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  1. 070 農学部, 大学院農学研究科
  2. 0702 紀要 ・刊行物
  3. 07024 信州大学農学部学術報告
  4. Vol. 6

山地荒廃の土質的研究:第3報 長野県における山地荒廃の場合

http://hdl.handle.net/10091/13931
http://hdl.handle.net/10091/13931
5c19fb6f-68ad-46a8-bedf-1debb5376553
名前 / ファイル ライセンス アクション
Bulletin_Agri-06-02.pdf Bulletin_Agri-06-02.pdf (1.0 MB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2012-03-07
タイトル
言語 ja
タイトル 山地荒廃の土質的研究:第3報 長野県における山地荒廃の場合
タイトル
言語 en
タイトル Studies on the Soil Mechanics of Denuded Forest Lands: Part Ⅲ. On the Soils of Nagano Districts
言語
言語 jpn
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ departmental bulletin paper
著者 辰野, 良秋

× 辰野, 良秋

WEKO 34935

辰野, 良秋

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堀内, 照夫

× 堀内, 照夫

WEKO 34936

堀内, 照夫

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出版者
出版者 信州大学農学部
引用
内容記述タイプ Other
内容記述 信州大学農学部学術報告 6: 15-30(1958)
書誌情報 信州大学農学部学術報告

巻 6, p. 15-30, 発行日 1958-08-25
抄録
内容記述タイプ Abstract
内容記述 Since the denuded lands are under influence of geology, soil mechanics, topography and climate, they must be investigated from various points of view. This paper presents detailed discussion on the soil mechanics of the denuded lands, especially on the lands in Nagano districts. From the observations and experimental facts we obtained the forms of the denuded lands in Nagano districts may be summarised as follws: 1) The land-creeps and disintegrations are observed in the crushed-zones (Trummerzon) of crystalline. It was found that the former is of small scale from the geological and soil mechanical point of view, compared with that of tertiary, and the later was simillar with a land-creeps, on which more immense and unstable sands and soils are found than the other cases. It has been reported that when a disintegration occurs once in a place, the land slide in the some place is seldom found afterward. This specific characters are known as immunity. However, the secondary disasters attracted keenly our attention. 2) Since the soil mechanics of diluvial originate in the weatherings of granite are apt be eroded, the surface soils are eroded intensely. Then this erosion is found to grow into the gully erosion, and at last into the large disintegration. 3) When the soils of tertiary originate in the clay of the weatherings shale are dry, the resisting power aganinst the land-creepings and land-slidings are found to be large. On the other hand when they absorb moisture, the shearresists of the soils extremely lower. Namely the unstability against the land-creepings in this case was considered to be get liquidity. 4) The denuded lands of palaeozoic are observed to be settled in many cases without the hillside works. And moreover greening after settlement was recongnized to be related to the soil mechanics.
資源タイプ(コンテンツの種類)
内容記述タイプ Other
内容記述 Article
ISSN
収録物識別子タイプ ISSN
収録物識別子 0559-8605
書誌レコードID
収録物識別子タイプ NCID
収録物識別子 AN00121341
出版タイプ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
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