| Title Transcription | ヘイヤ ブ ニ ブンプ スル カンシントウ ト カセン テイガイ フクリュウスイ ノ スイシツ トノ カンケイ ニツイテ : トットリケン ノ シュヨウカセン, ヒノガワ オヨビ チヨガワ ノ テイガイ シュスイ オ レイトシテ
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| Authors |
Nakamura, Haruo
Yamamoto, Tsunehisa
Oonawa, Satoru
Yahata, Yuji
Katoh, Mitsuaki
Yasumura, Misao
Sumita, Akihiro
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| Abstract | We find an increasing demand for city water with the developments of social community and industry. It is possible that water resources can be obtained from fissure-structures in basements, and also from Alluvium and Diluvium strata. In the case that water resources are pumped up from Alluvial strata, we have sometimes perplexed problems as for the chemical properties of ground surface water with large contents of Fe2+, Mn3+ and so on. These phenomena will be owed to the existence of clay beds in reduced state. In this paper, the relationships between Alluvial clay beds and the chemical properties of groundsurface water in rivers will be discussed.
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| Publisher | 鳥取大学教育学部
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| Content Type |
Departmental Bulletin Paper
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| ISSN | 03715965
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| NCID | AN00174585
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| Journal Title | 鳥取大学教育学部研究報告. 自然科学
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| Current Journal Title |
The Journal of the Faculty of Education, Tottori University. Natural science
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| Volume | 47
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| Issue | 2
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| Start Page | 91
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| End Page | 103
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| Published Date | 1998-09-10
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| Text Version |
None
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| Rights | 注があるものを除き、この著作物は日本国著作権法により保護されています。 / This work is protected under Japanese Copyright Law unless otherwise noted.
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| Citation | 鳥取大学教育学部研究報告. 自然科学. 1998. 47(2), 91-103.
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| Department |
Faculty of Regional Sciences/Graduate School of Regional Sciences
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| Language |
Japanese
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