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Algorithm of Microseism Processing by the H/V Method to Estimate the Parameters of a Two-Layer Velocity Model Based on Surface Rayleigh Wave Ellipticity. / Yablokov, A. V.; Dergach, P. A.; Liseikin, A. V. et al.

In: Seismic instruments, Vol. 59, No. 4-6, 24.03.2023, p. 116-126.

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@article{a261659496844697b514afcb5bde8b8a,
title = "Algorithm of Microseism Processing by the H/V Method to Estimate the Parameters of a Two-Layer Velocity Model Based on Surface Rayleigh Wave Ellipticity",
abstract = "The research develops the H/V method by designing a microseismic data processing workflow, which includes prefiltering, summation of amplitude spectra, calculation of the component spectrum ratio (H/V curve) and its inversion based on surface Rayleigh wave ellipticity curves. As a result of the algorithm, the resonance frequencies values, depth of the top of the bedrock, and S-wave velocity in the soil and bedrock are determined, tolerant to noise at the point of measurement. The search ranges of the solution to the inverse problem are evaluated using the results of processing active seismic data on refracted and surface waves. As a result of processing the H/V curves, distribution maps of the reconstructed parameters for the entire area of the vibroseismic test site near the settlement of Bystrovka, Novosibirsk oblast, are constructed. The depth of the top of the bedrock, calculated by different seismic methods, are highly correlated with each other. The distribution maps of the reconstructed parameters may apply for studying the near-surface section, estimating the depth of the top of the bedrock, determining the incremental seismic intensity by the seismic impedance method, or calculating synthetic earthquake accelerograms.",
author = "Yablokov, {A. V.} and Dergach, {P. A.} and Liseikin, {A. V.} and Serdyukov, {A. S.}",
note = "The study was supported by a joint grant from the Russian Science Foundation and the Government of Novosibirsk oblast, grant no. 23-27-10042 (https://rscf.ru/project/23-27-10042/). Algorithm of Microseism Processing by the H/V Method to Estimate the Parameters of a Two-Layer Velocity Model Based on Surface Rayleigh Wave Ellipticity / A. V. Yablokov, P. A. Dergach, A. V. Liseikin, A. S. Serdyukov // Seismic Instruments. – 2023. – Vol. 59, No. 4-6. – P. 116-126. – DOI 10.3103/s0747923925700021. ",
year = "2023",
month = mar,
day = "24",
doi = "10.3103/s0747923925700021",
language = "English",
volume = "59",
pages = "116--126",
journal = "Seismic instruments",
issn = "0747-9239",
publisher = "Allerton Press Inc.",
number = "4-6",

}

RIS

TY - JOUR

T1 - Algorithm of Microseism Processing by the H/V Method to Estimate the Parameters of a Two-Layer Velocity Model Based on Surface Rayleigh Wave Ellipticity

AU - Yablokov, A. V.

AU - Dergach, P. A.

AU - Liseikin, A. V.

AU - Serdyukov, A. S.

N1 - The study was supported by a joint grant from the Russian Science Foundation and the Government of Novosibirsk oblast, grant no. 23-27-10042 (https://rscf.ru/project/23-27-10042/). Algorithm of Microseism Processing by the H/V Method to Estimate the Parameters of a Two-Layer Velocity Model Based on Surface Rayleigh Wave Ellipticity / A. V. Yablokov, P. A. Dergach, A. V. Liseikin, A. S. Serdyukov // Seismic Instruments. – 2023. – Vol. 59, No. 4-6. – P. 116-126. – DOI 10.3103/s0747923925700021.

PY - 2023/3/24

Y1 - 2023/3/24

N2 - The research develops the H/V method by designing a microseismic data processing workflow, which includes prefiltering, summation of amplitude spectra, calculation of the component spectrum ratio (H/V curve) and its inversion based on surface Rayleigh wave ellipticity curves. As a result of the algorithm, the resonance frequencies values, depth of the top of the bedrock, and S-wave velocity in the soil and bedrock are determined, tolerant to noise at the point of measurement. The search ranges of the solution to the inverse problem are evaluated using the results of processing active seismic data on refracted and surface waves. As a result of processing the H/V curves, distribution maps of the reconstructed parameters for the entire area of the vibroseismic test site near the settlement of Bystrovka, Novosibirsk oblast, are constructed. The depth of the top of the bedrock, calculated by different seismic methods, are highly correlated with each other. The distribution maps of the reconstructed parameters may apply for studying the near-surface section, estimating the depth of the top of the bedrock, determining the incremental seismic intensity by the seismic impedance method, or calculating synthetic earthquake accelerograms.

AB - The research develops the H/V method by designing a microseismic data processing workflow, which includes prefiltering, summation of amplitude spectra, calculation of the component spectrum ratio (H/V curve) and its inversion based on surface Rayleigh wave ellipticity curves. As a result of the algorithm, the resonance frequencies values, depth of the top of the bedrock, and S-wave velocity in the soil and bedrock are determined, tolerant to noise at the point of measurement. The search ranges of the solution to the inverse problem are evaluated using the results of processing active seismic data on refracted and surface waves. As a result of processing the H/V curves, distribution maps of the reconstructed parameters for the entire area of the vibroseismic test site near the settlement of Bystrovka, Novosibirsk oblast, are constructed. The depth of the top of the bedrock, calculated by different seismic methods, are highly correlated with each other. The distribution maps of the reconstructed parameters may apply for studying the near-surface section, estimating the depth of the top of the bedrock, determining the incremental seismic intensity by the seismic impedance method, or calculating synthetic earthquake accelerograms.

UR - https://www.mendeley.com/catalogue/51385c50-6416-3745-a397-98ab135174cf/

UR - https://elibrary.ru/item.asp?id=81834750

U2 - 10.3103/s0747923925700021

DO - 10.3103/s0747923925700021

M3 - Article

VL - 59

SP - 116

EP - 126

JO - Seismic instruments

JF - Seismic instruments

SN - 0747-9239

IS - 4-6

ER -

ID: 71568865