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
velocity in sedimentary/porous rocks
brad range
-> low velocity for porous gas bearing members
ratio of the two wave velocities Vp/Vs or the Poisson’s ratio n is controlled mainly by …
rock type
pore fluid
velocity with fracturing
velocity decreases
velocity show pressure dependence
anisotropic?
Correlation of velocity with temperature
decreases with increasing temperature
shear wave velocity and change of pore fluid
insensitive ( gas brine)
effect of clay more relevant!
Five possible sources of seismic anisotropy
(1) aligned crystals,
(2) direct stress-induced anisotropy,
(3) lithological anisotropy (for example aligned grains),
(4) structural anisotropy (for example fine layering), and
(5) stress aligned crack-induced anisotropy.
elastic properties below the critical porosity
rock skeleton dominated
grain contact behavior controls many effects
elastic properties above the critical porosity
fluid dominated
particles are embedded in the fluid as a suspension
Sonic logging
with ..
using ..
measure ..
sound wave
piezoelectric transmitter and receiver
interval transit time,
which is typically a function of lithology and rock texture but particularly porosity
Borehole televiewers
measures ..
how..
amplitude and transit time at one of two frequencies
Short bursts of acoustic energy are emitted by a rotating transducer in pulse-echo mode