当サイトでは、より良いサービスを提供するため、クッキーを利用しています。クッキーの使用に同意いただける場合は「同意」ボタンをクリックし、クッキーポリシーについては「詳細を見る」をクリックしてください。詳しくは当サイトの サイトポリシー をご確認ください。

詳細を見る...
ログイン サインアップ
言語:

WEKO3

  • トップ
  • ランキング
To

Field does not validate



インデックスリンク

インデックスツリー

  • RootNode

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": "611d724d-2ef6-47b3-8c44-7296c6a2be1b"}, "_deposit": {"id": "4243", "owners": [1], "pid": {"revision_id": 0, "type": "depid", "value": "4243"}, "status": "published"}, "_oai": {"id": "oai:nied-repo.bosai.go.jp:00004243", "sets": []}, "author_link": [], "item_10001_biblio_info_7": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2010-11"}, "bibliographicIssueNumber": "2", "bibliographicPageEnd": "93", "bibliographicPageStart": "87", "bibliographicVolumeNumber": "64", "bibliographic_titles": [{"bibliographic_title": "COLD REGIONS SCIENCE AND TECHNOLOGY", "bibliographic_titleLang": "en"}]}]}, "item_10001_description_5": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "The water retention curve (WRC), which shows the relationship between volumetric water content (Or) and suction (h), is fundamental for characterizing hydraulic properties. Thus, to model water movement through the snow cover, a formulation for the WRC as a function of snow characteristics must be established. In order to examine the dependence of the WRC on the grain size of snow, we measured the WRCs of snow (550 kg m(-3)) of various grain sizes in gravity drainage column experiments. Our experiments revealed many similarities between the WRCs of snow and sand. Thus, we applied two soil physics models, the Brooks and Corey model (BC model) and the van Genuchten model (VG model), which are standard models in soil physics to analyze the WRC of snow. Two parameters in both models that affected the shape of the WRC had a strong relationship with sample grain size. The parameter related to the value of the reverse of air entry suction increased with an increase in grain size, whereas the parameter related to the gradient of theta(v) versus h (d theta(v)/dh) decreased with an increase in grain size. From these results, we obtained linear equations between those two parameters and grain size. Our results suggest that the WRC of snow can be described as a function of grain size using soil physics models. (C) 2010 Elsevier B.V. All rights reserved.", "subitem_description_language": "en", "subitem_description_type": "Other"}]}, "item_10001_publisher_8": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "ELSEVIER SCIENCE BV", "subitem_publisher_language": "en"}]}, "item_10001_relation_14": {"attribute_name": "DOI", "attribute_value_mlt": [{"subitem_relation_type_id": {"subitem_relation_type_id_text": "10.1016/j.coldregions.2010.05.008"}}]}, "item_10001_source_id_9": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "0165-232X", "subitem_source_identifier_type": "ISSN"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "Satoru Yamaguchi", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Takafumi Katsushima", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Atsushi Sato", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Toshiro Kumakura", "creatorNameLang": "en"}]}]}, "item_language": {"attribute_name": "言語", "attribute_value_mlt": [{"subitem_language": "eng"}]}, "item_title": "Water retention curve of snow with different grain sizes", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "Water retention curve of snow with different grain sizes", "subitem_title_language": "en"}]}, "item_type_id": "40001", "owner": "1", "path": ["1670839190650"], "permalink_uri": "https://nied-repo.bosai.go.jp/records/4243", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2023-03-30"}, "publish_date": "2023-03-30", "publish_status": "0", "recid": "4243", "relation": {}, "relation_version_is_last": true, "title": ["Water retention curve of snow with different grain sizes"], "weko_shared_id": -1}
  1. 防災科研関係論文

Water retention curve of snow with different grain sizes

https://nied-repo.bosai.go.jp/records/4243
https://nied-repo.bosai.go.jp/records/4243
01e1e755-2087-4775-a24d-57c1b7b2e0c2
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Water retention curve of snow with different grain sizes
言語
言語 eng
著者 Satoru Yamaguchi

× Satoru Yamaguchi

en Satoru Yamaguchi

Search repository
Takafumi Katsushima

× Takafumi Katsushima

en Takafumi Katsushima

Search repository
Atsushi Sato

× Atsushi Sato

en Atsushi Sato

Search repository
Toshiro Kumakura

× Toshiro Kumakura

en Toshiro Kumakura

Search repository
抄録
内容記述タイプ Other
内容記述 The water retention curve (WRC), which shows the relationship between volumetric water content (Or) and suction (h), is fundamental for characterizing hydraulic properties. Thus, to model water movement through the snow cover, a formulation for the WRC as a function of snow characteristics must be established. In order to examine the dependence of the WRC on the grain size of snow, we measured the WRCs of snow (550 kg m(-3)) of various grain sizes in gravity drainage column experiments. Our experiments revealed many similarities between the WRCs of snow and sand. Thus, we applied two soil physics models, the Brooks and Corey model (BC model) and the van Genuchten model (VG model), which are standard models in soil physics to analyze the WRC of snow. Two parameters in both models that affected the shape of the WRC had a strong relationship with sample grain size. The parameter related to the value of the reverse of air entry suction increased with an increase in grain size, whereas the parameter related to the gradient of theta(v) versus h (d theta(v)/dh) decreased with an increase in grain size. From these results, we obtained linear equations between those two parameters and grain size. Our results suggest that the WRC of snow can be described as a function of grain size using soil physics models. (C) 2010 Elsevier B.V. All rights reserved.
言語 en
書誌情報 en : COLD REGIONS SCIENCE AND TECHNOLOGY

巻 64, 号 2, p. 87-93
出版者
言語 en
出版者 ELSEVIER SCIENCE BV
ISSN
収録物識別子タイプ ISSN
収録物識別子 0165-232X
DOI
関連識別子 10.1016/j.coldregions.2010.05.008
戻る
0
views
See details
Views

Versions

Ver.1 2023-03-31 01:48:27.199113
Show All versions

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

Change consent settings


Powered by WEKO3

Change consent settings