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  1. 040 理学部
  2. 0402 紀要
  3. 04021 Journal of the Faculty of Science, Shinshu University
  4. Vol. 14

火山島の地下水(その1) : 小火山島の簡単な水収支

http://hdl.handle.net/10091/10520
40af90eb-d00f-402b-a96f-d20d4326b318
名前 / ファイル ライセンス アクション
Science14-02-05.pdf Science14-02-05.pdf (395.6 kB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2010-10-06
タイトル
タイトル 火山島の地下水(その1) : 小火山島の簡単な水収支
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
その他(別言語等)のタイトル
その他のタイトル Ground Water Flow in the Volcanic Island (NO. 1) : Simple method for the calculation of ground water balance in the example of small volcanic island
著者 熊井, 久雄

× 熊井, 久雄

WEKO 37174

熊井, 久雄

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工藤, 浩

× 工藤, 浩

WEKO 37175

工藤, 浩

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出版者
出版者 信州大学理学部
引用
内容記述タイプ Other
内容記述 信州大学理学部紀要 14(2): 107-115(1980)
書誌情報 信州大学理学部紀要

巻 14, 号 2, p. 107-115, 発行日 1980-03-28
抄録
内容記述タイプ Abstract
内容記述 Ground water balance of Toshima, Izu Island, have been studied as the type of small volcanic island. For the calculation of the ground water balance, this island was modelled as follows. a) This island is modelled as conical island which is consisted of homogeneous aquifer on the geologic and topographic aspects. b) It is assumed that the ground water flow tended radial from the center of the island to the coast. At this model, ground water table level is assumed from the level of salinity water surface which is sounded by the electoric survey. And then, the function is established for the calculation of the ground water balance of this island as follows. Lr2+2Kh2=C L:recharge volume from ground surface r:radius from center of island K:coefficient of permiability h:gound water table high from sea level C:integration constant Through this calculation, it is concluded that the total volume of ground water flow of this island is about 14,000m3/day. In this process, the coefficient of permiability of the aquifer is calculated as 1.66×10{ 3m/sec.
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 0583-063X
書誌レコードID
収録物識別子タイプ NCID
収録物識別子 AA00697923
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