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  1. 0 資料タイプ別
  2. 03 紀要論文
  1. 360 災害・復興科学研究所
  2. 20 紀要
  3. 90 新潟大学積雪地域災害研究センター研究年報
  4. 第21号

新潟県五頭山西麓の湧水と水文地質構造について

http://hdl.handle.net/10191/39205
http://hdl.handle.net/10191/39205
9d9ddb68-9f50-41f0-840e-a7e574f21cd3
名前 / ファイル ライセンス アクション
21_96-107.pdf 21_96-107.pdf (617.6 kB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2016-03-08
タイトル
タイトル 新潟県五頭山西麓の湧水と水文地質構造について
タイトル
言語 en
タイトル 新潟県五頭山西麓の湧水と水文地質構造について
言語
言語 jpn
キーワード
主題Scheme Other
主題 the Gozu mountain
キーワード
主題Scheme Other
主題 Oxygen isotope
キーワード
主題Scheme Other
主題 fault fracture zone
キーワード
主題Scheme Other
主題 hydrogeology
キーワード
主題Scheme Other
主題 groundwater
キーワード
主題Scheme Other
主題 spring water
キーワード
主題Scheme Other
主題 hydrochemistry
キーワード
主題Scheme Other
主題 五頭山
キーワード
主題Scheme Other
主題 酸素同位体
キーワード
主題Scheme Other
主題 断層破砕帯
キーワード
主題Scheme Other
主題 水文地質
キーワード
主題Scheme Other
主題 地下水
キーワード
主題Scheme Other
主題 湧水
キーワード
主題Scheme Other
主題 水質
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ departmental bulletin paper
その他のタイトル
その他のタイトル Hydrogeology and hydrochemistry of spring waters from the western slope of the Gozu mountain in Niigata Prefecture
著者 中川, 勉

× 中川, 勉

WEKO 161030

中川, 勉

Search repository
渡部, 直喜

× 渡部, 直喜

WEKO 161031

渡部, 直喜

Search repository
柚原, 雅樹

× 柚原, 雅樹

WEKO 161032

柚原, 雅樹

Search repository
徐, 輝竜

× 徐, 輝竜

WEKO 161033

徐, 輝竜

Search repository
著者別名
識別子 161034
識別子Scheme WEKO
姓名 Nakagawa, Tsutomu
著者別名
識別子 161035
識別子Scheme WEKO
姓名 Watanabe, Naoki
著者別名
識別子 161036
識別子Scheme WEKO
姓名 Yuhara, Masaki
著者別名
識別子 161037
識別子Scheme WEKO
姓名 Xu, Huilong
抄録
内容記述タイプ Abstract
内容記述 Groundwater circulation was investigated by means of natural spring waters in the western slope of the Gozu mountain which is located in 20km east away from Niigata City and is composed of mainly Cretecious granitic rocks. There is a tectonic line of NNE-SSW direction along the western foot of this mountain. Over the 120 water samples were collected from the western slope of this mountain and surrounding area. We found Ca-HCO_3 type spring waters having higher concentration than other spring waters along similar elevation of 300 to 500 meters above sea level. δ^<18>O values of these Ca-HCO_3 type waters are lower than other waters in surroundings. Such lower values suggest that Ca-HCO_3 type waters are derived from the higher recharge area and are formed by dissolution of plagioclase during longer circulation than others. These indicate that Ca-HCO_3 type waters having lower δ^<18>O values are discharging along the fault fractures of NE-SW direction and are different from the circulation of other groundwaters.
書誌情報 新潟大学積雪地域災害研究センター研究年報
en : 新潟大学積雪地域災害研究センター研究年報

巻 21, p. 96-107, 発行日 2000-03
出版者
出版者 新潟大学積雪地域災害研究センター
ISSN
収録物識別子タイプ ISSN
収録物識別子 03877892
書誌レコードID
収録物識別子タイプ NCID
収録物識別子 AN00183327
著者版フラグ
値 publisher
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