Abstract
Previous studies examining the relationship between the groundwater table and seismic velocities have been guided by empirical relationships only. Here, we develop a physics-based model relating fluctuations in groundwater table and pore pressure with seismic velocity variations through changes in effective stress. This model justifies the use of seismic velocity variations for monitoring of the pore pressure. Using a subset of the Groningen seismic network, near-surface velocity changes are estimated over a four-year period, using passive image interferometry. The same velocity changes are predicted by applying the newly derived theory to pressure-head recordings. It is demonstrated that the theory provides a close match of the observed seismic velocity changes.
Original language | English |
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Article number | 2684 |
Pages (from-to) | 1-20 |
Number of pages | 20 |
Journal | Remote Sensing |
Volume | 13 |
Issue number | 14 |
DOIs | |
Publication status | Published - 2 Jul 2021 |
Bibliographical note
Funding Information:Funding: This work is part of research programme DeepNL, financed by the Dutch Research Council (NWO) under project number DeepNL.2018.033.
Publisher Copyright:
© 2021 by the authors. Licensee MDPI, Basel, Switzerland.
Keywords
- Ambient noise
- Coda-based monitoring
- Groningen
- Passive image interferometry
- Pore pressure monitoring
- Seismic interferometry