COMPARISON BETWEEN GROUND-MOTION CHARACTERISTICS ON PLATEAU AND LOWLAND SITES BASED ON STRONG-MOTION AND MICROTREMOR OBSERVATIONS

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  • 地震観測・常時微動観測に基づくローム台地と沖積低地の地盤震動特性の比較
  • ジシン カンソク ジョウジ ビドウ カンソク ニ モトヅク ローム ダイチ ト チュウセキ テイチ ノ ジバン シンドウ トクセイ ノ ヒカク

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Abstract

Strong-motion and microtremor observations are carried out in loam plateaus and Holocene lowlands in the Hassaku area, Yokohama, to investigate site-amplification characteristics in the area. Strong-motion observations show that a plateau site has larger site-amplification characteristics in comparison to lowland sites by a factor of about 1.5 in peak horizontal ground velocity and about 2 in spectral peak amplitude of Fourier acceleration spectra. The amplification is due to subsurface soils which are accumulated on soft rocks. Microtremor observations demonstrate that resonance periods on plateaus are related to elevation; high site amplification areas distribute along rivers in the lowlands and on the Shimosueyoshi plateau.

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