Onland and Offshore Extrinsic Fabry–Pérot Optical Seismometer at the End of a Long Fiber
|Author(s)||Bernard Pascal1, Feron Romain2, 3, Plantier Guy2, 3, Nercessian Alexandre1, Couteau Julien1, Sourice Anthony2, 3, Feuilloy Mathieu2, 3, Cattoen Michel4, Seat Han‐cheng4, Chawah Patrick5, Chéry Jean5, Brunet Christophe1, Boudin Frédérick6, Boyer Daniel7, Gaffet Stéphane7, Geli Louis8, Pelleau Pascal8|
|Affiliation(s)||1 : IPGP, Université de Paris, UMR 7154 CNRS, 1 rue Jussieu, 75005 Paris, France
2 : ESEO Group, 10 Boulevard Jean Jeanneteau, 49100 Angers, France
3 : Also at LAUM, Université du Maine, Avenue Olivier Messiaen, 72085 Le Mans, France.
4 : LAAS‐CNRS, 7 Avenue du Colonel Roche, 31400 Toulouse, France
5 : Géosciences Montpellier, Place Eugène Bataillon, 34090 Montpellier, France
6 : Département de Géologie, ENS Paris, 24 Rue Lhomond, 75005 Paris, France
7 : Laboratoire Souterrain à Bas Bruit (LSBB), 84400 Rustrel, France
8 : IFREMER, 1625 Route de Sainte‐Anne, 29280 Plouzané, France
|Source||Seismological Research Letters (0895-0695) (Seismological Society of America (SSA)), 2019-11 , Vol. 90 , N. 6 , P. 2205-2216|
|WOS© Times Cited||7|
We report here the design, performance, and in situ demonstration, on‐land and offshore, of an innovative high‐resolution low‐cost optical (laser) seismometer. The instrument was developed within the Laser Interferometry for Earth Strain project (French Agence Nationale de la Recherche [ANR] program), and first tested at the low‐noise underground laboratory Laboratoire Souterrain à Bas Bruit (LSBB, France). It is based on Fabry–Pérot optical interferometry between the extremity of a probing optical fiber and a reflecting mirror secured to the mobile mass of a passive 2 Hz geophone. The detection technique is based on the wavelength modulation of the laser diode (1310 nm), which allows the separation of the optical power into two signals in quadrature, thanks to an heterodyne technique. The relative displacement of the mobile mass is retrieved in real time by the phase unwrapping of these two signals. At LSBB, the fiber was 3 km long. It recorded many teleseismic earthquakes and a few regional ones, and resolves the low‐seismic noise of the Earth for periods up to 6 s, presenting an acceleration noise floor lower than 1 ng/Hz−−−√ in the 0.3–5 Hz range. A three‐component version of this fiber‐based interferometric 2 Hz geophone has been recently constructed, shielded in a hyperbaric container, and installed offshore for test in Brittany (France) in April 2018, with an improved control system. Its record of the marine ambient noise matches those of a collocated commercial broadband seismometer for periods up to 50 s. This opens promising perspectives for large‐scale ocean bottom instrumentation with up to 50‐kilometer‐long optical lines; an installation is planned for 2020, off Guadeloupe, with a 5‐kilometer‐long fiber cable. It may also prove useful for installations in other challenging and exposed environments, such as deep hot boreholes, active volcanoes, unstable landslides, for real‐time monitoring in regions with high natural hazard, but also for seismic monitoring of geoindustries.