{"_buckets": {"deposit": "bd2e836d-41c1-47c5-a729-5eb38a22d520"}, "_deposit": {"id": "5730", "owners": [1], "pid": {"revision_id": 0, "type": "depid", "value": "5730"}, "status": "published"}, "_oai": {"id": "oai:nied-repo.bosai.go.jp:00005730", "sets": []}, "author_link": [], "item_10001_biblio_info_7": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2012", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "61", "bibliographicPageEnd": "12", "bibliographicPageStart": "6", "bibliographicVolumeNumber": "53", "bibliographic_titles": [{"bibliographic_title": "ANNALS OF GLACIOLOGY", "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 the volumetric liquid water content, theta(v), and suction, h, is a fundamental part of the characterization of hydraulic properties. Therefore, the formulation of the WRC as a function of snow characteristics is essential for establishing a model of water movement through the snow cover. In this study, we measured the WRC of several snow samples, which had different characteristics (grain size, bulk dry density and grain type), using a gravity drainage column experiment and then analysed these data using the Van Genuchten soil physics model (VG model). The shape of the WRC depended strongly on both the sample grain size, d, and bulk dry density, rho. Therefore, we introduced the parameter rho/d to model the WRC of snow. The relationships between the parameters alpha and n of the VG model and rho/d change with grain type. For melt forms, alpha, which is related to the inverse value of the air-entry suction, increases quickly as rho/d decreases, whereas n, which is related to the gradient of theta(v) vs h, increases with rho/d. Conversely, neither of these parameters of the VG model for rounded grains showed obvious dependence on rho/d. These results suggest that water movement through snow cover can be modelled using grain size, bulk dry density and grain type based on the soil physics model.", "subitem_description_language": "en", "subitem_description_type": "Other"}]}, "item_10001_publisher_8": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "INT GLACIOL SOC", "subitem_publisher_language": "en"}]}, "item_10001_relation_14": {"attribute_name": "DOI", "attribute_value_mlt": [{"subitem_relation_type_id": {"subitem_relation_type_id_text": "10.3189/2012AoG61A001"}}]}, "item_10001_source_id_9": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "0260-3055", "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": "Kunio Watanabe", "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": "Dependence of the water retention curve of snow on snow characteristics", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "Dependence of the water retention curve of snow on snow characteristics", "subitem_title_language": "en"}]}, "item_type_id": "40001", "owner": "1", "path": ["1670839190650"], "permalink_uri": "https://nied-repo.bosai.go.jp/records/5730", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2023-03-30"}, "publish_date": "2023-03-30", "publish_status": "0", "recid": "5730", "relation": {}, "relation_version_is_last": true, "title": ["Dependence of the water retention curve of snow on snow characteristics"], "weko_shared_id": -1}