<?xml version="1.0"?>
<oai_dc:dc xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:title>Characterization of site conditions (soil class, V-s30, velocity profiles) for 33 stations from the French permanent accelerometric network (RAP) using surface-wave methods</dc:title>
  <dc:creator>Hollender, F.</dc:creator>
  <dc:creator>/Cornou, C&#xE9;cile</dc:creator>
  <dc:creator>Dechamp, A.</dc:creator>
  <dc:creator>Oghalaei, K.</dc:creator>
  <dc:creator>Renalier, F.</dc:creator>
  <dc:creator>Maufroy, E.</dc:creator>
  <dc:creator>Burnouf, C.</dc:creator>
  <dc:creator>Thomassin, S.</dc:creator>
  <dc:creator>/Wathelet, Marc</dc:creator>
  <dc:creator>Bard, P. Y.</dc:creator>
  <dc:creator>Boutin, V.</dc:creator>
  <dc:creator>Desbordes, C.</dc:creator>
  <dc:creator>Douste-Bacque, I.</dc:creator>
  <dc:creator>Foundotos, L.</dc:creator>
  <dc:creator>Guyonnet-Benaize, C.</dc:creator>
  <dc:creator>Perron, V.</dc:creator>
  <dc:creator>Regnier, J.</dc:creator>
  <dc:creator>Roulle, A.</dc:creator>
  <dc:creator>Langlais, M.</dc:creator>
  <dc:creator>Sicilia, D.</dc:creator>
  <dc:subject>Accelerometric network</dc:subject>
  <dc:subject>Surface-wave methods</dc:subject>
  <dc:subject>Velocity profile</dc:subject>
  <dc:subject>V-s30</dc:subject>
  <dc:description>Data provided by accelerometric networks are important for seismic hazard assessment. The correct use of accelerometric signals is conditioned by the station site metadata quality (i.e., soil class, V-s30, velocity profiles, and other relevant information that can help to quantify site effects). In France, the permanent accelerometric network consists of about 150 stations. Thirty-three of these stations in the southern half of France have been characterized, using surface-wave-based methods that allow derivation of velocity profiles from dispersion curves of surface waves. The computation of dispersion curves and their subsequent inversion in terms of shear-wave velocity profiles has allowed estimation of V-s30 values and designation of soil classes, which include the corresponding uncertainties. From a methodological point of view, this survey leads to the following recommendations: (1) perform both active (multi-analysis surface waves) and passive (ambient vibration arrays) measurements to derive dispersion curves in a broadband frequency range; (2) perform active acquisitions for both vertical (Rayleigh wave) and horizontal (Love wave) polarities. Even when the logistic contexts are sometimes difficult, the use of surface-wave-based methods is suitable for station-site characterization, even on rock sites. In comparison with previous studies that have mainly estimated V-s30 indirectly, the new values here are globally lower, but the EC8-A class sites remain numerous. However, even on rock sites, high frequency amplifications may affect accelerometric records, due to the shallow relatively softer layers.</dc:description>
  <dc:date>2018</dc:date>
  <dc:type>text</dc:type>
  <dc:identifier>https://www.documentation.ird.fr/hor/fdi:010073025</dc:identifier>
  <dc:identifier>fdi:010073025</dc:identifier>
  <dc:identifier>Hollender F., Cornou C&#xE9;cile, Dechamp A., Oghalaei K., Renalier F., Maufroy E., Burnouf C., Thomassin S., Wathelet Marc, Bard P. Y., Boutin V., Desbordes C., Douste-Bacque I., Foundotos L., Guyonnet-Benaize C., Perron V., Regnier J., Roulle A., Langlais M., Sicilia D.. Characterization of site conditions (soil class, V-s30, velocity profiles) for 33 stations from the French permanent accelerometric network (RAP) using surface-wave methods. 2018, 16 (6),  2337-2365</dc:identifier>
  <dc:language>EN</dc:language>
  <dc:coverage>FRANCE</dc:coverage>
</oai_dc:dc>
