Title: The integral expression of the acoustic multiple scattering about cracks
1The integral expression of the acoustic multiple
scattering about cracks
Key Laboratory of Petroleum Resources,
Institute of Geology and Geophysics, Chinese
Academy of Sciences
2Outline
- Introduction
- Method
- Numerical examples
- Conclusions
3Outline
- Introduction
- Method
- Numerical examples
- Conclusions
4Introduction
- Biot theory (1956)
- Eshelby (1957) proposed the classical formulas
about the non-uniform media . - HKT theory
- Hudson (1980,1981) proposed the expression on
the velocity anisotropy caused by cracks and
scattering absorption. - Kuster and Toksoz(1979,1981) mainly presented
the equivalent velocity for the cracks with the
Biot viscous fluid in it. - Chen Xiaofei (1993), scattering matrix in
wavenumber domain by means of continuation
according to direction, -
-
5Introduction
- The defect about the HKT theory is that
- there is no analytical solution for the
- ellipsoidal seismic wave, because it lacks an
orthogonal coordinate system to get - the differential equation with coordinate
- separation.
6Introduction
- Characters of the integral expression which we
- proposed
- Via frequency wavenumber domain.
- Include the exponential function, separable
approximation and fractional operators.
- two important characteristics of the cracks
scattering - coupling among the spherical harmonic mode
- the multiple scattering
7Outline
- Introduction
- Method
- Numerical examples
- Conclusions
8Method
- Modified from Chen Xiaofeis method(1993), so
called continuation according to direction - Difference Chen find scattering matrix, We give
transfer matrix - Based on transfer matrix, we inverse its element
by Witt formula in pseudo differential operator
theory
9Transfer matrix expression
n
m
Modified from chen xiaofei (1993)
10Symbol Inversion via element of Transfer matrix
11Method
- In fact, R is an evolutional form of the
Sphere Reflection Coefficient, n-m is the Mode
Coupling Coefficient, and the factor
is depending on the shape of the
crack. If b0, R can be expressed as -
(8)
which is the spherical reflection coefficient.
12Method
- If the incident wave can be read as
(9)
the scattering wave can be read as
(10)
(11)
13Outline
- Introduction
- Method
- Numerical examples
- Conclusions
14the global scattering matrix
(a)
(b)
(d)
(c)
- the global scattering matrix changes with
the value of incident frequency which is 5Hz,
10Hz, 15Hz and 30Hz with respect to sub-picture
(a), (b), (c) and (d).
15the global scattering matrix
(a)
(b)
(c)
(d)
- the global scattering matrix changes with the
value - of the size about the crack which is
10m,20m,40m - and 80m corresponds to sub-picture
(a),(b),(c)and (d).
16incident wave
17Wave-field for single wavenumber
Angle.inpi/6 Ka1.5
18snapshots
t0.16s
t0.32s
t0.4s
19Outline
- Introduction
- Method
- Numerical examples
- Conclusions
20Conclusions
- two important characteristics of the scattering
firstly - spherical harmonic mode coupling which is
different from the sphere scattering. - it gives an expression about the multiple
scattering which is distinct from Eshebys
static field. - Eshebys static field methods ignore the multiple
scattering and the mode coupling, - the equavalent theory based on the method is
that the velocity anomaly becomes smaller while
the absorption anomaly become larger. - New quasi static approximation should be given
21Conclusions(continued)
- Further works
- more comparision of our method to numerical
calculation on single and more cracks - Giving the integral expression of the elastic
wave P-SV or P-SV-SH.
22Thanks for your attention!!
welcome comments and suggestions!!
23acknowledgements
- NSFC key project of National natural science
foundation(40830424) - MOSTNational Hi-Tech Research and Development
Program of China..(863 Program),Grant No
2006AA09A102-08 - MOSTNational Basic Research Program of
China..(973 Program), Grant No2007CB209603
24Method
- Figure 1 is the crack model. The length
of the crack is ab and the thickness of it is
a-b.
Fig1 the crack model
25Method
- The outward wave-field can be written as
(1)
Where is the outward scattering
coefficient, is the first kind n-order
Hankel function, the subscript gt means
outward, is the outward angle between the
normal and the outgoing wave, k is the
wavenumber,
The inward wave-field can be read as
(2)
Where is the inward scattering
coefficient, is the second kind n-order
Hankel function.
26Method
- we build up the transfer matrix chen xiaofei
(1993) give different formular on scattering
matrix
(3)
Where
27Method
- It should be noted that eq. (3) can be
adapted to calculate any convex inclusions. By
the differential operators, we can get
(4)
Where the global scattering matrix can
be read as
(5)
(6)
(7)