Chapter 6 Flashcards

1
Q

is the study of the mechanical properties of solid materials as well as fluids and gases.

A

Rheology

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2
Q

Equations that mathematically describe the relationship between stress and strain or strain rate.

A

constitutive laws

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3
Q

By isotropic we mean a medium that has the same mechanical properties in all directions, so that it reacts identically to stress regardless of its orientation.

A

Isotropic medium

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4
Q

resists a change in shape, but strains as more stress is applied. Ideally, it returns to its original shape once the applied stress (force) is removed.

A

elastic material

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5
Q

a linear relationship between stress (or force) and strain.

A

linear elastic material

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6
Q

is a constitutive equation for elastic materials

A

Hooke’s Law

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7
Q

The curves defined during straining (loading) and unstraining (unloading) may still be identical, in which case the material

A

perfect elastic

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8
Q

materials that do not change volume during deformation.

A

Incompressible materials

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9
Q

which gives the ratio between the extensions normal and parallel to the stress vector.

A

Poisson’s Ratio

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10
Q

are waves of elastic deformation or energy in which particles oscillate in the direction of wave propagation.

A

P-waves

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11
Q

are elastic body waves where particles oscillate perpendicular to the propagation direction.

A

S-waves

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12
Q

is the inverse of the compressibility of a medium, which is a measure of the relative volume change (volumetric strain) of a fluid or solid as a response to a pressure or mean stress change.

A

Bulk Modulus

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13
Q

The ease with which fluids flow is described in terms of their

A

Viscosity

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14
Q

implies dependence of stress on strain rate: higher stress means faster flow or more rapid strain accumulation.

-is therefore said to be irreversible and creates permanent strain

A

Viscous deformation

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15
Q

Viscous deformation can therefore be said to be ____________ strain is not instant but accumulates over time.

A

time-dependent deformation;

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16
Q

is a measure of how fast a rock object changes length or shape.

A

Strain rate

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17
Q

is resistance of layers or objects to flow. The term is qualitative and relative to that of its neighboring layers or matrix.

A

Competency

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18
Q

permanent strain is added to the elastic strain. If permanent strain keeps accumulating under a constant stress condition

A

perfect plastic deformation.

19
Q

is the permanent change in shape or size of a body without fracture, accumulated over time by a sustained stress beyond the elastic limit (yield point) of the material.

A

Plastic Strain

20
Q

is one where the stress cannot rise above the yield stress and strain can continue to accumulate without any change in the stress level.

A

perfectly plastic material

21
Q

Where there is an additional component of elastic deformation, then the material is

A

elastic perfect plastic

22
Q

means that the stress necessary to deform the rock must be increased for strain to accumulate, because the rock becomes stronger and harder to deform.

A

strain hardening

23
Q

During deformation, atomic-scale defects are known as

A

Dislocations

24
Q

If there is no strain hardening and the material keeps deforming without any increase in the applied force or stress

A

Creep

25
Q

is the case when less stress is required to keep the deformation going.

A

strain softening

26
Q

A geologic example is the effect of grain size reduction during plastic deformation

A

mylonitization

27
Q

This is the situation where stress and elastic strain increase until the yield point is reached, beyond which the deformation is plastic. A material that responds in this way is

A

elastic–plastic

28
Q

is one that flows as a perfectly viscous material, but only above a certain yield stress (a characteristic of plastic behavior). Below this yield stress there is no deformation at all.

A

Viscoplastic

29
Q

is where the deformation process is reversible, but both the accumulation and recovery of strain are delayed.

A

Kelvin viscoelastic behavior

30
Q

accumulates strain from the moment a stress is applied, first elastically and thereafter in a gradually more viscous manner.

A

Maxwell viscoelastic

31
Q

is a model that more closely approximates the response of natural rocks to stress.

A

General linear behavior

32
Q

is the plastic deformation of a material that is subjected to a persistent and constant stress when that material is at a high homologous temperature.

A

Creep

33
Q

An increase in temperature lowers the yield stress or weakens the rock.

A

Increasing the strain rate means increasing the flow stress level.

34
Q

tends to weaken rocks, lower the yield stress, and enhance crystal-plastic deformation

A

Presence of Fluid

35
Q

Increasing the _________ allows for larger finite strain to accumulate before failure and thus favors crystal-plastic deformation mechanisms.

A

confining pressure

36
Q

means being similar or uniform, while isotropic means having properties that do not vary with direction.

A

Homogeneous

37
Q

means that the state of strain is identical in any one piece of the area or volume in question

A

Homogeneous strain

38
Q

means that the volume has been shortened or extended by the same amount in every direction. It involves no change in shape, only a change in volume.

A

Isotropic Strain

39
Q

is a state where all three principal stresses are of equal magnitude. If they are not, stress can still be homogeneous if the state of stress is the same in every part of the rock

A

Isotropic Stress

40
Q

is one that accumulates permanent strain (flows) without macroscopically visible fracturing, at least until a certain point where its ultimate strength is exceeded.

A

Ductile material

41
Q

is one that deforms by fracturing when subjected to stress beyond the yield point.

A

Brittle Material

42
Q

are well represented in metamorphic rocks, i.e. rocks that have been deformed in the middle and lower part of the crust.

A

Ductile structures

43
Q

preserves continuity of originally continuous structures and layers and describes a scale-dependent deformation style that can form by a range of deformation mechanisms.

A

Ductile deformation

44
Q

is generally defined as the permanent change in shape or size of a body without fracture, produced by a sustained stress beyond the elastic limit of the material due to dislocation movement.

A

Plastic deformation