@article{PAR00025688,
  title = {{T}he "{G}lass {B}eads" {C}oupling {S}olution for {B}orehole and {P}osthole {A}ccelerometers: {S}haking {T}able {T}ests and {F}ield {R}etrievability},
  author = {{H}ollender, {F}. and {T}heodoulidis, {N}. and {M}ariscal, {A}rmand and {C}haudat, {T}. and {S}teidl, {J}. and {R}oumelioti, {Z}.},
  editor = {},
  language = {{ENG}},
  abstract = {{B}orehole accelerometers are designed to record strong ground movements at depth. {T}hey have become an important complement to surface accelerometers for seismic and earthquake engineering applications. {B}orehole accelerometers present several imple-mentation challenges, including their coupling with the geological environment. {O}ne possible coupling solution is the use of small glass beads, which are placed inside the borehole casing with the purpose of filling in any empty space between the sensor and the casing walls. {W}e carried out a test on a shaking table, over a wide range of peak ground accelerations ({PGA} from 0.17 to 1.64g), allowing the comparison of the sig-nals between a surface accelerometer and a borehole accelerometer coupled through the glass beads. {T}hese tests show that there is almost no difference between the surface and borehole accelerometer signals between 0.5 and 25 {H}z, and only very small differences outside this band (0.2-0.5 {H}z and 25-80 {H}z). {F}urthermore, experience from multiple ver-tical accelerometric arrays show that an installation using glass beads is "reversible", that is, 30 yr after the initial installation it can still be possible to easily extract the acceler-ometers for repair or replacement, without any problems or damage to the sensors.},
  keywords = {},
  booktitle = {},
  journal = {{S}eismological {R}esearch {L}etters},
  volume = {94},
  numero = {2},
  pages = {925--934},
  ISSN = {0895-0695},
  year = {2023},
  DOI = {10.1785/0220220292},
  URL = {https://www.documentation.ird.fr/hor/{PAR}00025688},
}