The last decade has seen the increased use of DAS (distributed acoustic sensor) and rotational sensor waveforms. To facilitate the interpretation of these data, modifications are made to the wavenumber integration and modal superposition codes of Computer Programs in Seismology (Herrmann, 2013) to compute stress, strain and rotation in a cylindrical coordinate system for 1-D velocity-density models. In addition an auxiliary program is provided to rotate these to a local Cartesian system at the observation point. The complete synthetics permit an evaluation of some deductions about the joint use of rotational and translational instrumentation (6C) to estimate Rayleigh- and Love-wave phase velocities. For a plane waves propagating in the x1 direction one can show that cR = (duz/dt) /ω13 for an observation at the free surface and cL = ½ (duL/dt)/ ω12 . However although cR = (duz/dt) /ωrz , cL ≠ ½ (duL/dt)/ ωrφ because the ωrφ contains near both Love and Rayleigh near field terms. Love wave phase velocities can be estimated only when there is no overlapping Rayleigh wave and when wavelengths are small compared to epicentral distance.
Herrmann, R. B. (2013) Computer programs in seismology: An evolving tool for instruction and research, Seism. Res. Lettr. 84, 1081-1088, doi:10.1785/0220110096
Session: Understanding Earth Systems with Fiber-optic Cables [Poster]
Type: Poster
Date: 4/19/2023
Presentation Time: 08:00 AM (local time)
Presenting Author: Robert B. .. Herrmann
Student Presenter: No
Invited Presentation:
Authors
Robert Herrmann
Presenting Author
Corresponding Author
robert.b.herrmann@gmail.com
Saint Louis University
Synthetics for Stress, Strain and Rotation
Category
Understanding Earth Systems with Fiber-optic Cables