Estimating near-surface shear wave velocity using the P-wave seismograms method in Japan

Using initial P-wave records at 298 seismic stations from the Kiban-Kyoshin network (KiK-net), the P-wave seismograms method is employed to estimate the near-surface shear wave velocity in Japan. The applicability of this method is validated by comparisons between the measured and estimated time-ave...

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Veröffentlicht in:Earthquake spectra 2018-11, Vol.34 (4), p.1955-1971
Hauptverfasser: Miao Yu, Miao Yu, Shi Yang, Shi Yang, Wang Suyang, Wang Suyang
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container_end_page 1971
container_issue 4
container_start_page 1955
container_title Earthquake spectra
container_volume 34
creator Miao Yu, Miao Yu
Shi Yang, Shi Yang
Wang Suyang, Wang Suyang
description Using initial P-wave records at 298 seismic stations from the Kiban-Kyoshin network (KiK-net), the P-wave seismograms method is employed to estimate the near-surface shear wave velocity in Japan. The applicability of this method is validated by comparisons between the measured and estimated time-averaged shear wave velocity to depth Z(VSZ, 5
doi_str_mv 10.1193/011818EQS015M
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The applicability of this method is validated by comparisons between the measured and estimated time-averaged shear wave velocity to depth Z(VSZ, 5&lt;Z&lt;300 m). Using a second-order polynomial regression relating log VSZ and log VS30, the estimated VS30 values agree well with the measured values. We also find that VS30 is directly related with the ratio of radial to vertical components of the initial P-wave velocity time series (RP). 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The applicability of this method is validated by comparisons between the measured and estimated time-averaged shear wave velocity to depth Z(VSZ, 5&lt;Z&lt;300 m). Using a second-order polynomial regression relating log VSZ and log VS30, the estimated VS30 values agree well with the measured values. We also find that VS30 is directly related with the ratio of radial to vertical components of the initial P-wave velocity time series (RP). 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The applicability of this method is validated by comparisons between the measured and estimated time-averaged shear wave velocity to depth Z(VSZ, 5&lt;Z&lt;300 m). Using a second-order polynomial regression relating log VSZ and log VS30, the estimated VS30 values agree well with the measured values. We also find that VS30 is directly related with the ratio of radial to vertical components of the initial P-wave velocity time series (RP). Compared with the theoretical method, the empirical relationship between RP and VS30 has an improvement in the accuracy for VS30 estimation, is basically region-independent for Japan and Central and Eastern North America (CENA), does not need any other parameters, and is potentially useful for other regions of the world.</abstract><cop>London, England</cop><pub>Earthquake Engineering Research Institute</pub><doi>10.1193/011818EQS015M</doi><tpages>17</tpages></addata></record>
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source SAGE Publications
subjects Asia
bedrock
body waves
boreholes
building codes
crust
earthquakes
elastic waves
Far East
ground motion
instruments
Japan
magnitude
measurement
networks
numerical analysis
P-waves
raypaths
S-waves
sediments
seismic waves
seismograms
seismographs
Seismology
shallow-focus earthquakes
soils
statistical analysis
time series analysis
velocity
wave amplification
title Estimating near-surface shear wave velocity using the P-wave seismograms method in Japan
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