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Long-term study of the seismic environment at LIGO

E J Daw et al 2004 Class. Quantum Grav. 21 2255-2273   doi: 10.1088/0264-9381/21/9/003  Help

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E J Daw1,2, J A Giaime1, D Lormand4, M Lubinski3 and J Zweizig5
1 Department of Physics and Astronomy, Louisiana State University, Nicholson Hall, Tower Drive, Baton Rouge, LA 70803-4001, USA
2 University of Sheffield, Department of Physics and Astronomy, Hicks Building, Hounsfield Road, Sheffield S3 7RH, UK
3 LIGO Hanford Observatory, Route 10, Mile Marker 2, Richland, Washington DC 99352-0159, USA
4 LIGO Livingston Observatory, 19100 Ligo Lane, Livingston, LA, 70754, USA
5 LIGO Laboratory, California Institute of Technology, Pasadena, CA 91125, USA
E-mail: e.daw@shef.ac.uk

Abstract. The LIGO experiment aims to detect and study gravitational waves using ground-based laser interferometry. A critical factor to the performance of the interferometers, and a major consideration in the design of possible future upgrades, is isolation of the interferometer optics from seismic noise. We present the results of a detailed programme of measurements of the seismic environment surrounding the LIGO interferometers. We describe the experimental configuration used to collect the data, which were acquired over a 613 day period. The measurements focused on the frequency range 0.1–10 Hz, in which the secondary microseismic peak and noise due to human activity in the vicinity of the detectors was found to be particularly critical to the interferometer performance. We compare the statistical distribution of the data sets from the two interferometer sites, construct amplitude spectral densities of seismic noise amplitude fluctuations with periods of up to 3 months and analyse the data for any long-term trends in the amplitude of seismic noise in this critical frequency range.

PACS numbers: 91.30.Dk, 95.80.Sf, 95.55.Ym

Print publication: Issue 9 (7 May 2004)
Received 19 December 2003
Published 2 April 2004

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