Station Overview

image
legend Overview at SOLB
Overview Location
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Network CH
Station Code SOLB
Station Description Solothurn, Schulhaus Bruehl, SO
Latitude (WGS84) 47.20683
Longitude (WGS84) 7.517052
Station altitude (CH1903) 430.0
running from 2011-11-22
...until now
Waveform Access open
Sensor Types Accelerometer
Geological Unit Alluvial fan
Site Morphology Class T1
T1: flat; T2: slope; T3: ridge and T4: steep ridge;
following Pessina and Fiorini (2014) A GIS procedure for fast topographic characterization of seismic recording stations, Soil Dynamics and Earthquake Engineering, 63, p248-258
Site Morphology Description Centre of the Aar alluvial plain
Ground type EC8 C
Ground type SIA D
Basin Information Aar basin, interface at fundamental frequency at 180 m depth
Reference Michel Clotaire, Burjanek J., Poggi V., Roten D., Cauzzi C., Fäh D., "Solothurn-Brühl (SOLB) Site characterization report", Swiss Seismological Service, ETH Zürich, 2013
Resonance Frequency (Hz) .54
Uncertainty Factor -
Vs 30 (m/s) 274
Location Map


Federal Office of Topograpy: National Map 1:25‘000
Topography Map


Federal Office of Topograpy: DHM25: Digital Height Model 1:25000
Geology Map

Federal Office of Topograpy: Geological map of Switzerland 1:500‘000

Sensor locations

Location Code (none)
Opening Date 22-11-2011
End Date -
Housing Class Urban free field
Housing Description SED small vault
sensor depth below station 0.5 m
Distance to Building (m) 5

Current Instrumentation

Location code (none)
On date 22-11-2011 00:00:00
Off date -
Sensor model EpiSensor ES-T
Sensor manufacturer Kinemetrics
Digitizer model Taurus
Digitizer manufacturer Nanometrics
Channels HGE , HGN , HGZ
Stream Noise (last week) HGE , HGN , HGZ

Site Characterization

channel group
Empirical Amplification
CH.SOLB..HG not available

Obtained from spectral modeling of small earthquakes with constant update.

  • Top: Fourier amplification with elastic (dashed line) and anelastic (solid line) amplification functions;
  • Centre: 5% damped response spectra amplification (anelastic);
  • Bottom: Number of recordings used.

See Edwards et al. (2013), Determination of Site Amplification from Regional Seismicity: Application to the Swiss National Seismic Networks. Seismological Research Letters, 84(4), 611–621.

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Authoritative Site Characterization Analysis details...
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