Coda Wave Interferometry for Estimating Nonlinear Behavior in Seismic Velocity

@article{Snieder2002CodaWI,
  title={Coda Wave Interferometry for Estimating Nonlinear Behavior in Seismic Velocity},
  author={Roel Snieder and Alexandre Gr{\^e}t and H. Douma and John A. Scales},
  journal={Science},
  year={2002},
  volume={295},
  pages={2253 - 2255}
}
In coda wave interferometry, one records multiply scattered waves at a limited number of receivers to infer changes in the medium over time. With this technique, we have determined the nonlinear dependence of the seismic velocity in granite on temperature and the associated acoustic emissions. This technique can be used in warning mode, to detect the presence of temporal changes in the medium, or in diagnostic mode, where the temporal change in the medium is quantified. 
Time-Lapse Monitoring with Coda Wave Interferometry
The coda of seismic waves consists of that part of the signal after the directly arriving phases. In a finite medium, or in one that is strongly heterogeneous, the coda is dominated by waves which
Coda Wave Interferometry for Accurate Simultaneous Monitoring of Velocity and Acoustic Source Locations in Experimental Rock Physics
In many geoscientific, material science, and engineering applications it is of importance to estimate a representative bulk seismic velocity of materials or to locate the source of recorded seismic
Coda Wave Interferometry for Accurate Velocity 1 Monitoring and Acoustic Source Location in 2 Experimental Rock Physics
14 Estimating the bulk seismic velocity of materials is of great importance in many appli15 cations in geoscience, material science and engineering. It is necessary for the interpre16 tation of
Time‐lapse monitoring of rock properties with coda wave interferometry
[1] The coda of seismic waves consists of that part of the signal after the directly arriving phases. In a finite medium, or in one that is strongly heterogeneous, the coda is dominated by waves
Coda wave interferometric detection of seismic velocity changes associated with the 1999 M = 3.6 event at Mt. Vesuvius
[1] We detect seismic wave velocity changes at Mt. Vesuvius, using doublets and the Coda Wave Interferometry method. The high sensitivity of multiply scattered coda waves to temporal changes in the
The Theory of Coda Wave Interferometry
Coda waves are sensitive to changes in the subsurface because the strong scattering that generates these waves causes them to repeatedly sample a limited region of space. Coda wave interferometry is
Damage detection in concrete using coda wave interferometry
Temporal changes in the lunar soil from correlation of diffuse vibrations.
TLDR
Using seismic waves recorded on the moon, it is shown that not only direct waves can be retrieved, but also late arrivals that have been scattered before reaching the seismometers, which is used to monitor periodic velocity changes in the lunar soil.
Coda wave interferometry and the equilibration of energy in elastic media.
  • R. Snieder
  • Geology
    Physical review. E, Statistical, nonlinear, and soft matter physics
  • 2002
TLDR
A simple model for the equilibration between P and S waves incorporates into the theory of coda wave interferometry the mode conversions that are inherent to multiply scattered elastic waves.
Time-lapse travel time change of multiply scattered acoustic waves
Existing techniques in correlation spectroscopy, such as coda wave interferometry and diffusing acoustic wave spectroscopy, determine the average motion of scatterers or change in the propagation
...
1
2
3
4
5
...

References

SHOWING 1-10 OF 44 REFERENCES
Development of the active doublet method for measuring small velocity and attenuation changes in solids
The measurement of small changes in elastic wave velocity and attenuation is important to a broad range of problems, such as earthquake prediction and early detection of rock failure in mines.
Source array analysis of coda waves near the 1989 Loma Prieta, California, mainshock: Implications for the mechanism of coseismic velocity changes
Coda waves are often considered to be generated by backscattering of primary waves from randomly distributed heterogeneities in the crust; however, modeling and experimental work indicates that much
Evidence for temporal variation of seismic velocity within the upper continental crust
Observations of systematic temporal variations of seismic anisotropy are presented for an induced-seismicity experiment at 9 km depth. These observations were made under particularly well-controlled
Stability of coda wave attenuation during the Loma Prieta, California, earthquake sequence
The Loma Prieta, California, earthquake occurred in a densely instrumented region with a history of microearthquake recording beginning more than a decade before the October 1989 mainshock. This
TEMPORAL VARIATION IN THE ATTENUATION OF EARTHQUAKE CODA NEAR STONE CANYON, CALIFORNIA
We present evidence of a temporal trend in the attenuation properties of the high frequency coda of local earthquakes near Stone Canyon, central California. The trend appears as a systematic increase
Monitoring a temporal change of seismic velocity in a volcano: Application to the 1992 eruption of M
Multiplets, i.e. events with similar waveforms, are selected from shallow earthquakes recorded on Merapi volcano (Indonesia) before the eruption of February 2nd, 1992. Two multiplet families are
Monitoring velocity variations in the crust using earthquake doublets: An application to the Calaveras Fault, California
We present a technique that greatly improves the precision in measuring temporal variations of crustal velocities using an earthquake doublet, or pair of microearthquakes that have nearly identical
A temporal change in coda wave attenuation observed during an eruption of Mount St. Helens
During the past few years there have been numerous reports of changes in coda wave attenuation occurring before major earthquakes. These observations are important because they may provide insight
Variation of Elastic Wave Velocities in Granites with Pressure and Temperature
The dilatational and rotational wave velocities have been measured as functions of pressure and temperature for five granites. The pressure range was 200-5,000 bars or higher. Dilatational velocities
Changes in source and site effects compared to codaQ−1 temporal variations using microearthquakes doublets in California
We analyse spectral ratio of the coda of doublets of microearthquakes. Our purpose is to find evidence for temporal changes of the attenuation in the crust before a large magnitude earthquake. A
...
1
2
3
4
5
...