New method to estimate bedrock shape of small-scale basin using modal properties of sediment

被引:4
|
作者
Suzuki, Yusuke [1 ]
Iiyama, Kahori [2 ]
Morikawa, Hitoshi [1 ]
Sakai, Kimitoshi [3 ]
Araki, Go [4 ]
机构
[1] Tokyo Inst Technol, Dept Civil & Environm Engn, Midori Ku, G3-7-4259 Nagatsuta, Yokohama, Kanagawa 2268502, Japan
[2] Kajima Tech Res Inst, 2-19-1 Tobitakyu, Tokyo 1820036, Japan
[3] Railway Tech Res Inst, 2-8-38 Hikari, Kokubunji, Tokyo 1858540, Japan
[4] Raito Kogyo, C23-3 Suwa, Tsukuba, Ibaraki 3002658, Japan
关键词
Estimation of bedrock shape; Microtremors; 2-D resonance; Mode shape; Sedimentary basin; Frequency domain decomposition (FDD); method; 2-D finite difference method (FDM); 2-DIMENSIONAL RESONANCE; HETEROGENEOUS MEDIA; PHASE VELOCITIES; WAVE PROPAGATION; RAYLEIGH-WAVES; SPECTRAL RATIO; EARTHQUAKE;
D O I
10.1016/j.soildyn.2021.106882
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
2-D resonances are known to occur in sedimentary basins, and it has been reported that the fundamental mode shapes appear to reflect the bedrock shape. This suggests that the bedrock shape of a valley can be estimated by evaluating the relationship between the mode shapes and the bedrock shape, and by identifying the resonance modes from the observation records of the ground motions. In the present study, the fundamental mode shapes of a small-scale valley were identified by applying the frequency domain decomposition (FDD) technique to microtremor observation records. 2-D finite difference models were used to investigate the relationship between the mode shapes and the bedrock shape. A new method was proposed for estimating the bedrock shape by comparing the mode shapes obtained from observation records and a numerical analysis. Furthermore, the applicability of the new method was confirmed using synthetic and observed data.
引用
收藏
页数:10
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