MODULE 1 Flashcards

1
Q

Saturated soils

A

voids are filled completely with water

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2
Q

Dry soil

A

voids are filled completely with air

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3
Q

Fines

A

Clay and Silt

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4
Q

Sand

A

0.06 - 2 mm

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5
Q

Gravel

A

2 - 60 mm

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6
Q

Cobbles

A

60 - 200 mm

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7
Q

Boulders

A

> 200mm

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8
Q

Coefficient of Angularity

A

Fu = 4πA/l^2
where A = cross-sectional area
and l = perimeter

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9
Q

Roundness Coefficient

A

R = r/x

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10
Q

Plastic Limit

A

wPL: water content below which fine soil behaves brittle and crumbly

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11
Q

To determine wPL

A
  • roll out threads of clay (3mm diameter)

- wPL is defined as the moisture content w when threads become brittle

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12
Q

Liquid Limit

A

wLL: water content above which fine soil behaves as a liquid

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13
Q

To determine wLL

A

BS: standard fall-cone tests
- usually carry out several tests at different w and draw a straight line between w and fall distance

US: use a Casagrande apparatus, cut V-shape in soil - count number of standard taps to cause the cut to disappear
- test requires more “judgement” than the fall - cone

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14
Q

Clays

A
  • have a plate-like structure

- the higher the wLL, wPL and PL, the more plastic the clay (i.e. the more it will shrink, swell and change volume)

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15
Q

Non-plastic silts

A
  • are like extremely fine sand

-

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16
Q

Soil Classification

A

35% fines = “fine”

17
Q

Static Compaction

A
  • sheepsfoot roller: shallow compaction
  • smooth-wheel roller: shallow compaction
  • pneumatic (multi-tired) roller: shallow compaction
18
Q

Dynamic Compaction

A
  • vibratory roller: shallow compaction
  • High Energy Impact Compaction (HEIC): deep compaction
  • Impact Load (weight dropping): very deep compaction
19
Q

Vibro-compaction

A

very deep compaction

20
Q

Proctor Compaction Tests

A

laboratory method of experimentally determining the optimal moisture content at which a given soil type will become most dense and achieve its maximum dry density

21
Q

Standard Proctor Test Method

A
  • cylindrical 1-litre mould (H=12.7cm and D=10cm)
  • standard hammer (M = 2.5kg; dropping height 300cm)
  • build 3 equal-volume layers and apply 27 blows per layer: compaction energy = 600kJ/m^3
22
Q

Modified Proctor Test Method

A
  • cylindrical 1-litre mould (H=12.7cm and D = 10cm)
  • standard hammer (M = 2.5kg; dropping height 450cm)
  • build 5 equal-volume layers and apply 25 blows per layer: compaction energy = 2700 kJ/m^3
23
Q

Compaction

A

densification of soil by expulsion of air and the rearrangement of particles

24
Q

Benefits of compaction

A
  • increases strength
  • reduces permeability
  • decreases compressibility (settlement)
25
Q

Effects of compactive effort

A
  • increase the dry unit weight (density)

- decrease the optimum water content

26
Q

Effects of gradation

A

(uniformity coefficient): poorly graded and gap graded granular soils are easy to compact

27
Q

effective stress, unsaturated soils

A

σ’ = (σ - Ua) + X(Ua - Uw)
where X depends on the degree of saturation
Ua = pore air pressure
Uw = pore water pressure

28
Q

C(u)

A

Coefficient of Uniformity

  • C(u) less than or equal to 10 “uniformly graded”
  • C(u) greater than 10 “well graded
29
Q

C(z)

A

Coefficient of Curvature

  • C(z) between1 and 3 = “well graded”
  • C(z) less than 1 or greater than 3 = “gap graded”
30
Q

Clay size

A

less than 0.002 mm

31
Q

Silt size

A

0.002 to 0.06 mm

32
Q

amount of fines for “coarse” soil

A

less than 35%

33
Q

amount of fines for “fine” soil

A

more than 35%

34
Q

very dense

A

D(r) more than 85%

35
Q

dense

A

D(r) 65 - 85%

36
Q

med. dense

A

D(r) 35-65%

37
Q

loose

A

D(r) 15 - 35%

38
Q

very loose

A

D(r) less than 15%

39
Q

Dense soils have superior engineering properties

A
  • higher stiffness (less deformability

- higher strength (improved stability)