2.4. Plasticity and structure of soil (Indices of Soil Consistency - Plasticity Index) Flashcards

1
Q

provides a measure of a soil plasticity: the amount of water that must be added to change a soil from its plastic limit to its liquid limit.

A

PI = LL - PL or Plasticity Index

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2
Q

Water content where soil changes from plastic to liquid.

A

Liquid Limit

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3
Q

Water content where soil changes from plastic to semi-solid.

A

Plastic Limit

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4
Q

More plastic, retains more water.

A

High Plasticity Index

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5
Q

Less plastic, transitions quickly to solid.

A

Low Plasticity Index

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6
Q

Liquid Limit (LL): 35–100
Plastic Limit (PL): 20–40
Activity (A): 0.3–0.5
Low plasticity and low swelling potential.

A

Kaolinite

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7
Q

Liquid Limit (LL): 60–120
Plastic Limit (PL): 35–60
Activity (A): 0.5–1.2
Moderate plasticity and moderate swelling.

A

Illite

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8
Q

Liquid Limit (LL): 100–900
Plastic Limit (PL): 50–100
Activity (A): 1.5–7.0
Highly plastic and expansive clay.

A

Montmorillonite

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8
Q

Liquid Limit (LL): 50–70
Plastic Limit (PL): 40–60
Activity (A): 0.1–0.2
Low plasticity and very low swelling.

A

Hydrated Halloysite

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8
Q

Liquid Limit (LL): 40–55
Plastic Limit (PL): 30–45
Activity (A): 0.4–0.6
Low plasticity and low swelling potential.

A

Dehydrated Halloysite

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9
Q

Liquid Limit (LL): 150–250
Plastic Limit (PL): 100–125
Activity (A): 0.4–1.3
Moderate to high plasticity.

A

Attapulgite

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10
Q

Liquid Limit (LL): 200–250
Plastic Limit (PL): 120–150
Activity (A): 0.4–1.3

A

Allophane

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11
Q

Nonplastic soil
No plasticity, behaves like granular soil (e.g., sand, silt).

A

PI = 0

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12
Q

Slightly plastic
Very low cohesion, minor deformation before breaking.

A

PI = 1–5

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13
Q

Low plasticity
Some plasticity, minimal swelling/shrinking behavior.

A

PI = 5–10

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13
Q

Medium plasticity
Moderate cohesion, workable and moldable soil.

A

PI = 10–20

14
Q

High plasticity
Highly cohesive, significant expansion/shrinkage.

A

PI = 20–40

15
Q

Very high plasticity
Extremely cohesive, large volume changes with moisture.