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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. 07025 信州大学農学部演習林報告
  4. Vol. 06

山腹工作物の凍害防止に関する研究 : 凍結破壊に関係する凍結土壌の性質について

http://hdl.handle.net/10091/13965
305fc378-952f-48b9-9aee-c8f7b2181e1f
名前 / ファイル ライセンス アクション
Agri_Forests-06-06.pdf Agri_Forests-06-06.pdf (939.1 kB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2012-03-07
タイトル
タイトル 山腹工作物の凍害防止に関する研究 : 凍結破壊に関係する凍結土壌の性質について
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
その他(別言語等)のタイトル
その他のタイトル On the Erosion Control Caused by Frost Heaving for Hillside works : About the Properties of frozen soil influence of damaging frost actions
その他(別言語等)のタイトル
その他のタイトル 山腹工作物の凍害防止に関する研究 : 凍結破坏に関係する凍結土壤の性質について
著者 辰野, 良秋

× 辰野, 良秋

WEKO 35240

辰野, 良秋

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堀内, 照夫

× 堀内, 照夫

WEKO 35241

堀内, 照夫

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出版者
出版者 信州大学農学部附属演習林
引用
内容記述タイプ Other
内容記述 信州大学農学部演習林報告 6: 79-98(1969)
書誌情報 信州大学農学部演習林報告

巻 6, p. 79-98, 発行日 1969-08-30
抄録
内容記述タイプ Abstract
内容記述 This paper is the observation on the relation between depth of frozen soil freezing and accumulative temperature, permeability, compressive strength of frozen soil. The results are summarized as follows; 1. Depth of frozen soil in southern shinshu. (1) Without influence of snow, depth of frozen soil (H) was proportion to a square root of accumulative temperature (U), and obtained following practical expression.〓 Here, U was the total of the mean temperature by the near weather station. (2) Generlly speaking, depth of frozen soil in the sunshine was a half of that in the shade. 2. Permeability of frozen soil. (1) Permeability of frozen soil was influenced by soil moisture content before freezing and its type was peculiar.〓 K: Coefficient of permeablity of unfrozen soil 3. Compressive strength of frozen soil. (1) Compressive strength of frozen soil was affected by nature of soils, and showed the highest strength when it was the largest density. In the case of soil variables, generally, increased with the effective soil texture, however, influence of strength of soil itself before freezing was very little. (2) Compressive strength of frozen soil was largely than one of ice itself on same degree and the ratio of the compressive strength was shown by function of the soil moisture content. (3) Compressive strength of frozen soil was not affect of accumulative temperature but increased with in proportion the lowest degree of temperature.
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 0559-8613
書誌レコードID
収録物識別子タイプ NCID
収録物識別子 AN00121330
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