132445661 Elasticity and Seismic Waves Pptx
Transcript of 132445661 Elasticity and Seismic Waves Pptx
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Elasticity and Seismic Waves
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Stress and Strain
Stress is defined as force per unit area.
Strain is defined as the amount of deformation anobject experiences compared to its original size andshape.
When a force is applied to a material, it deforms: stress
induces strain The SI unit for stress is the Pascal (symbol Pa), which is
equivalent to one Newton (force) per square meter(unit area), that is N/m2. In Imperial units, stress ismeasured in pound-force per square inch, which is
abbreviated as psi. Strains are dimensionless and are usually expressed as
a decimal fraction or a percentage.
For some materials, displacement is reversible = elastic
materials
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Compression. Stress that acts to shorten an object.
Tension. Stress that acts to lengthen an object.
NormalStress. Stress that acts perpendicular to a surface. Can be
either compressional or tensional. ShearStress that acts parallel to a surface. It can cause one object
to slide over another. It also tends to deform originally rectangular
objects into parallelograms. The most general definition is that
shear acts to change the angles in an object.
HydrostaticStress (usually compressional) that is uniform in all
directions. Stress in the earth is nearly hydrostatic. The term for
uniform stress in the earth is lithostatic.
DirectedStress. Stress that varies with direction. Stress under a
stone slab is directed; there is a force in one direction but nocounteracting forces perpendicular to it.
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LongitudinalorLinearStrain. Strain that changes thelength of a line without changing its direction. Can beeither compressional or tensional.
Compressionstrain. Longitudinal strain that shortens anobject.
Tension. Longitudinal strain that lengthens an object.
ShearStrain that changes the angles of an object. Shearcauses lines to rotate.
HomogeneousStrain. Uniform strain. Straight lines inthe original object remain straight. Parallel lines remainparallel. Circles deform to ellipses. Note that this
definition rules out folding, since an originally straightlayer has to remain straight.
InhomogeneousStrain. How real geology behaves.Deformation varies from place to place. Lines may bend
and do not necessarily remain parallel.
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Stress-strain relation
Strain is proportional to stress = Hookes law
Stress-strain relation: Elastic domain:
Stress-strain relation is linear
Hookes law applies
Beyond elastic domain: Initial shape not recovered when stress is removed
Plastic deformation
Eventually stress > strength of material => failure
Failure can occur within the elastic domain = brittlebehavior
Strain as a function of time under stress: Elastic = no permanent strain
Plastic = permanent strain
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Elastic Modulus
An elastic modulus, or modulus of elasticity, isthe mathematical description of an object orsubstance's tendency to be deformed elastically(i.e., non-permanently) when a force is applied to
it.
where lambda () is the elastic modulus. If stressis measured in Pascal, since strain is adimensionless quantity, then the units of arePascal as well.
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Young's modulus (E) describes tensile elasticity, or the
tendency of an object to deform along an axis when opposing
forces are applied along that axis; it is defined as the ratio oftensile stress to tensile strain. It is often referred to simply as
the elastic modulus.
The shear modulus or modulus of rigidity (G or ) describes
an object's tendency to shear (the deformation of shape at
constant volume) when acted upon by opposing forces; it is
defined as shear stress over shear strain.
The bulk modulus (K) describes volumetric elasticity, or the
tendency of an object to deform in all directions when
uniformly loaded in all directions; it is defined as volumetric
stress over volumetric strain.
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Poissons ratio
When an isotropic elastic object is subject toelongation or compressive stress z a strain z
results in the direction of the stress. At the
same time a strain arises in the transversedirections, x , y. Ifz is an elongation, then
x = y are compressive. The ratio
= x/z = y/z
is called Poissons ratio.