Interpretation of Seismic Cone Penetration Testing in Silty Soil Rikke Holmsgaard1, Lars Bo Ibsen2, and Benjaminn Nordahl Nielsen3 1PhD. Fellow, Master of Science in Civil Engineering, Aalborg University, Department of Civil Engineering, Sofiendalsvej 11, 9200 Aalborg SV, Denmark, Phone +45 40939994, email:
[email protected] 2Professor, Aalborg University, Department of Civil Engineering, Sofiendalsvej 11, 9200 Aalborg SV, Denmark, Phone +45 99408458, email:
[email protected] 3Associate Professor, Aalborg University, Department of Civil Engineering, Sofiendalsvej 11, 9200 Aalborg SV, Denmark, Phone +45 99408459, email:
[email protected] Corresponding author: Rikke Holmsgaard, email:
[email protected] ABSTRACT Five Seismic Cone Penetration Tests (SCPT) were conducted at a test site in northern Denmark where the subsoil consists primarily of sandy silt with clay bands. A portion of the test data were collected every 0.5 m to compare the efficacy of closely-spaced down-hole data collection on the computation of shear wave velocity. A minimum of eight seismic tests were completed at each depth in order to examine the reliability of shear wave velocity data, as well as to assess the impact of the time interval between CPT termination and seismic test initiation on SCPT results. The shear wave velocity was computed using three different methods: cross-over, cross-correlation and cross-correlation “trimmed with window”. In the “trimmed with window” technique the latter part of the signal is clipped off by setting the amplitude to zero. The result showed that more closely-spaced test intervals actually increased the variability of the shear wave velocity and that time interval between seismic tests is insignificant.