ATTERBERG LIMITS AND SIEVE ANALYSIS Flashcards

1
Q

boundary between the solid and semi-solid state

A

Shrinkage Limit

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2
Q

Boundary between the semi-solid and plastic state

A

Plastic Limit

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3
Q

boundary between the plastic and liquid state

A

Liquid Limit

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4
Q

plastic limit will be determined by rolling a soil paste into ____ diameter threads until it crumbles, and determining the moisture content.

A

3.2mm

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5
Q

“Atterberg Limits” is named after

A

the Swedish scientist Albert Mauritz Atterberg

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6
Q

Originally, six “limits of consistency” of fine-grained soils were defined by Albert Atterberg: the upper limit of viscous flow, the liquid limit, the sticky limit, the cohesion limit, the plastic limit, and the shrinkage limit. In current engineering usage, the term usually refers only to the liquid limit, plastic limit, and in some references, the shrinkage limit.

A

Atterberg Limits

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7
Q

the relative ease with which a soil can be deformed.

A

Consistency

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8
Q

the water content, in percent, of soil at the arbitrarily defined boundary between the semiliquid and plastic states.

A

Liquid Limit

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9
Q

the water content, in percent, of soil at the boundary between the plastic and semi-solid states.

A

Plastic Limit

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10
Q

a soil that has a range of water content over which it exhibits plasticity and which will retain its shape on drying.

A

Plastic Soil

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11
Q

the range of water content over which a soil behaves plastically. Numerically, it is the difference between the liquid and plastic limits.

A

Plasticity Index

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12
Q

Rotate the handle of the liquid limit device so that the cup lifts and drops at the rate of _______ drops per second.

A

1.9 to 2.1

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13
Q

is the difference between the liquid and plastic limits.

A

Plasticity Index

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14
Q

Roll the bass on the glass plate until it forms a thread about __ inches or ___mm in diameter.

A

⅛ inches or 3.2mm

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15
Q

ASTM used for LL and PL

A

(ASTM D 4318 - Standard Test Methods for Liquid Limit, Plastic Limit, and Plasticity Index of Soils)

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16
Q

The moisture content at which a standard cone of apex angle 30° and weight of 0.78 N (80 gf) will penetrate a distance d=20
mm in 5 seconds when allowed to drop from a position of point contact with the soil surface.

A

(BS 1377 - Fall Cone Method)

17
Q

The number of blows required to achieve closure
varies between ________. The results are plotted on semi-logarithmic graph paper.

A

15 and 35

18
Q

This method offers a more accurate method of determining the liquid and plastic limit;

A

Determination of Liquid Limit Using Fall Cone Method (BS 1377)

19
Q

The moisture content, in percent, at which the volume of the soil mass ceases to change. (ASTM D427/ ASTM D4943)

A

Shrinkage Limit

20
Q

What Soil Indices is indicated below?

0 - Non-plastic
1 – 5 Slightly plastic
5 – 10 Low plasticity
10 – 20 Medium plasticity
20 – 40 High plasticity
> 40 Very high plasticity

A

Plasticity Index Description

21
Q

defines the relative consistency of a cohesive soil in the natural state

A

Liquidity Index

22
Q

LI < 0 Semisolid
state

High strength; brittle; sudden
fracture is expected

0 < LI < 1 Plastic
state

Intermediate strength; soil
deformed like a plastic material

LI > 1 Liquid
state

Low strength; soil deforms like
a viscous fluid

A

TRUE

23
Q

the numerical difference between the plastic limit and shrinkage limit of the remolded soil

A

Shrinkage Limit

24
Q
  • a valuable parameter for classifying the predominant minerals in the sediment
A

Activity of Clas; Ac

25
Q
  • the ratio of a given volume change expressed as a percentage of dry volume to the corresponding charge
    in water content above the shrinkage limit expressed as a percentage of the weight of the oven-dried soil
A

Shrinkage Ratio

26
Q

AC = PI/μ

Where μ - percent finer than 0.002 mm

A

Activity of Clay

27
Q

Ac < 0.7 Inactive clay
0.7 < Ac < 1.2 Normal clay
Ac > 1.2 Active clay

A

TRUE

28
Q

an indicator of the relative shear strength. As ___ increases, the firmness, or shear strength of the soil
also increases.

A

Consistency Index

29
Q

the slope of the water content versus log10 of the blows number plot for the Casagrande cup method, is the
measure of the rate at which soil mass loses its shear strength with increased water content.

A

Flow Index

30
Q

is the determination of the size range of particles present in the soil, expressed as a percentage of the total
dry weight.

A

Mechanical Analysis

31
Q

Two methods are generally used to find the particle-size distribution of soil:

A

(1) sieve analysis
(2) hydrometer analysis

32
Q

—for particle sizes larger than 0.075 mm in diameter and

A

Sieve Analysis