Utilisateur:Koles trifonov/Brouillon

Coda Wave Interferometry is a ultrasound technique for detection of weak and local changes in complex inhomogeneous media. Sound waves that travel through a medium are scattered multiple times by heterogeneities in the medium, or boundaries in a sample of limited size, and generate slowly decaying waves, called coda waves.

Despite their noisy and chaotic appearance, coda waves are highly repeatable such that if no change occurs in the medium over time, the waveforms are identical. If a change occurs, such as a crack in the medium, the change in the multiple scattered waves will result in an observable change in the coda waves.

Snieder's model of Coda Wave

In the arcticle Roel Snieder described the theory of the coda wave interferometry. He assumed that fields is considered as a sum of trajectories:

$u_{i}(t)=\sum _{tr}^{}S_{tr}(t)$

Considering that $\lambda \ll l_{e}$ where $l_{e}$ is the elastic mean free path, Snieder's demonstrated that medium perturbations acted as a propagation time change:

$u_{p}(t)=\sum _{tr}^{}S_{tr}(t-\tau _{tr})$

Normalised correlation coefficient

In order to estimate a level of peerturbations we used the correlation coefficient. We consider a time window centred at time t and of 2T width. The correlation coefficient is given by:

$CC(\delta t)={\frac {\int _{t-T}^{t+T}u_{i}(t')u_{p}(t'+\delta t)dt'}{\sqrt {\int _{t-T}^{t+T}u_{i}^{2}(t')dt'\int _{t-T}^{t+T}u_{p}^{2}(t')dt'}}},CC\epsilon [-1,1]$

where $u_{i}$ is the reference measurement and $u_{p}$ is the pertubed measurement.

Velocity perturbation

The unperturbed travel time is given by

$t_{tr}=\int _{tr}^{}{\frac {1}{\upsilon }}ds,$

where $\upsilon$ is the coda wave velocity.

The pertubed travel time is

$t_{tr}+\tau _{tr}=\int _{tr}^{}{\frac {1}{\upsilon +\delta \upsilon }}ds=\int _{tr}^{}{\frac {1}{\upsilon }}{\frac {1}{1+{\frac {\delta \upsilon }{\upsilon }}}}ds\simeq \int _{tr}^{}{\frac {1}{\upsilon }}(1-{\frac {\delta \upsilon }{\upsilon }})ds=\int _{tr}^{}{\frac {1}{\upsilon }}ds-\int _{tr}^{}{\frac {\delta \upsilon }{\upsilon ^{2}}}ds,$

where $\delta \upsilon \ll \upsilon$ is the velocity perturbation.

Thus $\tau _{tr}=-\int _{tr}^{}{\frac {\delta \upsilon }{\upsilon ^{2}}}ds$ . If the relative velocity perturbation is assumed constant, then

$\tau _{tr}=-({\frac {\delta \upsilon }{\upsilon }}t_{tr})\simeq -{\frac {\delta \upsilon }{\upsilon }}t,$

where t is the center time of the employed time window.

Thus, the travel time perturbation depends on the arrival time of the coda wave, but not of the particular path followed.