Study of mechanism of site amplification effects on ground motion in far field loess during Wenchuan Ms8.0 earthquake
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Study of mechanism of site amplification effects on ground motion in far field loess during Wenchuan Ms8.0 earthquake
Vol. 33, Issue 12, (2012)
作者机构:
1. 甘肃省地震局 中国地震局黄土地震工程重点实验室,兰州,730000
2. 中国地震局兰州地震研究所,兰州,730000
3. 甘肃省岩土防灾工程技术研究中心,兰州,730000
4. 中国科学院寒区旱区环境与工程研究所 冻土工程国家重点实验室,兰州,730000
作者简介:
基金信息:
DOI:
CLC:TU435
Online First:15 December 2012,
Published:2012
稿件说明:
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WU Zhi-jian, WANG Lan-min, CHEN Tuo, et al. Study of mechanism of site amplification effects on ground motion in far field loess during Wenchuan Ms8.0 earthquake[J]. 2012, 33(12).
DOI:
WU Zhi-jian, WANG Lan-min, CHEN Tuo, et al. Study of mechanism of site amplification effects on ground motion in far field loess during Wenchuan Ms8.0 earthquake[J]. 2012, 33(12).DOI:
Study of mechanism of site amplification effects on ground motion in far field loess during Wenchuan Ms8.0 earthquake
Based on earthquake damage investigation after the Wenchuan Ms8.0 earthquake
it is discovered that the phenomena of site amplification effects on ground motion were very obvious both in the mountainous area of southeastern Gansu province and the Loess Plateau areas. Combining with the borehole exploration
site seismic response analysis of the typical loess tableland at Pingliang City
Gansu province is carried out applying the dynamic finite element method of two dimensions linearly equivalent for dynamic response numerical calculation; the local amplification effect of the loess tableland is studied as well. The results show that there are seismic amplification effects at loess tableland; and acceleration
velocity and displacement increases with increase in tableland height gradually. Moreover
the low frequency components become more abundant and the high-frequency components are absorbed with increase in tableland height. The long-period components of acceleration response spectrum have increased gradually as well. The numerical results are basically consistent with the earthquake damages
so as to have certain scientific significance for the reasonable seismic fortification in loess regions.