Characterisation of ground motion recording stations in the Groningen gas field View Full Text


Ontology type: schema:ScholarlyArticle      Open Access: True


Article Info

DATE

2018-05

AUTHORS

Rik Noorlandt, Pauline P. Kruiver, Marco P. E. de Kleine, Marios Karaoulis, Ger de Lange, Antonio Di Matteo, Julius von Ketelhodt, Elmer Ruigrok, Benjamin Edwards, Adrian Rodriguez-Marek, Julian J. Bommer, Jan van Elk, Dirk Doornhof

ABSTRACT

The seismic hazard and risk analysis for the onshore Groningen gas field requires information about local soil properties, in particular shear-wave velocity (VS). A fieldwork campaign was conducted at 18 surface accelerograph stations of the monitoring network. The subsurface in the region consists of unconsolidated sediments and is heterogeneous in composition and properties. A range of different methods was applied to acquire in situ VS values to a target depth of at least 30 m. The techniques include seismic cone penetration tests (SCPT) with varying source offsets, multichannel analysis of surface waves (MASW) on Rayleigh waves with different processing approaches, microtremor array, cross-hole tomography and suspension P-S logging. The offset SCPT, cross-hole tomography and common midpoint cross-correlation (CMPcc) processing of MASW data all revealed lateral variations on length scales of several to tens of metres in this geological setting. SCPTs resulted in very detailed VS profiles with depth, but represent point measurements in a heterogeneous environment. The MASW results represent VS information on a larger spatial scale and smooth some of the heterogeneity encountered at the sites. The combination of MASW and SCPT proved to be a powerful and cost-effective approach in determining representative VS profiles at the accelerograph station sites. The measured VS profiles correspond well with the modelled profiles and they significantly enhance the ground motion model derivation. The similarity between the theoretical transfer function from the VS profile and the observed amplification from vertical array stations is also excellent. More... »

PAGES

605-623

Identifiers

URI

http://scigraph.springernature.com/pub.10.1007/s10950-017-9725-6

DOI

http://dx.doi.org/10.1007/s10950-017-9725-6

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1100155698

PUBMED

https://www.ncbi.nlm.nih.gov/pubmed/29755286


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28 schema:description The seismic hazard and risk analysis for the onshore Groningen gas field requires information about local soil properties, in particular shear-wave velocity (<i>V</i><sub>S</sub>). A fieldwork campaign was conducted at 18 surface accelerograph stations of the monitoring network. The subsurface in the region consists of unconsolidated sediments and is heterogeneous in composition and properties. A range of different methods was applied to acquire in situ <i>V</i><sub>S</sub> values to a target depth of at least 30 m. The techniques include seismic cone penetration tests (SCPT) with varying source offsets, multichannel analysis of surface waves (MASW) on Rayleigh waves with different processing approaches, microtremor array, cross-hole tomography and suspension P-S logging. The offset SCPT, cross-hole tomography and common midpoint cross-correlation (CMPcc) processing of MASW data all revealed lateral variations on length scales of several to tens of metres in this geological setting. SCPTs resulted in very detailed <i>V</i><sub>S</sub> profiles with depth, but represent point measurements in a heterogeneous environment. The MASW results represent <i>V</i><sub>S</sub> information on a larger spatial scale and smooth some of the heterogeneity encountered at the sites. The combination of MASW and SCPT proved to be a powerful and cost-effective approach in determining representative <i>V</i><sub>S</sub> profiles at the accelerograph station sites. The measured <i>V</i><sub>S</sub> profiles correspond well with the modelled profiles and they significantly enhance the ground motion model derivation. The similarity between the theoretical transfer function from the <i>V</i><sub>S</sub> profile and the observed amplification from vertical array stations is also excellent.
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