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Short Note |
GeoForschungsZentrum
Telegrafenberg
Potsdam, 14473,
Germany
(S.P., P.B., C.M.)
Noise measurements were carried out in the Cologne area (Germany), and the
resonance frequency of each site was estimated from the main peak in the
spectral ratio between the horizontal and vertical component. For 32 of these
sites, the thickness of the sedimentary cover was known from boreholes, and a
clear correlation between resonance frequency and sediment thickness was
observed. A formula that correlates cover thickness with frequency of the main
peak in the horizontal-to-vertical spectral ratio was derived. In addition, a
best-fitting shear-wave-velocity distribution with depth,
vs(z), as well as a relationship between average
shear-wave velocity
s and thickness
of the sedimentary cover, was calculated. By using all of the noise
measurements and applying the derived relationships, we obtained a subsoil
classification for the Cologne area.
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