Version 1
: Received: 13 May 2024 / Approved: 14 May 2024 / Online: 14 May 2024 (06:50:44 CEST)
How to cite:
Koorambas, E. Horndeski-Like Gravity Perturbation Induced by Large-Magnitude Earthquake. Preprints2024, 2024050914. https://doi.org/10.20944/preprints202405.0914.v1
Koorambas, E. Horndeski-Like Gravity Perturbation Induced by Large-Magnitude Earthquake. Preprints 2024, 2024050914. https://doi.org/10.20944/preprints202405.0914.v1
Koorambas, E. Horndeski-Like Gravity Perturbation Induced by Large-Magnitude Earthquake. Preprints2024, 2024050914. https://doi.org/10.20944/preprints202405.0914.v1
APA Style
Koorambas, E. (2024). Horndeski-Like Gravity Perturbation Induced by Large-Magnitude Earthquake. Preprints. https://doi.org/10.20944/preprints202405.0914.v1
Chicago/Turabian Style
Koorambas, E. 2024 "Horndeski-Like Gravity Perturbation Induced by Large-Magnitude Earthquake" Preprints. https://doi.org/10.20944/preprints202405.0914.v1
Abstract
We hypothesis that large earthquakes generate Horndeski-like Gravitational Wave (GW). We find that such a Horndeski-like GW propagates with the speed of sound. The sound waves generated by an earthquake make a local and temporal change to the Earth’s diagravitational medium; therefore, they modify the GW speed in a standard, Alternative-Theory-of-Gravity (ATG) sense. The quantum of the Horndeski-like GW is a massless scalar quasiparticle and cannot exist outside of the propagation region of the P-field. The Horndeski-like GW may be detectable by future GW detectors with a sensitivity of 10−15 Hz−1/2 in the region of 0.1–1 Hz.
Keywords
Alternative theories of gravity; Gravitational waves; Sound waves; Earthquakes
Subject
Physical Sciences, Theoretical Physics
Copyright:
This is an open access article distributed under the Creative Commons Attribution License which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.