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": "30919f70-fec9-437f-8353-f32563751ba9"}, "_deposit": {"id": "2006828", "owners": [1], "pid": {"revision_id": 0, "type": "depid", "value": "2006828"}, "status": "published"}, "_oai": {"id": "oai:u-ryukyu.repo.nii.ac.jp:02006828", "sets": ["1642837940585", "1642838406414"]}, "author_link": [], "item_1617186331708": {"attribute_name": "Title", "attribute_value_mlt": [{"subitem_1551255647225": "\u7409\u7403\u8af8\u5cf6\u306b\u7523\u3059\u308b\u540d\u7a2e\u77f3\u7070\u5ca9\u306e\u6bd4\u8f03", "subitem_1551255648112": "ja"}, {"subitem_1551255647225": "Studies on the Various Kinds of the Limestones in the Ryukyu Islands", "subitem_1551255648112": "en"}]}, "item_1617186419668": {"attribute_name": "Creator", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "\u517c\u5cf6, \u6e05", "creatorNameLang": "ja"}]}, {"creatorNames": [{"creatorName": "Kaneshima, Kiyoshi", "creatorNameLang": "en"}]}]}, "item_1617186476635": {"attribute_name": "Access Rights", "attribute_value_mlt": [{"subitem_1522299639480": "open access", "subitem_1600958577026": "http://purl.org/coar/access_right/c_abf2"}]}, "item_1617186626617": {"attribute_name": "Description", "attribute_value_mlt": [{"subitem_description": "The various limestones in the Ryukyu Islands were classified according to the formation circumstances of limestones into four groups, which are hard limestone, soft limestone, crystallized limestone, and coral. The physical and chemical characters of the various kinds of the limestone in the Ryukyu Islands were studied for the purpose of clarifying the original nature of a limestone. The major and minor components of the limestones, such as calcium,  magnesium, iron, aluminum, silica, phosphorus, manganese, sulfate, chlorine, and sodium, were analyzed, and also the specific gravity and particle size of the limestones were measured. The following results were obtained: 1. The contents of silica, iron, aluminum, and phosphorus in the various limestones decrease in the followillg sequence:hard limestone, soft limestone, crystallized limestone, coral. 2. There is a positive correlation between the amounts of iron+aluminum and silica in the three kinds of the limestones. The facts shown above suggest that these limestones contain much more iron aluminum silicate impurities than the coral does. 3. The difference of the magnesium contents between hard limestone and soft limestone can not be distinguished, Nevertheless,  hard limestone contains more amounts of magnesium than crystallized limestone does. 4. The manganese contents of the limestones decrease in the following sequence:Hard limestone, crystallized limestone, coral. There is no difference of the manganese contents between hard limestone and soft limestone. There is a positive relationship between the amounts of manganese and iron+aluminum in the limestones. 5. The sulfate contents of the limestones decrease in the following sequence: coral, soft limeston hard limeston crystallized limestone. The sulfate contents of the coral is O.57% on the average. 6. The chlorine contents of the various limestones vary from 0.0022 to 0.037% and decrease in the following sequence:coral, soft limestone, hard limestone, crystallized limestone. 7. The sodium contents of the limestones vary from 0.005 to 0.33% and decrease in the following sequence:coral, soft limestone, hard limestone crystallized limestone There is a positive relationship between the contents of sodium and chlorine in the limestones. There is no positive correlation between the amounts of chlorine and sulfate in the limestones. The facts shown above suggest that the chlorine enter as sodium chloride in the limestones. 8. The specific gravity of the various limestones vary from 2.35 to 2.80 and decrease in the following sequence: coral, crystallized limestone, hard limestone, soft limestone. 9. The results of X-ray diffraction methods indicate that the three kinds of the limestones consist of calcite structure, and the coral consists of aragonite or calcite structures.", "subitem_description_type": "Other"}, {"subitem_description": "\u7d00\u8981\u8ad6\u6587", "subitem_description_type": "Other"}]}, "item_1617186643794": {"attribute_name": "Publisher", "attribute_value_mlt": [{"subitem_1522300295150": "ja", "subitem_1522300316516": "\u7409\u7403\u5927\u5b66\u6587\u7406\u5b66\u90e8"}, {"subitem_1522300295150": "en", "subitem_1522300316516": "Arts and Science Division, University of the Ryukyus"}]}, "item_1617186702042": {"attribute_name": "Language", "attribute_value_mlt": [{"subitem_1551255818386": "jpn"}]}, "item_1617186783814": {"attribute_name": "Identifier", "attribute_value_mlt": [{"subitem_identifier_type": "HDL", "subitem_identifier_uri": "http://hdl.handle.net/20.500.12000/23027"}]}, "item_1617186920753": {"attribute_name": "Source Identifier", "attribute_value_mlt": [{"subitem_1522646500366": "ISSN", "subitem_1522646572813": "0557-577X"}, {"subitem_1522646500366": "NCID", "subitem_1522646572813": "AN0025080X"}]}, "item_1617186941041": {"attribute_name": "Source Title", "attribute_value_mlt": [{"subitem_1522650068558": "ja", "subitem_1522650091861": "\u7409\u7403\u5927\u5b66\u6587\u7406\u5b66\u90e8\u7d00\u8981 \u7406\u5b66\u7bc7"}]}, "item_1617187056579": {"attribute_name": "Bibliographic Information", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1965-06", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "8", "bibliographicPageEnd": "54", "bibliographicPageStart": "23"}]}, "item_1617258105262": {"attribute_name": "Resource Type", "attribute_value_mlt": [{"resourcetype": "departmental bulletin paper", "resourceuri": "http://purl.org/coar/resource_type/c_6501"}]}, "item_1617265215918": {"attribute_name": "Version Type", "attribute_value_mlt": [{"subitem_1522305645492": "VoR", "subitem_1600292170262": "http://purl.org/coar/version/c_970fb48d4fbd8a85"}]}, "item_1617605131499": {"attribute_name": "File", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_access", "download_preview_message": "", "file_order": 0, "filename": "No8p023.pdf", "future_date_message": "", "is_thumbnail": false, "mimetype": "", "size": 0, "url": {"objectType": "fulltext", "url": "https://u-ryukyu.repo.nii.ac.jp/record/2006828/files/No8p023.pdf"}, "version_id": "872b32b2-962b-4085-a4bb-008a73c56a33"}]}, "item_title": "\u7409\u7403\u8af8\u5cf6\u306b\u7523\u3059\u308b\u540d\u7a2e\u77f3\u7070\u5ca9\u306e\u6bd4\u8f03", "item_type_id": "15", "owner": "1", "path": ["1642837940585", "1642838406414"], "permalink_uri": "http://hdl.handle.net/20.500.12000/23027", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2012-02-03"}, "publish_date": "2012-02-03", "publish_status": "0", "recid": "2006828", "relation": {}, "relation_version_is_last": true, "title": ["\u7409\u7403\u8af8\u5cf6\u306b\u7523\u3059\u308b\u540d\u7a2e\u77f3\u7070\u5ca9\u306e\u6bd4\u8f03"], "weko_shared_id": -1}
  1. 紀要論文
  2. 琉球大学文理学部紀要 理学篇
  3. 8号
  1. 部局別インデックス
  2. 理学部

琉球諸島に産する名種石灰岩の比較

http://hdl.handle.net/20.500.12000/23027
http://hdl.handle.net/20.500.12000/23027
01aa8773-9bb5-44a1-ac35-c3127a1828b1
名前 / ファイル ライセンス アクション
No8p023.pdf No8p023.pdf
Item type デフォルトアイテムタイプ(フル)(1)
公開日 2012-02-03
タイトル
タイトル 琉球諸島に産する名種石灰岩の比較
言語 ja
作成者 兼島, 清

× 兼島, 清

ja 兼島, 清

Kaneshima, Kiyoshi

× Kaneshima, Kiyoshi

en Kaneshima, Kiyoshi

アクセス権
アクセス権 open access
アクセス権URI http://purl.org/coar/access_right/c_abf2
内容記述
内容記述タイプ Other
内容記述 The various limestones in the Ryukyu Islands were classified according to the formation circumstances of limestones into four groups, which are hard limestone, soft limestone, crystallized limestone, and coral. The physical and chemical characters of the various kinds of the limestone in the Ryukyu Islands were studied for the purpose of clarifying the original nature of a limestone. The major and minor components of the limestones, such as calcium, magnesium, iron, aluminum, silica, phosphorus, manganese, sulfate, chlorine, and sodium, were analyzed, and also the specific gravity and particle size of the limestones were measured. The following results were obtained: 1. The contents of silica, iron, aluminum, and phosphorus in the various limestones decrease in the followillg sequence:hard limestone, soft limestone, crystallized limestone, coral. 2. There is a positive correlation between the amounts of iron+aluminum and silica in the three kinds of the limestones. The facts shown above suggest that these limestones contain much more iron aluminum silicate impurities than the coral does. 3. The difference of the magnesium contents between hard limestone and soft limestone can not be distinguished, Nevertheless, hard limestone contains more amounts of magnesium than crystallized limestone does. 4. The manganese contents of the limestones decrease in the following sequence:Hard limestone, crystallized limestone, coral. There is no difference of the manganese contents between hard limestone and soft limestone. There is a positive relationship between the amounts of manganese and iron+aluminum in the limestones. 5. The sulfate contents of the limestones decrease in the following sequence: coral, soft limeston hard limeston crystallized limestone. The sulfate contents of the coral is O.57% on the average. 6. The chlorine contents of the various limestones vary from 0.0022 to 0.037% and decrease in the following sequence:coral, soft limestone, hard limestone, crystallized limestone. 7. The sodium contents of the limestones vary from 0.005 to 0.33% and decrease in the following sequence:coral, soft limestone, hard limestone crystallized limestone There is a positive relationship between the contents of sodium and chlorine in the limestones. There is no positive correlation between the amounts of chlorine and sulfate in the limestones. The facts shown above suggest that the chlorine enter as sodium chloride in the limestones. 8. The specific gravity of the various limestones vary from 2.35 to 2.80 and decrease in the following sequence: coral, crystallized limestone, hard limestone, soft limestone. 9. The results of X-ray diffraction methods indicate that the three kinds of the limestones consist of calcite structure, and the coral consists of aragonite or calcite structures.
内容記述タイプ Other
内容記述 紀要論文
出版者
言語 ja
出版者 琉球大学文理学部
言語
言語 jpn
資源タイプ
資源タイプ departmental bulletin paper
資源タイプ識別子 http://purl.org/coar/resource_type/c_6501
出版タイプ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
識別子
識別子 http://hdl.handle.net/20.500.12000/23027
識別子タイプ HDL
収録物識別子
収録物識別子タイプ ISSN
収録物識別子 0557-577X
収録物識別子タイプ NCID
収録物識別子 AN0025080X
収録物名
言語 ja
収録物名 琉球大学文理学部紀要 理学篇
書誌情報
号 8, p. 23-54, 発行日 1965-06
戻る
0
views
See details
Views

Versions

Ver.1 2022-01-28 01:53:16.258875
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

確認


Powered by WEKO3


Powered by WEKO3