Week 8 Soil Strength 1 Flashcards

1
Q

Why is soil strength difficult to predict and understand compared to materials like concrete or steel?

A

Soil strength is not a constant property and varies depending on various factors such as soil type, formation, grading, previous stresses, and confinement.

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2
Q

What factors influence the strength properties of soil?

A

Soil type, formation, particle size (grading), previous applied stresses, confinement, stress conditions, and drainage conditions.

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3
Q

What are the three factors contributing to soil shear strength?

A

1) Cohesion (c) of the soil. 2) Friction (Φ) between soil particles. 3) Normal stress (σn) acting across the shear surface.

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4
Q

What is meant by the ‘angle of friction’ or ‘angle of shearing resistance’?

A

It refers to the friction (Φ) between soil particles.

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5
Q

What are ‘Shear Strength Parameters’?

A

The cohesion (c) and friction (Φ) values of a soil, which can be determined through tests.

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6
Q

Why is normal stress (σn) not fixed in a given drainage condition?

A

It depends on the stress within the soil due to unit weight, depth, and external loads.

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7
Q

What happens when soil is subjected to increased stress?

A

It undergoes strain or displacement of particles, resulting in mobilized shear resistance.

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8
Q

What is ‘yield stress’ in soil?

A

The stress level causing strains so large that it may form a ‘serviceability’ limit state, not necessarily the maximum shear strength.

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9
Q

What is ‘peak stress’ in soil?

A

The maximum shear stress the soil can withstand, typically used to determine shear strength parameters.

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10
Q

What is ‘ultimate stress’ in soil?

A

A constant value of stress achieved during very large strains, common in loose sands or soft clays that undergo work hardening.

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11
Q

What is ‘residual strength’ in soil?

A

The lower shear strength value achieved after a peak stress, especially in soils that have previously failed and undergone large displacements.

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12
Q

Why is residual strength important in geotechnical engineering?

A

It determines the required applied shear stress to re-activate old failure surfaces, such as those within landslides.

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13
Q

What is the Mohr-Coulomb equation for shear strength?

A

τ = c + σn tan Φ, where: τ = Shear strength, c = Cohesion, σn = Normal stress, Φ = Angle of friction.

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14
Q

What is the effective stress version of the Mohr-Coulomb equation?

A

τ = c’ + σ’n tan Φ’, where: c’ = Effective cohesion, σ’n = Effective normal stress, Φ’ = Effective angle of friction.

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15
Q

Why is soil strength often determined in effective stress terms?

A

Because shear movement is resisted by the soil skeleton, not the pore water, so effective stress reflects the actual stress passing through the soil particles.

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16
Q

How is effective stress calculated during soil strength tests?

A

By subtracting pore water pressure from the total stress.