Localization of seismic waves with submarine fiber optics using polarization-only measurements
Abstract
Monitoring seismic activity on the ocean floor is a critical yet challenging task, largely due to the difficulties of physical deployment and maintenance of sensors in these remote areas. Optical fiber sensing techniques are well-suited for this task, given the presence of existing transoceanic telecommunication cables. However, current techniques capable of interrogating the entire length of transoceanic fibers are either incompatible with conventional telecommunication lasers or are limited in their ability to identify the position of the seismic wave. In this work, we propose and demonstrate a method to measure and localize seismic waves in transoceanic cables using only conventional polarization optics, by launching pulses of changing polarization. We demonstrate our technique by measuring and localizing seismic waves from a magnitude Mw 6.0 earthquake (Guerrero, Mexico) using a submarine cable connecting Los Angeles, California and Valparaiso, Chile. Our approach introduces a cost-effective and practical solution that can potentially increase the density of geophysical measurements in hard-to-reach regions, improving disaster preparedness and response, with minimal additional demands on existing infrastructure.
Copyright and License
© The Author(s) 2023. This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.
Acknowledgement
Z.Z. acknowledges the support of the NSF CAREER award and the Moore Foundation.
Contributions
L.C. designed the algorithm and processed the data. L.C. prepared the manuscript with support from all authors. S.V. and P.M. set up and conducted the experiments. Z.Z., V.K. and P.M. led and supervised the project. All authors contributed to the experiment design. All authors participated in the data analysis and interpretation.
Data Availability
The data that support the findings of this study are available from the corresponding author upon reasonable request.
Code Availability
The code that supports the findings of this study is available from the corresponding author upon reasonable request.
Conflict of Interest
S.V. and P.M. are employed by Infinera Corporation. V.K. is employed at Valey Kamalov, LLC.
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Additional details
- PMCID
- PMC10955929
- National Science Foundation
- EAR-1848166
- Gordon and Betty Moore Foundation
- 9500
- Caltech groups
- Division of Geological and Planetary Sciences, Seismological Laboratory