The pseudo method used to calculate shear wave velocity (Vs) in seismic cone penetration (SCP) tests often generates high variability of Vs values at shallow depths. This occurs when travel paths are small and signal variability large to allow accurate arrival time differentiation between successive signals. The offset distance between the source and receivers has the largest influence on signal variability. A method described in this paper shows good results in reducing Vs variability of SCP tests during post processing. The method consists of increasing the sampling interval to calculate Vs and then regrouping the data to provide its original test-depth profile. The method is illustrated with a case study
International audienceThe local geology can strongly affect the seismic ground motion at the surface...
These days cone penetration tests (CPT) have gained more popularity as an alternative to the convent...
textA study was undertaken to improve the signal quality and the resolution of the velocity profile ...
The pseudo method used to calculate shear wave velocity (Vs) in seismic cone penetration (SCP) tests...
The commonly used data reduction methods to determine shear wave velocity (Vs) require the depth int...
In-situ measurement of the dynamic characteristics of surficial soils is becoming more common in geo...
The seismic cone penetration test (SCPTu) is the most efficient means for geotechnical site charact...
The impact of earthquakes worldwide on critical infrastructure has shown the importance of accountin...
Recent developments in cone penetration testing have resulted in the addition of both pore pressure ...
textThe shear wave velocity (VS) profile has been used as an important parameter in characterizing...
Measurements of the shear wave velocity (Vs) of near-surface soils by downhole and crosshole techni...
Surface waves can be used to determine the shear velocity profile from the ground surface to some de...
Site characterization is a basic step in any study involving the estimation of local seismic amplifi...
Different types of sources and receivers used with the seismic cone penetration test were investigat...
704283870Final Report; May 2008-February 2011PDFTech Reporthttp://ntl.bts.gov/lib/36000/36000/36005/...
International audienceThe local geology can strongly affect the seismic ground motion at the surface...
These days cone penetration tests (CPT) have gained more popularity as an alternative to the convent...
textA study was undertaken to improve the signal quality and the resolution of the velocity profile ...
The pseudo method used to calculate shear wave velocity (Vs) in seismic cone penetration (SCP) tests...
The commonly used data reduction methods to determine shear wave velocity (Vs) require the depth int...
In-situ measurement of the dynamic characteristics of surficial soils is becoming more common in geo...
The seismic cone penetration test (SCPTu) is the most efficient means for geotechnical site charact...
The impact of earthquakes worldwide on critical infrastructure has shown the importance of accountin...
Recent developments in cone penetration testing have resulted in the addition of both pore pressure ...
textThe shear wave velocity (VS) profile has been used as an important parameter in characterizing...
Measurements of the shear wave velocity (Vs) of near-surface soils by downhole and crosshole techni...
Surface waves can be used to determine the shear velocity profile from the ground surface to some de...
Site characterization is a basic step in any study involving the estimation of local seismic amplifi...
Different types of sources and receivers used with the seismic cone penetration test were investigat...
704283870Final Report; May 2008-February 2011PDFTech Reporthttp://ntl.bts.gov/lib/36000/36000/36005/...
International audienceThe local geology can strongly affect the seismic ground motion at the surface...
These days cone penetration tests (CPT) have gained more popularity as an alternative to the convent...
textA study was undertaken to improve the signal quality and the resolution of the velocity profile ...