Site classification and Vs30 estimation of free-field TSMIP stations using the logging data of EGDT

The Engineering Geological Database for TSMIP (EGDT), the Taiwan Strong Motion Instrumentation Program, has been under construction by the National Center for Research on Earthquake Engineering and the Central Weather Bureau in Taiwan since 2000. Site characterization, comprising surface investigati...

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Published inEngineering geology Vol. 129-130; pp. 68 - 75
Main Authors Kuo, Chun-Hsiang, Wen, Kuo-Liang, Hsieh, Hung-Hao, Lin, Che-Min, Chang, Tao-Ming, Kuo, Kai-Wen
Format Journal Article
LanguageEnglish
Published Kidlington Elsevier B.V 19.03.2012
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Abstract The Engineering Geological Database for TSMIP (EGDT), the Taiwan Strong Motion Instrumentation Program, has been under construction by the National Center for Research on Earthquake Engineering and the Central Weather Bureau in Taiwan since 2000. Site characterization, comprising surface investigations and logging measurements, was carried out throughout the project. We provide a set of specifications and a description to help users understand the subject matter of the database. EGDT contains 469 surveyed stations, 439 of which were drilled and the logging measurements completed. Of these, 385 had logging data reaching at least 30m, and we used these to examine and determine the most accurate extrapolation of Vs30 (the average S-wave velocity of the top 30m of strata) for the other 54 stations with velocity profiles less than 30m. The chosen method assumed that the bottom velocity is identical from the actual depth of the hole to a distance of 30m, that is, the Bottom Constant Velocity (BCV) method. In order to utilize other existing boreholes which have only N values but no velocities in the future, the empirical S-wave velocity equations for seven different regions and the whole of Taiwan were evaluated by a multivariable analysis. Henceforth, for those existing boreholes which have an N profile less than 30m, the S-wave velocity profile can first be calculated by empirical S-wave velocity equations, and then Vs30 can be estimated by reliable extrapolation. Some other studies of site classifications of TSMIP stations were compared with our results to demonstrate the necessity of reclassification. Ultimately, the Vs30 values of the 439 drilled free-field TSMIP stations were derived and the new site classification was achieved according to the Vs30-based provisions of the National Earthquake Hazards Reduction Program. ► 469 stations are surveyed in the Engineering Geological Database for TSMIP (EGDT). ► The BCV was proposed the most accurate extrapolation for Vs30 in Taiwan. ► Empirical S-wave velocity equations are evaluated as a function of N (and depth). ► The proposed Vs30 and site classification are better than the previous results. ► Vs30 of an N profile less than 30m can be derived by the equations and BCV.
AbstractList The Engineering Geological Database for TSMIP (EGDT), the Taiwan Strong Motion Instrumentation Program, has been under construction by the National Center for Research on Earthquake Engineering and the Central Weather Bureau in Taiwan since 2000. Site characterization, comprising surface investigations and logging measurements, was carried out throughout the project. We provide a set of specifications and a description to help users understand the subject matter of the database. EGDT contains 469 surveyed stations, 439 of which were drilled and the logging measurements completed. Of these, 385 had logging data reaching at least 30m, and we used these to examine and determine the most accurate extrapolation of Vs30 (the average S-wave velocity of the top 30m of strata) for the other 54 stations with velocity profiles less than 30m. The chosen method assumed that the bottom velocity is identical from the actual depth of the hole to a distance of 30m, that is, the Bottom Constant Velocity (BCV) method. In order to utilize other existing boreholes which have only N values but no velocities in the future, the empirical S-wave velocity equations for seven different regions and the whole of Taiwan were evaluated by a multivariable analysis. Henceforth, for those existing boreholes which have an N profile less than 30m, the S-wave velocity profile can first be calculated by empirical S-wave velocity equations, and then Vs30 can be estimated by reliable extrapolation. Some other studies of site classifications of TSMIP stations were compared with our results to demonstrate the necessity of reclassification. Ultimately, the Vs30 values of the 439 drilled free-field TSMIP stations were derived and the new site classification was achieved according to the Vs30-based provisions of the National Earthquake Hazards Reduction Program. ► 469 stations are surveyed in the Engineering Geological Database for TSMIP (EGDT). ► The BCV was proposed the most accurate extrapolation for Vs30 in Taiwan. ► Empirical S-wave velocity equations are evaluated as a function of N (and depth). ► The proposed Vs30 and site classification are better than the previous results. ► Vs30 of an N profile less than 30m can be derived by the equations and BCV.
The Engineering Geological Database for TSMIP (EGDT), the Taiwan Strong Motion Instrumentation Program, has been under construction by the National Center for Research on Earthquake Engineering and the Central Weather Bureau in Taiwan since 2000. Site characterization, comprising surface investigations and logging measurements, was carried out throughout the project. We provide a set of specifications and a description to help users understand the subject matter of the database. EGDT contains 469 surveyed stations, 439 of which were drilled and the logging measurements completed. Of these, 385 had logging data reaching at least 30m, and we used these to examine and determine the most accurate extrapolation of Vs30 (the average S-wave velocity of the top 30m of strata) for the other 54 stations with velocity profiles less than 30m. The chosen method assumed that the bottom velocity is identical from the actual depth of the hole to a distance of 30m, that is, the Bottom Constant Velocity (BCV) method. In order to utilize other existing boreholes which have only N values but no velocities in the future, the empirical S-wave velocity equations for seven different regions and the whole of Taiwan were evaluated by a multivariable analysis. Henceforth, for those existing boreholes which have an N profile less than 30m, the S-wave velocity profile can first be calculated by empirical S-wave velocity equations, and then Vs30 can be estimated by reliable extrapolation. Some other studies of site classifications of TSMIP stations were compared with our results to demonstrate the necessity of reclassification. Ultimately, the Vs30 values of the 439 drilled free-field TSMIP stations were derived and the new site classification was achieved according to the Vs30-based provisions of the National Earthquake Hazards Reduction Program.
Author Lin, Che-Min
Hsieh, Hung-Hao
Kuo, Chun-Hsiang
Chang, Tao-Ming
Kuo, Kai-Wen
Wen, Kuo-Liang
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  givenname: Kuo-Liang
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  fullname: Wen, Kuo-Liang
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  givenname: Hung-Hao
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  surname: Lin
  fullname: Lin, Che-Min
  organization: National Center for Research on Earthquake Engineering, Taipei, Taiwan
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  surname: Kuo
  fullname: Kuo, Kai-Wen
  organization: Seismology Center, Central Weather Bureau, Taipei, Taiwan
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Keywords Vs30
S-wave velocity
Taiwan
Site classification
SPT-N
Free field
Instruments
Site analysis
Empirical method
Extrapolation
Classification
Database
S wave
Wave velocity
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Snippet The Engineering Geological Database for TSMIP (EGDT), the Taiwan Strong Motion Instrumentation Program, has been under construction by the National Center for...
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SubjectTerms Applied sciences
Buildings. Public works
earthquakes
environmental engineering
equations
Exact sciences and technology
Geotechnics
instrumentation
Measurements. Technique of testing
S-wave velocity
Site classification
Soil investigations. Testing
SPT-N
Taiwan
taxonomic revisions
Vs30
weather
Title Site classification and Vs30 estimation of free-field TSMIP stations using the logging data of EGDT
URI https://dx.doi.org/10.1016/j.enggeo.2012.01.013
https://www.proquest.com/docview/1710220665
Volume 129-130
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