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液状化発生率におよぼす強震動の継続時間と地域性の影響
https://nied-repo.bosai.go.jp/records/5963
https://nied-repo.bosai.go.jp/records/596334249237-c497-4f78-921b-64c115c06626
Item type | researchmap(1) | |||||||||||||||||||||
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公開日 | 2023-03-30 | |||||||||||||||||||||
タイトル | ||||||||||||||||||||||
言語 | ja | |||||||||||||||||||||
タイトル | 液状化発生率におよぼす強震動の継続時間と地域性の影響 | |||||||||||||||||||||
タイトル | ||||||||||||||||||||||
言語 | en | |||||||||||||||||||||
タイトル | Liquefaction Occurrence Ratio Estimation Considering Strong Ground Motion Duration and Regional Characteristics | |||||||||||||||||||||
言語 | ||||||||||||||||||||||
言語 | jpn | |||||||||||||||||||||
著者 |
先名重樹
× 先名重樹
× 松岡昌志
× 若松加寿江
× 翠川三郎
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抄録 | ||||||||||||||||||||||
内容記述タイプ | Other | |||||||||||||||||||||
内容記述 | <p>2011年東北地方太平洋沖地震では,東北地方から関東地方にかけての極めて広い範囲で液状化が発生した.特に関東地方の被害範囲・規模は非常に大きなものであった.被害が大きくなった理由については,継続時間の長さが被害規模を大きくしたことが推測される.本研究では,東北地方太平洋沖地震および近年の液状化が発生した地震において液状化発生率には地域性がみられること,および,液状化発生率には計測震度のみならず,継続時間の影響もみられることを示した.そして,地震動強さの指標としてリアルタイム震度と継続時間から計算される<i>ΔIs</i>を導入し,<i>ΔIs</i>から液状化発生率を推定する簡便法を提案した.</p> | |||||||||||||||||||||
言語 | ja | |||||||||||||||||||||
抄録 | ||||||||||||||||||||||
内容記述タイプ | Other | |||||||||||||||||||||
内容記述 | <p>During to the 2011 off the Pacific coast of Tohoku Earthquake (the Great East Japan Earthquake) that occurred on March 11, 2011, liquefaction occurred over a large area in the Tohoku and Kanto regions. At present, the areas where liquefactions were identified extend from Aomori Prefecture in the north to Kanagawa Prefecture in the south within approximately 650-km long zone. This earthquake was characterized by the long duration of ground motion with several successive events of the source area. In this paper, firstly we examined the liquefaction occurrence ratio in terms of measured seismic intensities by geomorphologic classification units based on a dataset of strong ground motion data and observation records of liquefaction sites during the 2011 off the Pacific coast of Tohoku Earthquake to show the liquefaction potentials differing between the Tohoku and the Kanto regions. Next, in order to investigate the effect of the ground motion duration, we calculated the real-time seismic intensity and its accumulated index (<i>ΔIs</i>) as explanatory parameters of ground motion intensity. As a result, although it was found that there was still regionality in the Tohoku and the Kanto regions, it clarified that the large <i>ΔIs</i> caused to increase the liquefaction occurrence ratio.</p> | |||||||||||||||||||||
言語 | en | |||||||||||||||||||||
書誌情報 |
ja : 日本地震工学会論文集(Web) en : 日本地震工学会論文集(Web) 巻 18, 号 2, p. 2_82-2_94, 発行日 2018 |
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出版者 | ||||||||||||||||||||||
言語 | ja | |||||||||||||||||||||
出版者 | 公益社団法人 日本地震工学会 | |||||||||||||||||||||
出版者 | ||||||||||||||||||||||
言語 | en | |||||||||||||||||||||
出版者 | JAPAN ASSOCIATION FOR EARTHQUAKE ENGINEERING | |||||||||||||||||||||
ISSN | ||||||||||||||||||||||
収録物識別子タイプ | ISSN | |||||||||||||||||||||
収録物識別子 | 1884-6246 | |||||||||||||||||||||
DOI | ||||||||||||||||||||||
関連識別子 | 10.5610/jaee.18.2_82 |