Measuring soil strength Flashcards

1
Q

How do soils generally fail?

A

shear when the shear
forces acting on the soil reach the shear strength

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2
Q

What does soil shear strength =?

A

Soil shear resistance

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3
Q

What is the strength of a material?

A

The greatest stress (shear stress) it can maintain

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4
Q

What is soil shear strength derived from?

A

Cohension and friction

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5
Q

What are the characteristics of soil cohesion?

A

Stress independent
Cementation between sand grains
Electrostatic attraction between clay particles

Stickiness

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6
Q

How is factor of safety calculated?

A

Shear resistance / shear force

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7
Q

How does factor of safety calculation define slope stability?

A

If less then or close to one slope is unstable

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8
Q

Is resistance stress dependant?

A

Yes

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9
Q

What is the equation for stress?

A

Stress (sigma) = force (N)/ area (m2)

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10
Q

What are 2 methods for emasuring direct shear?

A

Shear box - force on top in box with known area allows stress to be known when a load cell moves at a set rate (but need to reverse to continue - know remolded strength)

Ring shear - small sample rotated round - find resdiual strength - stress is the rate of turn

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11
Q

What will happen to normally consolidate material during shear?

A

WHen they moe the soil compacts

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12
Q

WHat happens to heavily compacted soil during shear?

A

Rise up and dilate - as particles move apart

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13
Q

What happens to loosely compacted soils during shear?

A

Densification

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14
Q

WHat will happen to stress when a soil dilates?

A

Will be a high peak before “collapse” to residual

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15
Q

What is the strength of densely packed sands?

A

stronger (then loosely) but weaken due to dilatancy as they shear

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16
Q

What is the strength of loosely compacted sands?

A

weaker (than dense), but strain leads to increased
density (tighter packing)

17
Q

What will happen to the strength of sands as strain increases?

A

Strength converges to a critical value

18
Q

Why might multiple tests be done for failure criteria?

A

Get peak stress and allow a stress envelope to be developed which can be comapred to mohr circle to see if failure will occur

19
Q

What is the angle of internal friction for sand?

A

34* depending on grain size (relatively steep angle)

20
Q

What is the angle of internal friction like for clays? (Smectite)

A

5* as particles finer and flatter

21
Q

What happens to mohr circles as loading increases?

A

Mohr circle increases in diameter until failure occurs and the failure envelope is met

22
Q

Will soil above the water table be drained or undrained?

A

Drained as water can flow

23
Q

Will soil be drained or undrained when below the water table?

A

Undrained as nowhere to flow

24
Q

What is effective stress?

A

The stress that controls changes in the volume and strength of a soil

Terzaghi (1925-36)

25
Q

How do you calculate effective stress?

A

sigma - pore pressure

26
Q

What happens to the mohr circle and failure envelope as water pressure increases in soil?

A

Effective stress lowered and failure more likely as less frictinal strength is mobilised

27
Q

What is drained soil?

A

pore fluid is free to move in or out of the soil without affecting the soil properties. High permeability (e.g. sandy) soils and/or slow loading (give
the water time to move

28
Q

What is undrained soil?

A

no movement of pore fluid within the soil, interaction between solid particles and pore fluid. Low permeability soils and/or rapid loading

29
Q

What are the parameters of drained triaxial experiment?

A

Drainage allowed during cell pressure application
Increase deviatoric stress keeps cell pressure constant, sample fluid pressure constant
Water can drain so test ran slower to prevent the development of pore presssure

30
Q

What sediment does drained soil strength apply to?

A

Sediments which can contain pore fluid but that pore fluid can move and change volume
Volume can change during strain: grains incompressible but pore fluid can escape

31
Q

When will drainage occur in the undrained triaxial water experiment?

A

Drainge in consolidation

32
Q

When will drainge occur in the draine dtriaxial water experiment?

A

Drainage in consolidation and shear

33
Q

What will happen because water cant drain in the undrained triaxial experiment?

A

Pore water pressure increases and can be measured

34
Q

When does sediment liquefy?

A

when grains no longer in contact and strength drops to zero

35
Q
A
36
Q

What happens in undrained densely and loosley compacted soils?

A

Dense - prevention of dilation (drop pore pressure and increase strength)
Loose - Contraction prevented (increse pore pressure and loss of strength)

37
Q

What will ultimately lead to liquefaction?

A

as no volume chnage during shearing of loose sands

38
Q

What are the stress paths of drained, undrained and liquefied?

A

Drained - No pore water pressure (diagonal line)
Undrained - Development of pore water pressure (efefctive stress decrease to envelope)
Liquefaction - increase to failure enevelope and decrease to 0 for normal and shear stress