Impact of infrasound atmospheric noise on gravity detectors used for astrophysical and geophysical applications

Donatella Fiorucci, Jan Harms, Matteo Barsuglia, Irene Fiori, and Federico Paoletti
Phys. Rev. D 97, 062003 – Published 30 March 2018

Abstract

Density changes in the atmosphere produce a fluctuating gravity field that affects gravity strainmeters or gravity gradiometers used for the detection of gravitational waves and for geophysical applications. This work addresses the impact of the atmospheric local gravity noise on such detectors, extending previous analyses. In particular we present the effect introduced by the building housing the detectors, and we analyze local gravity-noise suppression by constructing the detector underground. We present also new sound spectra and correlation measurements. The results obtained are important for the design of future gravitational-wave detectors and gravity gradiometers used to detect prompt gravity perturbations from earthquakes.

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  • Received 16 January 2018

DOI:https://doi.org/10.1103/PhysRevD.97.062003

© 2018 American Physical Society

Physics Subject Headings (PhySH)

Gravitation, Cosmology & AstrophysicsInterdisciplinary Physics

Authors & Affiliations

Donatella Fiorucci1, Jan Harms2,3, Matteo Barsuglia1, Irene Fiori4, and Federico Paoletti4,5

  • 1APC, AstroParticule et Cosmologie, Université Paris Diderot, CNRS/IN2P3, CEA/Irfu, Observatoire de Paris, Sorbonne Paris Cité, 10, rue Alice Domon et Léonie Duquet, 75205 Paris Cedex 13, France
  • 2Gran Sasso Science Institute (GSSI), I-67100 L’Aquila, Italy
  • 3INFN, Laboratori Nazionali del Gran Sasso, I-67100 Assergi, Italy
  • 4European Gravitational Observatory (EGO), I-56021 Cascina, Pisa, Italy
  • 5INFN, Sezione di Pisa, I-56127 Pisa, Italy

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Issue

Vol. 97, Iss. 6 — 15 March 2018

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