Joint deconvolution of building and downhole seismic recordings: an application to three test cases

In this study, the joint deconvolution is applied to recordings of three test cases located in the cities of Bishkek, Kyrgyzstan, Istanbul, Turkey, and Mexico City, Mexico. Each test case consists of a building equipped with sensors and a nearby borehole installation in order to investigate differen...

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Veröffentlicht in:Bulletin of earthquake engineering 2018-02, Vol.16 (2), p.613-641
Hauptverfasser: Petrovic, Bojana, Parolai, Stefano, Pianese, Giovanna, Dikmen, S. Umit, Moldobekov, Bolot, Orunbaev, Sagynbek, Paolucci, Roberto
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container_end_page 641
container_issue 2
container_start_page 613
container_title Bulletin of earthquake engineering
container_volume 16
creator Petrovic, Bojana
Parolai, Stefano
Pianese, Giovanna
Dikmen, S. Umit
Moldobekov, Bolot
Orunbaev, Sagynbek
Paolucci, Roberto
description In this study, the joint deconvolution is applied to recordings of three test cases located in the cities of Bishkek, Kyrgyzstan, Istanbul, Turkey, and Mexico City, Mexico. Each test case consists of a building equipped with sensors and a nearby borehole installation in order to investigate different cases of coupling (impedance contrasts) between the building and the soil by analyzing the wave propagation through the building-soil-layers, and hence resolving the soil–structure-interactions. The three installations considering different dynamic characteristics of buildings and soil, and thus, different building-soil couplings, are investigated. The seismic input (i.e., the part of the wave field containing only the up-going waves after removing all down-going waves) and the part of the wave field that is associated with the waves radiated back from the building are separated by using the constrained deconvolution. The energy being radiated back from the building to the soil has been estimated for the three test cases. The values obtained show that even at great depths (and therefore distances), the amount of wave field radiated back by the building to the soil is significant (e.g., for the Bishkek case, at 145 m depth, 10% of the estimated real input energy is expected to be emitted back from the building; for Istanbul at 50 m depth, the value is also 10–15% of the estimated real input energy while for Mexico City at 45 m depth, it is 25–65% of the estimated real input energy). Such results confirm the active role of buildings in shaping the wave field.
doi_str_mv 10.1007/s10518-017-0215-6
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subjects Aseismic buildings
Boreholes
Case depth
Civil Engineering
Connectors
Couplings
Deconvolution
Depth
Dynamic characteristics
Earth and Environmental Science
Earth Sciences
Earthquake construction
Energy
Environmental Engineering/Biotechnology
Geophysics/Geodesy
Geotechnical Engineering & Applied Earth Sciences
Hydrogeology
Interactions
Original Research Paper
Seismic waves
Soil
Soil analysis
Soil dynamics
Soil investigations
Soil layers
Soil structure
Soils
Structural Geology
Studies
Wave propagation
title Joint deconvolution of building and downhole seismic recordings: an application to three test cases
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