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六甲山系の侵食環境の変遷と池沼堆積物: 兵庫県南部地震による環境変化に関連した予察的検討
https://doi.org/10.24517/00053733
https://doi.org/10.24517/00053733ee21c6fc-9d97-4622-9001-57bde572d9f6
名前 / ファイル | ライセンス | アクション |
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SC-PR-KASHIWAYA-K-263.pdf (1.0 MB)
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Item type | 学術雑誌論文 / Journal Article(1) | |||||
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公開日 | 2021-07-19 | |||||
タイトル | ||||||
タイトル | 六甲山系の侵食環境の変遷と池沼堆積物: 兵庫県南部地震による環境変化に関連した予察的検討 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Changes in Erosional Environment and Pond Sedimentation in the Rokko Mountains, Kobe, Japan-a Preliminary Discussion on Environmental Change due to the Kobe Earthquake, 1995 | |||||
言語 | ||||||
言語 | jpn | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
資源タイプ | journal article | |||||
ID登録 | ||||||
ID登録 | 10.24517/00053733 | |||||
ID登録タイプ | JaLC | |||||
著者 |
柏谷, 健二
× 柏谷, 健二× 沖村, 孝× 八藤, 仁美 |
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著者別表示 |
Kashiwaya, Kenji
× Kashiwaya, Kenji× Okimura, Takashi× Yatsufuji, Hitomi |
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提供者所属 | ||||||
内容記述タイプ | Other | |||||
内容記述 | 金沢大学環日本海域環境研究センター | |||||
書誌情報 |
地形 en : Transactions, Japanese Geomorphological Union 巻 18, 号 3, p. 263-275, 発行日 1997-07-25 |
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ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 0389-1755 | |||||
NCID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00333248 | |||||
出版者 | ||||||
出版者 | 日本地形学連合 = Japanese Geomorphological Union | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | Changes in hydro-erosinal environment and pond sedimentation during past 100 years in Kobe district are discussed with precipitational data and pond sediment information. Analyses of precipitational data show that the years when erosional phenomena, such as landslides, debris flows etc., happened were related to excess amount of critical daily rainfall (annual summation of exess amount over 100 mm/day and 50 mm/day). There are some dominant periods (80, 25, 15, 10 and 7 years) in the excess rainfall datasets. Analyses of physical properties of core samples from the two ponds in the Rokko Mountains show that there are rapid coarsening in the heavy rainfall times, especially in 1967 when severe natural disaster happened due to landslides, debris flows and floods. Comparing the sedimentation rate before the Kobe earthquake inferred from the core sample from Kawauso-ike on after the earthquake from sediment traps in the same pond shows significant increase in the rate after the earthquake. |
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権利 | ||||||
権利情報 | Copyright © 日本地形学連合 Japanese Geomorphological Union | |||||
著者版フラグ | ||||||
出版タイプ | VoR | |||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||
関連URI | ||||||
識別子タイプ | URI | |||||
関連識別子 | http://ci.nii.ac.jp/naid/10002187787/ | |||||
関連名称 | http://ci.nii.ac.jp/naid/10002187787/ | |||||
関連URI | ||||||
識別子タイプ | URI | |||||
関連識別子 | https://sites.google.com/site/japangeomorphologicalunion/tjguarchive | |||||
関連名称 | https://sites.google.com/site/japangeomorphologicalunion/tjguarchive | |||||
関連URI | ||||||
識別子タイプ | URI | |||||
関連識別子 | http://www.jgu.jp/ | |||||
関連名称 | http://www.jgu.jp/ |