ログイン
言語:

WEKO3

  • トップ
  • ランキング
To
lat lon distance
To

Field does not validate



インデックスリンク

インデックスツリー

メールアドレスを入力してください。

WEKO

One fine body…

WEKO

One fine body…

アイテム

{"_buckets": {"deposit": "6c3ac3b8-a1ba-4c76-a3e0-f4f6c32923d0"}, "_deposit": {"id": "11302", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "11302"}, "status": "published"}, "_oai": {"id": "oai:soar-ir.repo.nii.ac.jp:00011302", "sets": ["1135"]}, "author_link": ["35240", "35241"], "control_number": "11302", "item_10_biblio_info_6": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1969-08-30", "bibliographicIssueDateType": "Issued"}, "bibliographicPageEnd": "98", "bibliographicPageStart": "79", "bibliographicVolumeNumber": "6", "bibliographic_titles": [{"bibliographic_title": "信州大学農学部演習林報告"}]}]}, "item_10_description_20": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "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.", "subitem_description_type": "Abstract"}]}, "item_10_description_30": {"attribute_name": "資源タイプ(コンテンツの種類)", "attribute_value_mlt": [{"subitem_description": "Article", "subitem_description_type": "Other"}]}, "item_10_description_5": {"attribute_name": "引用", "attribute_value_mlt": [{"subitem_description": "信州大学農学部演習林報告 6: 79-98(1969)", "subitem_description_type": "Other"}]}, "item_10_publisher_4": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "信州大学農学部附属演習林"}]}, "item_10_select_64": {"attribute_name": "著者版フラグ", "attribute_value_mlt": [{"subitem_select_item": "publisher"}]}, "item_10_source_id_35": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "0559-8613", "subitem_source_identifier_type": "ISSN"}]}, "item_10_source_id_39": {"attribute_name": "NII ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "0559-8613", "subitem_source_identifier_type": "ISSN"}]}, "item_10_source_id_40": {"attribute_name": "書誌レコードID", "attribute_value_mlt": [{"subitem_source_identifier": "AN00121330", "subitem_source_identifier_type": "NCID"}]}, "item_10_text_66": {"attribute_name": "sortkey", "attribute_value_mlt": [{"subitem_text_value": "06"}]}, "item_1627890569677": {"attribute_name": "出版タイプ", "attribute_value_mlt": [{"subitem_version_resource": "http://purl.org/coar/version/c_970fb48d4fbd8a85", "subitem_version_type": "VoR"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "辰野,  良秋"}], "nameIdentifiers": [{"nameIdentifier": "35240", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "堀内,  照夫"}], "nameIdentifiers": [{"nameIdentifier": "35241", "nameIdentifierScheme": "WEKO"}]}]}, "item_files": {"attribute_name": "ファイル情報", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_date", "date": [{"dateType": "Available", "dateValue": "2015-09-25"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "Agri_Forests-06-06.pdf", "filesize": [{"value": "939.1 kB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_free", "mimetype": "application/pdf", "size": 939100.0, "url": {"label": "Agri_Forests-06-06.pdf", "url": "https://soar-ir.repo.nii.ac.jp/record/11302/files/Agri_Forests-06-06.pdf"}, "version_id": "9a1974e5-854e-485d-9a2a-fd995366abdb"}]}, "item_language": {"attribute_name": "言語", "attribute_value_mlt": [{"subitem_language": "jpn"}]}, "item_resource_type": {"attribute_name": "資源タイプ", "attribute_value_mlt": [{"resourcetype": "departmental bulletin paper", "resourceuri": "http://purl.org/coar/resource_type/c_6501"}]}, "item_title": "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", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "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", "subitem_title_language": "ja"}, {"subitem_title": "On the Erosion Control Caused by Frost Heaving for Hillside works : About the Properties of frozen soil influence of damaging frost actions", "subitem_title_language": "en"}]}, "item_type_id": "10", "owner": "1", "path": ["1135"], "permalink_uri": "http://hdl.handle.net/10091/13965", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2012-03-07"}, "publish_date": "2012-03-07", "publish_status": "0", "recid": "11302", "relation": {}, "relation_version_is_last": true, "title": ["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"], "weko_shared_id": -1}
  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
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
言語 ja
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
タイトル
言語 en
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
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 35240

辰野, 良秋

Search repository
堀内, 照夫

× 堀内, 照夫

WEKO 35241

堀内, 照夫

Search repository
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
出版タイプ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
戻る
0
views
See details
Views

Versions

Ver.1 2021-03-01 11:52:57.459974
Show All versions

Share

Mendeley Twitter Facebook Print Addthis

Cite as

エクスポート

OAI-PMH
  • OAI-PMH JPCOAR
  • OAI-PMH DublinCore
  • OAI-PMH DDI
Other Formats
  • JSON
  • BIBTEX

Confirm


Powered by WEKO3


Powered by WEKO3