06 - Elastic properties Flashcards
Elastic materials deform …
when a force is applied and return to their original shape when the force is removed
Young’s modulus
E = stress / strain
measure of the stiffness of a solid material.
Poisson ratio v
v = - (dL* / L*) / (dL/L)
Hooke’s law
sigma_ik
relationship between stress and strain
sigma_ik = C_iklm * strain_lm
p-wave velocity v_p
v_p = sqrt( (lambda+2mü)/rho )
s-wave velocity v_s
v_s = sqrt( mü/rho )
Correlation of Poisson ratio to Velocityratio
v_p/v_s = sqrt( 2* (1-v)/(1-2*v) )
the larger v the larger p and s-wave difference
Transmission technique
from transmitter ..
receiver..
visualizing ..
what?
..an ultrasonic pulse passes through sample
.. transform elastic wave into electrical signal
.. with an oscilloscope
the signal and travel time
shear modulus of fluids and minerals
fluids: 0 -> no
Minerals: yes
compressional modulus of fluids and minerals
all: yes
order: Gas, oil and water, minerals
(under specific conditions)
p-wave velocity
slower to fast:
oil, water, air
air
oil
water
Differences of s and p-wave velocities in Rocks
greater differences occur in:
Granite Diorite Gabbro Ultramafic rocks Basalt Eclogit
p-wave velocity
slower to fast:
shale, sand&gravel, sandstone, all others
sand&gravel
shale
sandstone
all others
velocity of igneous rocks
increases from felsic to mafic
velocity in methamorphic rocks
anisotropy (gneiss schist)
-> greater velocity parallel to schistosity