Soils and Materials Flashcards

1
Q

Moisture content calculation

A

((wet - dry weight)/wet) x 100

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2
Q

Calculating liquid limit

A

The liquid limit is defined as the
water content at which the groove
cut into the soil will close over a
distance of 13 mm following 25
blows.

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3
Q

parameters gained from shear test

A

Cohesion
angle of internal friction

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4
Q

Soil description order

A

Strength
Colour
Structure
Soil type
Additional info

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5
Q

Determination of Liquid Limit tests (atterberg limits)

A

One-point Casagrande method (line in soil closing 13mm after 25 blows)

Cone penetrometer method (moisture content at which a standard cone will
penetrate a distance of 20 mm in 5 seconds)

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6
Q

Atterberg Limits

A

basic measure of the critical water contents of a fine-grained soil

L– for low plasticity soil (liquid limit < 50)
H– for high plasticity soil (liquid limit > 50)

Liquid limit
Plastic limit PI=0.73(LL-20)
Shrinkage limit

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7
Q

What is Cohesion

A

property of like molecules (of the same substance) to stick
to each other due to mutual attraction (e.g. soil particles).

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8
Q

what is Adhesion

A

the property of different molecules or surfaces to cling to each
other (e.g. soil & water).

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9
Q

What is the proctor test and how is it performed

A

used to obtain the maximum dry density of compaction and the optimum moisture content

The soil is mixed with varying amounts of water, then compacted in 3 equal layers in a standard mould using a 2.5kg rammer

Parameters gained:
The maximum dry density and optimum moisture content is
determined from the results of the test.

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10
Q

what is Compaction

A

process of increasing the bulk density of a soil or aggregate by removing the air voids trapped within. The density achieved is very much dependent on the moisture content

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11
Q

Importance of the proctor test

A
  • It gives density that must be achieved in the field.
  • Provides the moisture range that allows for minimum compaction
    effort to achieve density.
  • Provides data on the behaviour of the material in relation to various
    moisture contents.
  • It is not possible the determine if a soil density test passes or fails
    without it.
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12
Q

Determination of coefficient of permeability, (k) tests

A

The constant-head test (For permeable soils (k>10-3 mm/sec)) FOR MEDIUM TO COURSE SOILS

The falling-head test (variable-head), (For less permeable soils (k<10-3
mm/sec)) FOR SAND

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13
Q

Unit weight of water

A

1000 kg/m3

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14
Q

Specific gravity of soil

A

Gs = Density soil / Density of water

typically varies between 2.6 and 2.8

enables the volume of solid particles to be
calculated from mass or weight.

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15
Q

coefficient of permeability calculation

A

From Darcy Law

𝑘 =𝑞/𝐴i

q = flow rate = mm3 of liquid / time in seconds
A = cross sectional area of sample
i = h/L = change in head height mm/length of sample mm

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16
Q

Loads on masonary

A

compressive and shar loads

Parallel flexure and normal flexure

17
Q

Compaction proactor test calcs

A

moisiture content (w)= wet - dry / dry
bulk density (p) = sample mass in grams (m) / volume of mould in m3 (v)
dry density = 100p/100+w

plot on graph to find max dry density and optimum water content

18
Q

Liquid limit calculation

A

Calculate moisure content = Ww/Ws x 100
Ww = mass of wet
Ws = Mass of solid

plot

LL = blows at 25

19
Q

Sieve test Cu (uniformity) coefficient

A

Typical values for Cu:
* Cu >5 indicates a well-graded soil.
* 1< Cu <4 indicates a good soil.
* Cu =1 indicates that all the particles are in the same size.

20
Q

Sieve test Cc (curvature) coefficient

A

Typical values for Cc:
* 0.5< Cc <2 indicates a well-graded soil
* Cc <0.1 indicates a possible gap-graded soil

21
Q

Geological strata on whitecliff bay in chronological order

A

White chalk
Reading beds
London clay
Bagshot sands
Bracklesham sands

22
Q

Hard engineering examples

A

Gabions
Concrete sea wall
rock armour
tetrapods
Gryones

23
Q

Soft engineering examples

A

Creating offshore sand dunes
Dredging
Beach replenishing

24
Q

Shear box test pocess

A

1) Internal box measured
2) loading weight determined
3) Box filled with sample in 10mm layers
4) topper and weight added
5) motor and timer started
6) shear stress values taken every 15 secs for several mins until guage fluctuates
7) failure occurs when guage drops

25
Q

importance of shear box test

A

As normal load is directly proportional to the shear loa, the shear stress can be determined from the results

Angle of internal friction and cohesion are also determined from results collected in the test. These are used in the design process for engineering applications such as foundations and retaining walls.

26
Q

Weaknesses of the shear box test

A

Does not demonstrate the weakest plane
Failure plane may not be the weakest plane
Not a uniform stress
Uncontrollable variables

27
Q

specific gravity of soil grain

A

between 2.6 and 2.8

28
Q

Determination of Liquid Limit
Cone penetrometer method

A

hollow stem filled with lead shot. 80g mass of assembly height, 30 degree cone, 5mm high

29
Q

Determination of Liquid Limit
One-point Casagrande method

A