A numerical study of 3D topographic site effects considering wavefield incident direction and geomorphometric parameters

The topographic site effect plays a vital role in controlling the characteristics of earthquake ground motions. Due to its complexity, the factors affecting topographic amplification have not been fully identified. In this study, 100 ground motion simulations generated by double-couple point sources...

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Main Authors: Fuchen Wang, Qiang Ma, Dongwang Tao, Quancai Xie
Format: Article
Language:English
Published: Frontiers Media S.A. 2023-01-01
Series:Frontiers in Earth Science
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/feart.2022.996389/full
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author Fuchen Wang
Fuchen Wang
Qiang Ma
Qiang Ma
Dongwang Tao
Dongwang Tao
Quancai Xie
Quancai Xie
author_facet Fuchen Wang
Fuchen Wang
Qiang Ma
Qiang Ma
Dongwang Tao
Dongwang Tao
Quancai Xie
Quancai Xie
author_sort Fuchen Wang
collection DOAJ
description The topographic site effect plays a vital role in controlling the characteristics of earthquake ground motions. Due to its complexity, the factors affecting topographic amplification have not been fully identified. In this study, 100 ground motion simulations generated by double-couple point sources in the homogeneous linear elastic half-space are performed based on the 3D (three-dimensional) Spectral Element Method, taking the Menyuan area of Qinghai Province, China as a local testbed site. A relationship between incident direction and the strength of topographic amplification has been observed. The horizontal ground motion is affected by the back-azimuth, which is typically chosen to be the direction from seismic station to seismic source measured clockwise from north. Specifically, the east-west PGA (Peak Ground-motion Acceleration) is significantly amplified when back-azimuth is about 90° or 270°, and the north-south PGA is significantly amplified when back-azimuth is around 0° or 180°. The vertical ground motion is affected by the dipping angle, which is the angle from vertical at which an incoming seismic wave arrives. The vertical PGA is strongly amplified when the seismic wave is almost horizontally incident (e.g., dipping angle = 78°). A correlation study between geomorphometric parameters and frequency-dependent topographic amplification indicates that relative elevation and smoothed curvature contain similar information, both of which are closely related to the topographic amplification of horizontal components, but not the vertical component. Our study reveals the influence of source and propagation path on topographic amplification and provides a reference for considering the topographic site effect in real engineering sites.
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spelling doaj.art-685796cb0bc549dd862fca135048ffde2023-01-05T06:25:47ZengFrontiers Media S.A.Frontiers in Earth Science2296-64632023-01-011010.3389/feart.2022.996389996389A numerical study of 3D topographic site effects considering wavefield incident direction and geomorphometric parametersFuchen Wang0Fuchen Wang1Qiang Ma2Qiang Ma3Dongwang Tao4Dongwang Tao5Quancai Xie6Quancai Xie7Key Laboratory of Earthquake Engineering and Engineering Vibration, Institute of Engineering Mechanics, China Earthquake Administration, Harbin, ChinaKey Laboratory of Earthquake Disaster Mitigation, Ministry of Emergency Management, Harbin, ChinaKey Laboratory of Earthquake Engineering and Engineering Vibration, Institute of Engineering Mechanics, China Earthquake Administration, Harbin, ChinaKey Laboratory of Earthquake Disaster Mitigation, Ministry of Emergency Management, Harbin, ChinaKey Laboratory of Earthquake Engineering and Engineering Vibration, Institute of Engineering Mechanics, China Earthquake Administration, Harbin, ChinaKey Laboratory of Earthquake Disaster Mitigation, Ministry of Emergency Management, Harbin, ChinaKey Laboratory of Earthquake Engineering and Engineering Vibration, Institute of Engineering Mechanics, China Earthquake Administration, Harbin, ChinaKey Laboratory of Earthquake Disaster Mitigation, Ministry of Emergency Management, Harbin, ChinaThe topographic site effect plays a vital role in controlling the characteristics of earthquake ground motions. Due to its complexity, the factors affecting topographic amplification have not been fully identified. In this study, 100 ground motion simulations generated by double-couple point sources in the homogeneous linear elastic half-space are performed based on the 3D (three-dimensional) Spectral Element Method, taking the Menyuan area of Qinghai Province, China as a local testbed site. A relationship between incident direction and the strength of topographic amplification has been observed. The horizontal ground motion is affected by the back-azimuth, which is typically chosen to be the direction from seismic station to seismic source measured clockwise from north. Specifically, the east-west PGA (Peak Ground-motion Acceleration) is significantly amplified when back-azimuth is about 90° or 270°, and the north-south PGA is significantly amplified when back-azimuth is around 0° or 180°. The vertical ground motion is affected by the dipping angle, which is the angle from vertical at which an incoming seismic wave arrives. The vertical PGA is strongly amplified when the seismic wave is almost horizontally incident (e.g., dipping angle = 78°). A correlation study between geomorphometric parameters and frequency-dependent topographic amplification indicates that relative elevation and smoothed curvature contain similar information, both of which are closely related to the topographic amplification of horizontal components, but not the vertical component. Our study reveals the influence of source and propagation path on topographic amplification and provides a reference for considering the topographic site effect in real engineering sites.https://www.frontiersin.org/articles/10.3389/feart.2022.996389/fulltopographic site effectspectral element methodback-azimuthdipping anglerelative elevationsmoothed curvature
spellingShingle Fuchen Wang
Fuchen Wang
Qiang Ma
Qiang Ma
Dongwang Tao
Dongwang Tao
Quancai Xie
Quancai Xie
A numerical study of 3D topographic site effects considering wavefield incident direction and geomorphometric parameters
Frontiers in Earth Science
topographic site effect
spectral element method
back-azimuth
dipping angle
relative elevation
smoothed curvature
title A numerical study of 3D topographic site effects considering wavefield incident direction and geomorphometric parameters
title_full A numerical study of 3D topographic site effects considering wavefield incident direction and geomorphometric parameters
title_fullStr A numerical study of 3D topographic site effects considering wavefield incident direction and geomorphometric parameters
title_full_unstemmed A numerical study of 3D topographic site effects considering wavefield incident direction and geomorphometric parameters
title_short A numerical study of 3D topographic site effects considering wavefield incident direction and geomorphometric parameters
title_sort numerical study of 3d topographic site effects considering wavefield incident direction and geomorphometric parameters
topic topographic site effect
spectral element method
back-azimuth
dipping angle
relative elevation
smoothed curvature
url https://www.frontiersin.org/articles/10.3389/feart.2022.996389/full
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