[en] We present analyses of the noise wave field in the vicinity of Virgo, the Italian–French gravitational wave observatory located close to Pisa, Italy, with special reference to the vibrations induced by a nearby wind farm. The spectral contribution of the wind turbines is investigated using (1) onsite measurements, (2) correlation of spectral amplitudes with wind speed, (3) directional properties determined via multichannel measurements, and (4) attenuation of signal amplitude with distance. Among the different spectral peaks thus discriminated, the one at frequency 1.7 Hz is associated with the greatest power, and under particular conditions it can be observed at distances as large as 11 km from the wind farm. The spatial decay of amplitudes exhibits a complicated pattern, which we interpret in terms of the combination of direct surface waves and body waves refracted at a deep (≈800 m) interface between the Plio-Pleistocenic marine, fluvial, and lacustrine sediments and the Miocene carbonate basement. We develop a model for wave attenuation that allows determining the amplitude of the radiation from individual turbines, which is estimated on the order of 300-400 micro ms^-1/sqrt(Hz) for wind speeds over the 8–14 m/s range. On the basis of this model, we then develop a predictive relationship for assessing the possible impact of future wind farm projects.
Disciplines :
Earth sciences & physical geography
Author, co-author :
Saccorotti, Gilberto; Istituto Nazionale di Geofisica e Vulcanologia > Pisa
Piccinini, Davide; Istituto Nazionale di Geoficia e Vulcanologia > Pisa
Cauchie, Léna ; Université de Liège - ULiège > Département de géologie > Géologie de l'environnement
Fiori, Irene; European Gravitational Observatory-VIRGO
Language :
English
Title :
Seismic Noise by Wind Farms: A Case Study from the Virgo Gravitational Wave Observatory, Italy
Publication date :
April 2011
Journal title :
Bulletin of the Seismological Society of America
ISSN :
0037-1106
eISSN :
1943-3573
Publisher :
Seismological Society of America, United States - California
Acernese, F., F. Antonucci, S. Aoudia, K. G. Arun, P. Astone, G. Ballardin, F. Barone, M. Barsuglia, T. S. Bauer, and M. G. Beker, et al. (2010). Measurements of Superattenuator seismic isolation by Virgo interferometer. Astropart. Phys. 33, 182-189.
Accadia, T., F. Acernese, F. Antonucci, P. Astone, G. Ballardin, F. Barone, M. Barsuglia, T. S. Bauer, M. G. Beker, and A. Belletoile, et al. (2010). Noise from scattered light in Virgo's second science run data, Classical Quant. Grav. 27, no. 19, doi 10.1088/0264-9381/27/19/194011.
Campbell, K. W. (2009). Estimates of shear-wave Q and k0 for unconsolidated and semiconsolidated sediments in eastern North America, Bull. Seismol. Soc. Amer. 99, no. 4, 2365-2392, doi 10.1785/ 0120080116.
Cantini, P., G. Testa, G. Zanchetta, and R. Cavallini (2001). The Plio-Pleistocene evolution of extensional tectonics in northern Tuscany, as constrained by new gravimetric data from the Montecarlo basin (lower Arno Valley, Italy), Tectonophysics 330, 25-43.
Castagna, J. P., M. L. Batzle, and R. L. Eastwood (1985). Relationships between compressional-wave and shear-wave velocities in clastic silicate rocks, Geophysics 50, 571-581.
Del Pezzo, E., and F. Giudicepietro (2002). Plane wave fitting method for a plane, small aperture, short period seismic array: A MATHCAD 2000 professional program, Comput. Geosci. 28, 59-64.
Del Pezzo, E., G. Lombardo, and S. Spampinato (1989). Attenuation of volcanic tremor at Mt. Etna, Sicily, Bull. Seismol. Soc. Amer. 79, 1989-1994.
Della Rocca, B., R. Mazzanti, and E. Pranzini (1987). Studio geomorfologico della Pianura di Pisa, Geografia Fisica e Dinamica Quaternario 10, 56-84.
Fanucci, F., M. Firpo, and A. Ramella (1987). Genesi ed evoluzione di piane costiere del Mediterraneo: Esempi di piccole piane della Liguria, Geografia Fisica e Dinamica Quaternario 10, 193-203.
Fiori, I., L. Giordano, S. Hild, G. Losurdo, E. Marchetti, G. Mayer, and F. Paoletti (2009). A study of the seismic disturbance produced by the wind park near the gravitational wave detector GEO-600, Proc. 3rd Int. Meeting on Wind Turbine Noise, Aalborg, Denmark, 17-19 June 2009.
Grassi, S., and G. Cortecci (2005). Hydrogeology and geochemistry of the multilayered confined aquifer of the Pisa plain (Tuscany-central Italy), Appl. Geochem. 20, 41-54.
Mariani, M., and R. Prato (1988). I bacini neogenici costieri del margine tirrenico: Approccio sismicostratigrafico, Memorie della Società Geografica Italiana 41, 519-531.
Mazzanti, R., and A. Rau (1994). La geologia, in La pianura di Pisa e i rilievi contermini. La natura e la storia, Mazzanti, R. (Ed.), Memorie della Società Geografica Italiana 50, 31-87.
Patacca, E., R. Sartori, and P. Scandone (1990). Tyrrhenian basin and Apenninic arcs: Kinematic relations since Late Tortonian times, Memorie della Società Geografica Italiana 45, 425-451.
Saulson, P. R (1994). Fundamentals of Interferometric Gravitational Wave Detectors, World Scientific Publishing, Singapore, 316 pp.
Schofield, R. (2001). Seismic Measurements at the Stateline Wind Project, Rept. no. LIGO T020104-00-Z, Laser Interferometer Gravitational Wave Observatory, 28 pp., available at http://www.ligo.caltech.edu/docs/T/T020104-00.pdf (last accessed January 2011).
Stefanelli, P., C. Carmisciano, F. Caratori Tontini, L. Cocchi, N. Beverini, F. Fidecaro, and D. Embriaco (2008). Microgravity vertical gradient measurement in the site of VIRGO interferometric antenna (Pisa plain, Italy), Ann. Geophys. 51, 877-886.
Styles, P. (2005). A detailed study of the propagation and modelling of the effects of low frequency seismic vibration and infrasound from wind turbines, Proc. 1st Int. Meeting on Wind Turbine Noise, Berlin, Germany, 17-18 October 2005.
Vinet, J.-Y., V. Brisson, and S. Braccini (1996). Scattered light noise in gravitational wave interferometric detectors: Coherent effects, Phys. Rev. D 54, 1276-1286.
Welch, P. (1967). A direct digital method of power spectrum estimation, IBM J. Res. Dev. 5, 141.
Withers, M. M., R. C. Aster, C. J. Young, and E. P. Chael (1996). High-frequency analysis of seismic background noise as a function of wind speed and shallow depth, Bull. Seismol. Soc. Amer. 86, 1507-1515.