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  1. 060 工学部
  2. 0601 学術論文

Effect of groundwater flow on forming arsenic contaminated groundwater in Sonargaon, Bangladesh

http://hdl.handle.net/10091/16078
d7b0e9b9-2283-4afa-b2ff-6cf0271734e8
名前 / ファイル ライセンス アクション
Effect_groundwater_flow_forming_arsenic_contaminated2.pdf Effect_groundwater_flow_forming_arsenic_contaminated2.pdf (3.7 MB)
Item type 学術雑誌論文 / Journal Article(1)
公開日 2012-11-21
タイトル
言語 en
タイトル Effect of groundwater flow on forming arsenic contaminated groundwater in Sonargaon, Bangladesh
言語
言語 eng
キーワード
主題Scheme Other
主題 Arsenic
キーワード
主題Scheme Other
主題 Groundwater
キーワード
主題Scheme Other
主題 Flow path
キーワード
主題Scheme Other
主題 Contamination
キーワード
主題Scheme Other
主題 Bangladesh
キーワード
主題Scheme Other
主題 Hotspots
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ journal article
著者 Nakaya, Shinji

× Nakaya, Shinji

WEKO 37710

Nakaya, Shinji

Search repository
Natsume, Haruyasu

× Natsume, Haruyasu

WEKO 37711

Natsume, Haruyasu

Search repository
Masuda, Harue

× Masuda, Harue

WEKO 37712

Masuda, Harue

Search repository
Mitamura, Muneki

× Mitamura, Muneki

WEKO 37713

Mitamura, Muneki

Search repository
Biswas, Dipak Kumar

× Biswas, Dipak Kumar

WEKO 37714

Biswas, Dipak Kumar

Search repository
Seddique, Ashraf A.

× Seddique, Ashraf A.

WEKO 37715

Seddique, Ashraf A.

Search repository
信州大学研究者総覧へのリンク
氏名 Nakaya, Shinji
URL http://soar-rd.shinshu-u.ac.jp/profile/ja.jCLabpkh.html
出版者
出版者 ELSEVIER SCIENCE BV
引用
内容記述タイプ Other
内容記述 JOURNAL OF HYDROLOGY. 409(3-4):724-736 (2011)
書誌情報 JOURNAL OF HYDROLOGY

巻 409, 号 3-4, p. 724-736, 発行日 2011-11-09
抄録
内容記述タイプ Abstract
内容記述 Three-dimensional groundwater flow in Sonargaon, Bangladesh is numerically simulated in order to evaluate the flow paths of As-contaminated drinking groundwater in the Holocene aquifer of the Ganges-Blamaptra-Meghna delta plain over a recent 30-year period. The model indicates that vertical infiltration of surface groundwater into the shallow Holocene aquifer occurs frequently in the Ganges-Blamaptra-Meghna delta plain. It predicts that the water recharged from ground surface moves approximately 10-20 m vertically downward beneath the flood plain, with a gradually increasing horizontal flow, toward the underlying Pleistocene middle mud layer (aquitard). The model also predicts that groundwaters containing highest As concentrations (>700 mu g/L) are formed on the vertical groundwater flow paths where surface water recharges the Holocene aquifer and not on the horizontal flow paths. Combining with the groundwater chemistry, reducing groundwater condition is not essential for the As-contaminated groundwater of the studied area in the Ganges delta plain.
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 0022-1694
書誌レコードID
収録物識別子タイプ NCID
収録物識別子 AA00699543
DOI
関連識別子
識別子タイプ DOI
関連識別子 https://doi.org/10.1016/j.jhydrol.2011.09.006
関連名称
関連名称 10.1016/j.jhydrol.2011.09.006
出版タイプ
出版タイプ AM
出版タイプResource http://purl.org/coar/version/c_ab4af688f83e57aa
WoS
表示名 Web of Science
URL http://gateway.isiknowledge.com/gateway/Gateway.cgi?&GWVersion=2&SrcAuth=ShinshuUniv&SrcApp=ShinshuUniv&DestLinkType=FullRecord&DestApp=WOS&KeyUT=000296949600011
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