2013
DOI: 10.3997/1365-2397.31.8.70632
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Surveying near-surface depocentres by means of shear wave seismics

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Cited by 29 publications
(10 citation statements)
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“…However, the VP/VS values are extremely high in the edges of the profile with values above 20, which seem unrealistic and not representative for saturated clays and sands. The high values of VP/VS in these positions may be related to a lower resolution of the VS and VP models in these areas and/or due to extremely low VS (studies in the same area,Polom et al 2013 andComina et al 2017, obtained similar values) Bailey et al (2013). associate high VP/VS to an increased porosity, saturation and clay content, all of which are conditions present in this study area.…”
mentioning
confidence: 54%
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“…However, the VP/VS values are extremely high in the edges of the profile with values above 20, which seem unrealistic and not representative for saturated clays and sands. The high values of VP/VS in these positions may be related to a lower resolution of the VS and VP models in these areas and/or due to extremely low VS (studies in the same area,Polom et al 2013 andComina et al 2017, obtained similar values) Bailey et al (2013). associate high VP/VS to an increased porosity, saturation and clay content, all of which are conditions present in this study area.…”
mentioning
confidence: 54%
“…The model parameterization was similar in all the lines. Constant values for density (1.7 g/cm 3 ) and Poisson's ratio (0.48) were estimated from the data collected in previous studies (Polom et al 2013;Salas-Romero et al 2016, 2019. Halfspace depth was defined using the information from the extracted dispersion curves (0.5 max), resulting in an averaged value estimated for all the lines (26 m).…”
Section: Inversion Of Dispersion Curvesmentioning
confidence: 99%
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“…Near-surface applications started with refraction techniques but since 1980 significant progress has been made in seismic reflection surveying (Steeples 2005). In the beginning, P-waves (compressional waves) were mainly created by explosives or weight drops, but nowadays seismic vibrators of different sizes are at hand and can be used for P-wave as well as for S-wave (shear wave) surveys (e.g., Krawczyk et al 2012Krawczyk et al , 2013Polom et al 2013;Tamiru and Wiederhold 2020). These studies also show that seismic reflection methods work quite well in the unconsolidated sediments of the North European Lowlands despite only minor velocity contrasts between layers.…”
Section: Seismic Reflection Methodsmentioning
confidence: 99%
“…Large-scale investigations can often only be carried out in connection with research projects (e.g., BURVAL Working Group 2009). Convincing and meaningful studies concerning application of S-and/or P-wave seismic reflections in northern Germany, Denmark and Canada were presented by, e.g., Polom et al (2013), Krawczyk et al (2012Krawczyk et al ( , 2013, Pugin et al (2009Pugin et al ( , 2013; in combination with airborne electromagnetic surveys by Burschil et al (2012a, b), Jørgensen et al (2012), Høyer et al (2013), Tamiru and Wiederhold (2020); and in combination with direct-push by Hoffmann et al (2008). Recently Sun et al (2020) demonstrated the imaging of shallow groundwater resources in glacial deposits by high frequency data using an explosive seismic source.…”
Section: Introductionmentioning
confidence: 99%