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.