

Water Volume

Solids Volume

Page 30: Soil mechanics a[1].ppt

Example 1

Phase Trimmings Mass

(g)

Sample Mass, M

(g)

Sample Weight, Mg

(kN)

Total 55 290 2845 10-6

Solid 45 237.3 2327.9 10-6

Water 10 52.7 517 10-6

• Distribution by mass and weight

• Distribution by volume (assume Gs = 2.65)

Total Volume V = r2 l

Water Volume

Solids Volume

Air Volume Va = V - Vs - Vw

Page 31: Soil mechanics a[1].ppt

Moisture content

Page 32: Soil mechanics a[1].ppt

Moisture content

Voids ratio

Page 33: Soil mechanics a[1].ppt

Moisture content

Voids ratio

Degree of Saturation

Page 34: Soil mechanics a[1].ppt

Moisture content

Voids ratio

Degree of Saturation

Bulk unit weight

Page 35: Soil mechanics a[1].ppt

Moisture content

Voids ratio

Degree of Saturation

Bulk unit weight

Dry unit weight

Page 36: Soil mechanics a[1].ppt

Moisture content

Voids ratio

Degree of Saturation

Bulk unit weight

Dry unit weight

Saturated unit weight

Note that dry < bulk < sat

Page 37: Soil mechanics a[1].ppt

Example 2Volume and weight distributions

Phase Volume

(m3)

Dry Weight

(kN)

Saturated Weight

(kN)

Voids 0.7 0 0.7 9.81 = 6.87

Solids 1.0 2.65 9.81 = 26.0 26.0

Page 38: Soil mechanics a[1].ppt

Example 2Volume and weight distributions

Dry unit weight,

Phase Volume

(m3)

Dry Weight

(kN)

Saturated Weight

(kN)

Voids 0.7 0 0.7 9.81 = 6.87

Solids 1.0 2.65 9.81 = 26.0 26.0

Page 39: Soil mechanics a[1].ppt

Example 2Volume and weight distributions

Dry unit weight,

Saturated unit weight

Phase Volume

(m3)

Dry Weight

(kN)

Saturated Weight

(kN)

Voids 0.7 0 0.7 9.81 = 6.87

Solids 1.0 2.65 9.81 = 26.0 26.0

Page 40: Soil mechanics a[1].ppt

Example 2Volume and weight distributions

Dry unit weight,

Saturated unit weight

Moisture content (if saturated)

Phase Volume

(m3)

Dry Weight

(kN)

Saturated Weight

(kN)

Voids 0.7 0 0.7 9.81 = 6.87

Solids 1.0 2.65 9.81 = 26.0 26.0

Page 41: Soil mechanics a[1].ppt