Geologic structure and geochemical characteristics of sediments of fluoride and arsenic contaminated groundwater aquifer in Kalalanwala and its vicinity, Punjab, Pakistan
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- MASUDA HARUE
- Department of Geosciences, Osaka City University
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- MITAMURA MUNEKI
- Department of Geosciences, Osaka City University
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- FAROOQI ABIDA M.
- Department of Geosciences, Osaka City University
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- MUHANMAD NASIIM
- Geoscience Laboratory, Geological Survey of Pakistan
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- OWADA MASAFUMI
- Department of Geosciences, Osaka City University
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- OKAZAKI KAORI
- Department of Geosciences, Osaka City University
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- SEDDIQUE ASHRAF ALI
- Department of Geosciences, Osaka City University
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To constrain the origin of fluoride and arsenic contamination of groundwater in Kalalanwala, Punjab, Pakistan, the geochemical and mineralogical characteristics of the aquifer were studied. Subsurface geology of the area was studied using data from drilled cores. The residential and industrial areas including Kalalanwala are covered with Pleistocene aeolian deposits. These sediments cover two aquifers intercalated by a less permeable layer. Most polluted groundwater appears in the first aquifer at 15 to 25 m depth beneath the center of the village of Kalalanwala. A considerable amount of anthropogenic fluoride contaminates the aquifer along an ancient river channel. Arsenic might derive from anthropogenic sources such as industrial waste, or detrital chlorite.
収録刊行物
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- GEOCHEMICAL JOURNAL
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GEOCHEMICAL JOURNAL 44 (6), 489-505, 2010
一般社団法人日本地球化学会
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詳細情報 詳細情報について
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- CRID
- 1390001204552991872
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- NII論文ID
- 10027720006
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- NII書誌ID
- AA00654975
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- COI
- 1:CAS:528:DC%2BC3MXjtFahsro%3D
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- ISSN
- 18805973
- 00167002
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- NDL書誌ID
- 10936302
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- 本文言語コード
- en
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- データソース種別
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- JaLC
- NDL
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- 使用不可