Consistency Of Soil Flashcards

(50 cards)

1
Q

Rupture resistance is best described using

A

Stickiness and Plasticity

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2
Q

Describe the strength with which soil materials are held together

A

Consistency of soil

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3
Q

The ability of soil materials to change shape(but not volume), continuous under the influence of a constant pressure and to retain the impressed shape when the pressure is removed

A

Plasticity

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4
Q

Soil begins to stick to fingers but comes off one or the other cleanly; does not stretch when the fingers are opened

A

Slighty sticky

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5
Q

The ability of soil materials to adhere to other objects

A

Stickiness

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6
Q

Field test for stickiness

A

Non sticky
Slightly sticky
Sticky
Very sticky

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7
Q

The field measure of the ability of the soil to withstand pressure as applied using the thumb and forefinger

A

Rupture resistance

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8
Q

Separates inorganic clays from inorganic slits

A

A-line

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9
Q

When describing rupture resistance, we attempt to describe it using

A

Moist, Dry, and wet consistency

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10
Q

The resistance of soils to deformation and rupture

A

Consistency of soil

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12
Q

Water is added to soil to increase water content

A

Wet consistency

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12
Q

Soil sticks to both thumb and forefinger and tends to stretch a little and pull apart rather than pulling free from your finger

A

Sticky

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13
Q

Shrinkage limit, Plastic limit, and Liquid Limit are also known as

A

Atterberg limits

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15
Q

Atterberg limits were oberved by

A

Albert Mauritz Atterberg

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16
Q

Consistency can be described as

A

Dry, moist, and wet consistency

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17
Q

Atterberg limits were refined by

A

Arthur Casagrande

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18
Q

Soil sticks firmly to both thumb and forefinger and stretches when the fingers are opened

A

Very Sticky

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19
Q

Liquid Index ( LI)

A

LI = (w- PL) / ( LL-PL)

= (w-PL) / PI

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20
Q

The degree to which a reworked soil can be permanently deformed without rupturing

A

Plasticity of solids

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22
Q

Can undergo deformation without cracking

A

Plastic soil

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23
Q

No soil or practically no soil sticks to fingers

23
Q

Describes as the response of soil to physical change through (increasing) moisture content

24
Q

Are basically the limits of water content used to define soil behavoir

A

Atterberg limits

25
Q

Moisture content at which soil begins to behave as liquid material and begins to flow

26
Moisture content at which soil begins to behave as plastic material
Plastic limit
27
Moisture content at which no futher volume change occurs further reduction in moisture content
Shrinkage limit
28
What lab apparatus is used to test liquid limit
Casagrande cup
29
After how many blows to reach the liquid limit
25
30
Specific Gravity
Gs = 1 / [( 1/SR) - (SL/100)]
31
The slope of the flow rate
Flow index
32
Flow index is equal to
FI = (w1 - w2) / log (N2/N1)
33
Another method to obtain the liquid limit
Fall cone test method
34
Is the moisture content at which the soil, when rolled into threads of 3.2mm (1/8 inch),crumbles
Plastic limit
35
PI =
PI = LL - PL
36
Indicates how much volume change is possible as changes above water content above the shrinkage limit occur
Shrinkage ratio
37
Is the moisture content of which the volume change of the soil mass ceases( or the volume no longer goes smaller)
Shrinkage limit
39
Is the upper limit of the relationship of the PI to the LL for any soil found so far
U-line
40
Is an index for identifying the swelling potential of clay soils
``` A = PI / u u = percent finer ```
41
Formula for change in moisture content
Change in moisture = density ( V1- V2) / m2
41
Shrinkage limit formula
SL = [(m1 -m2) / m2] -[(V1-V2)/ m2 ] density
42
Is themeasure of plasticity of the soil
Plasticity index
43
Provides the relative consistency of a cohesive soil with respect to the atterberg limits
Liquid Index ( LI )
43
Shrinkage ratio ( SR)
SR = density of dry / density of water
44
Commonly used to indicate the in situ denseness and loosenessof soil
Relative Density (Sr)
45
Relative Density is equal to
Dr = (emax -e) / (emax - emin)
46
Very loose, Dr is equal to
0-15
47
Loose, Dr is equal to
15-50
48
Medium, Dr is equal to
50-70
49
Dense, Dr is equal to
70-85
50
Very Dense, Dr is equal to
85-100