Soils II T2 Flashcards

1
Q

Consolidation definition

A

Consolidation: is the densification of soils by expelling water from the voids and allowing the soil particles to become more tightly packed.

Recall:
 Compaction: removal of air
 Consolidation: removal of water

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2
Q

Settlement and compressive deformation result from

A

The major cause of settlement is compressive
deformation of soil below the structure.
Compressive deformation results from a reduction
in void volume.

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3
Q

Causes of settlement

A

Causes of settlement:
 Deformation of soil particles
 Relocation of soil particles
 Expulsion of water or air from the void spaces
 Reduction in void volume
 Rearrangement of soil grains
 Compression of material in the void

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4
Q

Consolidation of dry soil

A

 Voids filled with air
 Air is compressible
 Rearrangement of soil grains occurs rapidly

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5
Q

Consolidation of saturated soils

A

 Voids of saturated soil are filled with water
 Water is incompressible
 Before soil grains can be rearranged, water must be
extruded
 High permeability soils
i.e. coarse grained soils (sand, gravel)
Short time interval
Most settlement occurs by completion of construction

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6
Q

High permeability soils

A

 i.e. coarse grained soils (sand, gravel)
 Short time interval
 Most settlement occurs by completion of construction

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7
Q

Low permeability soils

A

 i.e. fine grained soils (silt, clay)
 Long time interval
 Strain occurs very slowly
 Settlement occurs slowly
 Continues over long period of time
 Long term uncertainty

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8
Q

Settlement phases

A

 3 phases
1. Immediate Settlement
2. Primary Consolidation Settlement
3. Secondary Compression Settlement

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9
Q

Immediate Settlement of Loads
on Clay

A

 Occurs rapidly after load application
 Caused by soil volume distortion
 Completed quickly
 Constitutes small amount of total settlement
 Caused by the elastic deformation of dry soil, of moist
and saturated soils
 No changes in moisture content
 Calculations are based on equations derived from
theory of Elasticity

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10
Q

Primary Consolidation

A

 Occurs due to the extrusion of water from the voids
 Volume change in saturated cohesive soils
 Result of increased loading
 Very slow
 Continues over a long period of time
 Results in primary consolidation settlement

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11
Q

Secondary Consolidation

A

 Primary consolidation has ended
 Soil compression and associated settlement continue at a very slow rate under a constant effective stress
 Result of plastic readjustment of soil grains
 New, changed stresses in soil
 Progressive breaking of clayey particles and interparticle
bonds
 Results in Secondary Consolidation Settlement

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12
Q

Consolidation Test

A

 Test is performed over 24 hour period
 A specific pressure is applied to the top of the
undisturbed soil sample
 Dial readings = deformation
 Recorded at various times
 Prepare graph
 X-axis (abscissa) → log scale, time (min)
 Y-axis (ordinate) → Deformation (mm)
 Pressure is doubled and test re-run

Results:
1. The e-log p curve (void ratio – log pressure)
2. The cv-log p curve (coefficient of consolidation – log
pressure)
3. The initial void ratio e0

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13
Q

CBR

A

The CBR Test measures the shearing resistance of a soil under controlled moisture and density conditions.

The test yields a bearing-ratio number. This number is not a constant for a given soil but applies only for the tested state of the soil.

The CBR number (or, simply CBR) is obtained as the ratio of the unit stress required to produce a certain depth of penetration of the penetration piston into a compacted specimen of soil at some water content and density to the standard unit stress required to obtain the same depth of penetration on a standard sample of crushed stone.

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14
Q

CBR Values

A

CBR = Test Unit Stress / Standard Unit Stress * 100%

  1. The CBR Value
  2. Moisture contents
  3. Dry unit weights
  4. Swell
  5. Curve of penetration
    stress vs penetration
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15
Q

CBR on site

A

CBR values “on site” may not bear any relationship to the CBR values employed in the road design, due to softening from wet weather and trafficking from site vehicles.

“Capping layers” have been introduced to help solve the problem of sub-grades wetting up and losing strength during construction by protecting the subgrade from the worst of the damage caused by site traffic.

If CBR values are taken on site after the sub-grade has been exposed and dry weather has caused the moisture content of the soil to decrease, increasing soil stiffness, the CBR value will be higher than natural moisture content, this is an incorrect value for design purposes and will cause a serious under design of the road pavement.

Natural soil moisture content, after drainage, is the correct moisture content for determining CBR values for highway design purposes because in the course of time natural soil moisture conditions will be re-established.

Good drainage is an essential part of road construction to allow the optimum strength/CBR to be obtained, and maintained. Drainage must be kept operating efficiently during the life of the road to prevent the strength/CBR decreasing through weakening of the foundation by a rising water table.

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16
Q

Fundamentals of consolidation

A

Saturated soil layer subjected to stress increase
Pore water pressure increases

Sandy soils
Highly permeable
Drainage caused by increase in pore water pressure completed immediately
Pore water drainage accompanied by reduction in volume of soil = settlement
Immediate settlement and consolidation occur simultaneously

17
Q

In clay soils consolidation

A

Low hydraulic conductivity
Consolidation settlement is time dependent
Water is incompressible

In a saturated sample the total stress is the sum of the increase in effective stress and the increase in pore water pressure.

18
Q

What happens to the water as a result of pressure

A

Water in the void spaces begins to be squeezed out and drain in both directions into the sand layers

The excess pore water pressure at any depth on the clay layer gradually decreases and the stress carried by the soil solids (effective stress) increases.