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  1. B300 農学部/生命農学研究科
  2. B300b 紀要
  3. 名古屋大学農学部演習林報告
  4. 9

Slope failure in the rectilinear zone of hillsides

https://doi.org/10.18999/bulnuf.9.22
https://doi.org/10.18999/bulnuf.9.22
3edcd15a-c779-48f1-8bc6-81092d850ca1
名前 / ファイル ライセンス アクション
bulnuf_9_22.pdf bulnuf_9_22.pdf (1.1 MB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2007-08-15
タイトル
タイトル Slope failure in the rectilinear zone of hillsides
言語 en
その他のタイトル
その他のタイトル 傾斜変換帯における崩壊
言語 ja
著者 TAKEDA, Yasuo

× TAKEDA, Yasuo

WEKO 18761

en TAKEDA, Yasuo

Search repository
竹田, 泰雄

× 竹田, 泰雄

WEKO 18762

ja 竹田, 泰雄

Search repository
KATAOKA, Jun

× KATAOKA, Jun

WEKO 18763

en KATAOKA, Jun

Search repository
片岡, 順

× 片岡, 順

WEKO 18764

ja 片岡, 順

Search repository
IIDA, Osamu

× IIDA, Osamu

WEKO 18765

en IIDA, Osamu

Search repository
飯田, 修

× 飯田, 修

WEKO 18766

ja 飯田, 修

Search repository
TANAKA, Tanafumi

× TANAKA, Tanafumi

WEKO 18767

en TANAKA, Tanafumi

Search repository
田中, 隆文

× 田中, 隆文

WEKO 18768

ja 田中, 隆文

Search repository
アクセス権
アクセス権 open access
アクセス権URI http://purl.org/coar/access_right/c_abf2
キーワード
主題Scheme Other
主題 Slope failure
キーワード
主題Scheme Other
主題 Rectilinear zone of slope
キーワード
主題Scheme Other
主題 Morphometry
キーワード
主題Scheme Other
主題 Depth of surface soil layer
抄録
内容記述 地形解析により斜面を傾斜変換帯とそれ以外の地域に分け、それぞれの地域における崩壊発生頻度、崩壊面積、上部変換線から崩壊発生位置までの距離について検討した。その結果、傾斜変換帯の上部地域に崩壊が多発していることが明らかになった。また土壌の深さについては、崩壊地の上部で厚く、下部で薄くなっているが、崩壊地に近接する未崩壊斜面では逆の傾向がみられた。これらを総合して、表層土壌の深さの不均一さが、傾斜変換帯上部における浸透水の集中と崩壊の発生に密接に関係していると考えられた。従って、傾斜変換帯あるいは上部傾斜変換線は、山地における崩壊危険地帯予知の1つの有用な指標になりうると判断された。
言語 ja
内容記述タイプ Abstract
抄録
内容記述 The mountain slope was divided into two parts, the rectilinear zone and curvilinear zone (the convex or concave zone) by analyzing topographical maps. The frequency and size of slope failure and its position from the upper inflection contour line were studied in regard with the rectilinear or curvilinear zone of the mountain slope. It was then made clear that many slope failures were distributed in the upper part of the rectilinear zone of slope. The measurement of soil condition showed that the surface soil layer was generally deep at the upper part of slope failure and was shallow at the lower part. On the other hand, the depth of the surface soil on nearby nonfailed slopes was quite reverse to the above mentioned situation. From these analyses, it was concluded that the disproportion in the depth of the surface soil layer was closely related to the concentration of infiltrated water and the occurrence of slope failures at the upper part of the rectilinear zone of slope. The rectilinear zone of slope or the upper inflection contour line could probably be a very useful index for predicting the dangerous area of slope failure occurrence in the mountain.
言語 en
内容記述タイプ Abstract
内容記述
内容記述 農林水産研究情報センターで作成したPDFファイルを使用している。
言語 ja
内容記述タイプ Other
出版者
言語 ja
出版者 名古屋大学農学部付属演習林
言語
言語 eng
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ departmental bulletin paper
出版タイプ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
ID登録
ID登録 10.18999/bulnuf.9.22
ID登録タイプ JaLC
関連情報
関連タイプ isVersionOf
識別子タイプ URI
関連識別子 http://rms1.agsearch.agropedia.affrc.go.jp/contents/JASI/pdf/academy/40-2641.pdf
ISSN(print)
収録物識別子タイプ PISSN
収録物識別子 0469-4708
書誌情報 ja : 名古屋大学農学部演習林報告

巻 9, p. 22-31, 発行日 1987-03
フォーマット
application/pdf
著者版フラグ
値 publisher
URI
識別子 http://hdl.handle.net/2237/8663
識別子タイプ HDL
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