Bibliographic Information
- Other Title
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- ナラシ フキン ニ オケル カコウガンルイ シュウヘン ノ チカスイ オヨビ シンセイダイソウ チュウ ノ ウラン ニ ツイテ
- On the Geochemistry of Uranium in Groundwater and the Cenozoic Strata around Granite Batholith at Nara City
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Abstract
This paper is to describe about the geochemical cycle of uranium in the bed rock, the Cenozoic strata and groundwater. Uraium contained in granite is easily oxided and dissolved into circulating water. Therefore, groundwater contains uranium of 1 to 2 ppb at Jigokudani and Tawara basins, the eastern part of Nara City where the Pliocene rests on granite. Then, at the southern alluvial plain of the city, the uranium contents of groundwater being almost 2 ppb at the east granite zone gradually decrease to be less than 1 ppb as groundwater moves to west downstream. The Cenozoic strata around granite such as Jigokudani and Saho formations contain uranium of less than 2 ppm by absorption from circulating water. The capturing behaviors of clay, humus and limonite which construct every stratum seem to be concordant with those examined in laboratory.
Journal
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- 奈良学芸大学紀要. 自然科学
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奈良学芸大学紀要. 自然科学 10 (2), 121-128, 1962-03-26
奈良学芸大学
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Details 詳細情報について
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- CRID
- 1050564287514798336
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- NII Article ID
- 120002674096
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- NII Book ID
- AN00181015
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- ISSN
- 03693937
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- NDL BIB ID
- 9139217
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- Text Lang
- ja
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- Article Type
- departmental bulletin paper
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- Data Source
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- IRDB
- NDL
- CiNii Articles