| タイトル |
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平成15年8月出水における額平川の崩壊地とその要因について
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| その他のタイトル |
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RESEARCH ON SLOPE FAILURES INDUCED BY FLOOD IN AUGUST 2003 IN NUKABIRA RIVER AND ITS CAUSES
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| 作成者 |
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| 権利情報 |
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Copyright 2004 土木学会 ダウンロードを含むこの著作物の利用は、著作権法の私的使用及び引用の範囲に限り認められます。その範囲外の利用については、土木学会 の承諾が必要です。
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| 主題 |
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Other
Slope failure
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Other
drift wood
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Other
sediment
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Other
geology
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Other
hourly rainfall
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NDC
510
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| 内容注記 |
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Other
A heavy rainfall caused by a stationary front vitalized from season’s 10th typhoon occurred in southeastern part of Hokkaido Japan on August 8 to 10, 2003. The 48 hour total rainfall at the Biratori observation point catchments recorded 306.2mm was largest in the last 41 years. During the event, huge amount of sediment and drift wood has been provided from the upstream of Nukabira river basin. Based on field investigation and remote sensing data analysis after the event, and also analysis of contributing factor of slope failure such as rainfall amount, slope angle, vegetation and geological conditions, it was made clear that 1) the slope failure area were increased by about 3.6 times that off 2002; 2) the slope failure event strong related with hourly rainfall.
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| 出版者 |
土木学会
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| 日付 |
Created2016-02-15
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Issued2004-06
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| 言語 |
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| 資源タイプ |
journal article |
| 出版タイプ |
VoR |
| 資源識別子 |
URI
http://hdl.handle.net/10258/1543
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| 関連 |
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isIdenticalTo
NCID
BA67519158
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isIdenticalTo
NAID
120004681077
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| 収録誌情報 |
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| ファイル |
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| コンテンツ更新日時 |
2021-04-13 |
