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Engineering properties of the soil around Nishiyama and Kompirayama after the eruption at Mount Usu in 2000
http://hdl.handle.net/10191/39229
http://hdl.handle.net/10191/3922932be73bf-e811-43ff-a2b1-6ddc44a645e7
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
23_63-76.pdf (687.1 kB)
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| Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
|---|---|---|---|---|---|---|
| 公開日 | 2016-03-08 | |||||
| タイトル | ||||||
| タイトル | Engineering properties of the soil around Nishiyama and Kompirayama after the eruption at Mount Usu in 2000 | |||||
| タイトル | ||||||
| タイトル | Engineering properties of the soil around Nishiyama and Kompirayama after the eruption at Mount Usu in 2000 | |||||
| 言語 | en | |||||
| 言語 | ||||||
| 言語 | eng | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | Mount Usu | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | Volcanic eruption | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | Shear strength | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | Consistency limit | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | X-ray diffraction | |||||
| 資源タイプ | ||||||
| 資源 | http://purl.org/coar/resource_type/c_6501 | |||||
| タイプ | departmental bulletin paper | |||||
| 著者 |
Tiwari, Binod
× Tiwari, Binod× Marui, Hideaki× Sato, Osamu× Yamagishi, Hiromitsu× Watanabe, Naoki× Furuya, Gen× Suzuki, Koji× Inaba, Kazunari× Shimura, Kazuo× Yamazaki, Fumiaki |
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| 抄録 | ||||||
| 内容記述タイプ | Abstract | |||||
| 内容記述 | Mount Usu is erupting frequently from 18th century. Comparing the recent eruptions, the property of the erupted materials have been found different in various eruption periods. The major eruption in 1978 had been concentrated in Mount Koushu and Mount Oushu. However, the eruption of 2000 had been localized around Nisiyama and Kompirayama area. The soil samples collected from Nishiyama and Kompirayama had shown slight difference in strength and other soil physical properties. The mineralogical properties also show the possibility of different rocks in the vicinity of Nishiyama and Kompirayama. The strength of the soil and the mineralogical property of the volcanic ash in 1978 and 2000 eruptions show considerable difference in the soil properties. Due to the difference in nature of eruption and high clay content in Nishiyama, it exhibited less shear strength than the soil from Ousu in 1978. The density of the soil near crater of Nishiyama is very low with high silt content. This clarifies the possibility of mass movement in various forms after the rainfall. Recalling the triggering of huge mass movement at mount Usu after 1978 eruption, the possible mass movement there in future can not be neglected, based on the low strength, existing land deformations and potential topography for slides. | |||||
| 書誌情報 |
新潟大学積雪地域災害研究センター研究年報 en : 新潟大学積雪地域災害研究センター研究年報 巻 23, p. 63-76, 発行日 2001-12 |
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| 出版者 | ||||||
| 出版者 | 新潟大学積雪地域災害研究センター | |||||
| ISSN | ||||||
| 収録物識別子タイプ | ISSN | |||||
| 収録物識別子 | 03877892 | |||||
| 書誌レコードID | ||||||
| 収録物識別子タイプ | NCID | |||||
| 収録物識別子 | AN00183327 | |||||
| 著者版フラグ | ||||||
| 値 | publisher | |||||
