2018
DOI: 10.1007/s10950-018-9767-4
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Analysis of seismic noise in the Romanian-Bulgarian cross-border region

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Cited by 6 publications
(4 citation statements)
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“…However, recent studies that have focused on the analysis of urban seismic noise variations provided insights into the sources responsible for generating seismic noise in different frequency bands. Road traffic has an important contribution to the seismic noise wave field in various frequency bands, such as 2-9 and 10-20 Hz (Dias et al, 2020), 2.5-10 Hz (Green et al, 2017), 8-35 Hz (Boese et al, 2015, and 8-12 Hz (Diaz et al, 2017). Overground and subway trains generate seismic noise at very low frequencies (∼ 0.01-0.05 Hz) (Sheen et al, 2009;Diaz et al, 2017;Green et al, 2017) and at high frequencies (20-40 Hz) (Diaz et al, 2017).…”
Section: Discussionmentioning
confidence: 99%
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“…However, recent studies that have focused on the analysis of urban seismic noise variations provided insights into the sources responsible for generating seismic noise in different frequency bands. Road traffic has an important contribution to the seismic noise wave field in various frequency bands, such as 2-9 and 10-20 Hz (Dias et al, 2020), 2.5-10 Hz (Green et al, 2017), 8-35 Hz (Boese et al, 2015, and 8-12 Hz (Diaz et al, 2017). Overground and subway trains generate seismic noise at very low frequencies (∼ 0.01-0.05 Hz) (Sheen et al, 2009;Diaz et al, 2017;Green et al, 2017) and at high frequencies (20-40 Hz) (Diaz et al, 2017).…”
Section: Discussionmentioning
confidence: 99%
“…Road traffic has an important contribution to the seismic noise wave field in various frequency bands, such as 2-9 and 10-20 Hz (Dias et al, 2020), 2.5-10 Hz (Green et al, 2017), 8-35 Hz (Boese et al, 2015, and 8-12 Hz (Diaz et al, 2017). Overground and subway trains generate seismic noise at very low frequencies (∼ 0.01-0.05 Hz) (Sheen et al, 2009;Diaz et al, 2017;Green et al, 2017) and at high frequencies (20-40 Hz) (Diaz et al, 2017). Furthermore, industrial activities can also contribute to the seismic noise spectra in the 1-25 and 25-40 Hz bands (Groos and Ritter, 2009).…”
Section: Discussionmentioning
confidence: 99%
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“…Seismometer monitoring and evaluation activities at the InaTEWS are carried out through a seismometer sensor calibration system using the Seismic Data Quality Analysis software or known as SQLX [1]. SQLX software produces digital images in the form of power spectrum density, also known as Power Spectral Density (PSD), and probability density, also called Probability Density Function (PDF), derived from seismometer measurements [2][3]. The digital image can describe the condition of the seismometer that operates following the spectrum result.…”
Section: Introductionmentioning
confidence: 99%