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Energy partitioning into the strain tensor components for diffuse elastic waves in three-dimensional homogeneous
1Department of Geophysics, Graduate School of Science, Tohoku University, Aoba-ku, Sendai, 980-8578, Japan.
Distributed Acoustic Sensing (DAS) measures axial strain, but energy partitioning is unknown. This study models seismic wave energy partitioning into strain components, aiding quantitative interpretation of DAS strain seismograms.
Area of Science:
- Geophysics
- Seismology
- Optical Fiber Sensing
Background:
- Distributed Acoustic Sensing (DAS) enables dense axial strain measurements along optical fibers.
- The partitioning of seismic wave energy into measured strain components remains poorly understood.
- Existing research focuses on energy partitioning into displacement components.
Purpose of the Study:
- To formulate energy partitioning into different strain tensor components for diffuse waves.
- To investigate the depth-dependent contributions of body and surface waves to strain components.
- To provide a framework for quantitative interpretation of DAS strain seismograms.
Main Methods:
- Developed a theoretical model for energy partitioning into six independent strain components.
- Analyzed diffuse wave propagation in a 3D homogeneous isotropic half-space.
- Examined the influence of depth on wave contributions to strain components.
Main Results:
- Surface DAS measurements (horizontal strains) are dominated by shear horizontal-waves and Rayleigh waves.
- Borehole DAS measurements (vertical strain) are initially dominated by Rayleigh waves.
- Rayleigh wave contribution to vertical strain decays rapidly with depth, with shear vertical-wave contribution persisting.
Conclusions:
- The study provides a theoretical basis for understanding seismic wave energy partitioning in DAS measurements.
- Findings clarify the wavefield composition of measured strains at different depths and locations.
- This work facilitates quantitative interpretation of DAS strain data, particularly the late coda.
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