Stress Flashcards

1
Q

Describe the concept of stress

A

Used to describe the physical state of a material body on which forces are applied, considers surface forces

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2
Q

What are the two kinds of forces?

A

Body forces, surface forces

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3
Q

Describe body forces

A

Act at a distance on all the volume elements of a rock, e.g. gravity, EM forces
Magnitude is directly proportional to mass or volume

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4
Q

Describe surface forces

A

Either arise directly from the action of one body on another across the surface between them or indirectly from the action of one body part of a body on another part across an imaginary internal surface
Magnitude is directly proportional to the surface area over which it acts

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5
Q

What governs the response of an object to a force?

A

The intensity of the force

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6
Q

Define traction

A

Force intensity at a point on a surface of specified orientation
Force intensity = force / area over which the force acts, measured in N/m^2 or Pascal

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7
Q

Define state of stress (σ)

A

Force intensity on surfaces of all possible orientations

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8
Q

Define vector

A

The traction acting on a surface within a loaded body, can be obtained by adding components acting normal and parallel to the surface

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9
Q

Describe positive traction

A

Compressive with an anticlockwise sense of shear, this is the Mohr circle convention

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10
Q

How can traction be used to define a strain ellipse?

A

In 2d, the tails of the traction vectors (traction acting on planes of all possible orientations)

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11
Q

What four numbers define state of stress?

A

Two normal stresses (σn=σxx,σyy) and two shear stresses (τ=σxy,σyx)
These can be written as a 2x2 matrix

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12
Q

When are shear stresses positive?

A

If the shear sense on the sides of the square that cut the negative coordinate axes are in a postive direction
This is the tensor convention (can also be used on the cube in 3d)
σxy = σyx

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13
Q

Describe mechanical equilibrium

A

σxy = - σyx

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14
Q

Describe principal stresses (σ1 and σ2)

A

When the normal stresses are parallel to the coordinate axes and shear stresses are zero
σ1 ≥ σ2

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15
Q

Describe the use of the Mohr circle representation of stress

A

To calculate the stresses on a plane of any orientation

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16
Q

Define stress in 3d

A

Stresses acting on any three mutually perpendicular surfaces

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17
Q

What are the three forces applied to a stress ellipsoid?

A

Fx (σxx,σyx,σzx) Fy (σyy,σxy,σzy), Fz (σzz, σxz,σyz)
Can be written as 3x3 matrix

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18
Q

Difference between normal stresses and shear stresses

A

Normal stresses are diagonal terms and shear stresses are off-diagonal terms

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19
Q

Why is stress a tensor quantity?

A

The individual components are defined in a coordinate frame with a particular orientation, is rotated then the values of the components change
The changed values can be calculated from the known original values using a transformation equation

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20
Q

What are the only non-zero terms in the stress matrix when the coordinate frame is aligned so the shear stresses are zero?

A

The three normal stresses, these are the three principal stresses; σ1, σ2, σ3

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21
Q

What are the two matrices that any stress tensor can be split into?

A

Mean stress and deviatoric stress

22
Q

Describe mean stress

A

Causes or arises from dilation (volume change)

23
Q

Describe deviatoric stress

A

Causes or arises form distortion (shape change)

24
Q

Describe mean stress in the lithosphere

A

Usually similar in magnitude to confining pressure (controlled by burial depth and density of the overlying rock column)
Greater than deviatoric stress

25
Q

When does the strain ellipsoid become a sphere?

A

When there is no deviatoric stress
This is isostatic/hydrostatic/lithostatic stress

26
Q

What affects normal stresses by not shear stresses?

A

Pore fluid pressure

27
Q

How does pore fluid pressure effect a Mohr diagram?

A

Shifts the Mohr circle to the left without changing the diameter

28
Q

Give five reasons for the importance of knowing the state of stress in the Earth

A

Construction, borehole stability, controlled fracture of rocks for oil/gas production, predicting hazards, understanding plate tectonics

29
Q

Describe borehole breakouts

A

Zones of failure in the wall of the borehole that give it an irregular elongate shape

30
Q

Describe overcoring

A

A strain reducing method to reduce borehole breakouts

31
Q

Describe hydrofracking

A

A way of establishing the orientation and magnitude of the principal stress
Fluid is pumped into packers in boreholes, an extension fracture forms at a critical pressure, fluid pressure reduces just enough to keep the crack open

32
Q

How are the orientation and relative magnitude of earthquakes estimated?

A

Using earthquaeke first motion studies and fault plane and slip vector orientation measurements (e.g from stylolites, vein systems, conjugate fractures)

33
Q

How can principal stress orientations be estimated?

A

Using orientation of mechanical twins and of deformation lamellae

34
Q

What does an increase in the principal stress magnitude result in?

A

Increased incidence of calcite twinning and dislocation density and decreased subgrain diameter and dynamically recrystallised grain size

35
Q

What are the orientations of principal stresses at the Earth’s surface and why?

A

One vertical (σv) and two horizontal
One is vertical because air and water cannot sustain a shear stress

36
Q

Give the formula for the vertical stress at the Earth’s surface

A

σv = ρrock g z
ρrock=avg density of rock column
g=acceleration due to gravity
z=depth

37
Q

Describe the stress during burial with no lateral strain (uniaxial strain)

A

Horizontal stress is expected to be one third to one half of the vertical stress

38
Q

Describe isostatic readjustment

A

The raising or lowering of the lithosphere based on whether it is getting thicker by sedimentation of thinner by erosion

39
Q

What is the result of isostatic readjustment?

A

Locally horizontal stress is greater on the thinner section of the lithosphere because they are being applied over a smaller area

40
Q

What causes deviations from states of stress?

A

Tectonic processes
Split into three regimes (Andersonian classification) based on which of the principal stresses is verticle

41
Q

Where do plates bend and what does this bending result in?

A

Results is stresses
Occurs at subduction zones, in response to surface loading, and in reponse to movement across latitudes.
Can occur locally adjacent to other structures, e.g. faults, folds, diapiric intrusions

42
Q

Give five microscale example of high stresses can be induced in rocks

A

Changes in temperature and pressure, lattice defects, crystallisation of a melt, metamorphic reactions

43
Q

How are microscale stresses stored in the rock?

A

As residual stresses that may be relieved during uplift and erosion by fracturing

44
Q

What is stress at given depth often approximated as?

A

Strength of the rocks at that depth

45
Q

What factors are considered for strength vs depth plots?

A

Strain-rate, geothermal gradient, lithological stratification

46
Q

What three models are used for the strength at depth of the continental lithosphere?

A

Jelly sandwich, creme brulee, banana split

47
Q

Describe the jelly sandwich model of strength at depth of the continental lithosphere

A

Weak lower crust between strong upper durst and upper mantle
Thought to apply to cooler geothermal gradients and hydrated lower crust

48
Q

Describe the creme brulee model of strength at depth of the continental lithosphere

A

Strong crust and weak mantle
Thought to apple to higher geothermal gradients and dehydrated lower crust

49
Q

Describe the banana split model of strength at depth of the continental lithosphere

A

Applied to long established major fault zones that extend to great depth

50
Q

What determins the cause of a mechanical process?

A

Boundary conditions (the conditions that are externally imposed on a body)

51
Q

Describe what happens when stresses are imposed and maintain on the boundaries

A

Stress is the cause of the deformation and strain is the response to it

52
Q

Describe what happens when boundaries are required to move by prescribed amount or rate

A

Strain is the cause of the process and stresses develop in reponse to it
For example, the uniaxial reference state