Strong Motion Instrumentation for Civil Engineering Structures 2001
DOI: 10.1007/978-94-010-0696-5_21
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Estimation of dynamic characteristics of ground and structures with microtremor measurements- A supportive tool for strong ground motion instrumentation

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Cited by 42 publications
(74 citation statements)
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“…However, we cannot obtain such low‐frequency data below about 0.1 Hz due to the low sensitivity of the short‐period sensors. For further improvement of the velocity estimation, the technique of Nakamura (Berg et al., 2018; Lin et al., 2014; Nakamura, 1989) and the joint inversion of ambient noise and receiver functions (e.g., Ball et al., 2014; Bodin et al., 2012) could be feasible. However, such research is beyond the scope of this study.…”
Section: Potential Of Obs Array For Investigating 3‐d Sedimentary Str...mentioning
confidence: 99%
“…However, we cannot obtain such low‐frequency data below about 0.1 Hz due to the low sensitivity of the short‐period sensors. For further improvement of the velocity estimation, the technique of Nakamura (Berg et al., 2018; Lin et al., 2014; Nakamura, 1989) and the joint inversion of ambient noise and receiver functions (e.g., Ball et al., 2014; Bodin et al., 2012) could be feasible. However, such research is beyond the scope of this study.…”
Section: Potential Of Obs Array For Investigating 3‐d Sedimentary Str...mentioning
confidence: 99%
“…The most traditional techniques for site effect estimation of the S n term, known as convolutive methods, are based upon computation of the ratio between: (a) the spectrum of the signal (or a portion of it) at the (sedimentary) site of interest; and (b) the spectrum of a reference signal, preferably recorded at a nearby (bedrock) site. Similarly, Nakamura (1989; and Nakamura and Gurler (2001) analyzed site effects by a method based on the computation of the spectral ratio between horizontal (usually the square root of the product between the spectra of the NS and EW components is used) and vertical components (H/V) obtained from seismic noise (microtremors).…”
Section: A Warning About Site Effectsmentioning
confidence: 99%
“…HVSR method is one of the main applications about seismic noise study. It was developed by Nakamura (1989) for the definition of the characteristics of the subsoil through the study of the environmental seismic noise (microtremors). A three‐component broadband velocimeter measures vertical and two horizontal (north–south and east–west) components of ambient seismic noise, which includes microtremors induced by wind, ocean waves and anthropogenic activity.…”
Section: Geophysical Measurementsmentioning
confidence: 99%