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
Authors
Nakamura, Haruo
Yamamoto, Tsunehisa
Oonawa, Satoru
Yahata, Yuji
Katoh, Mitsuaki
Yasumura, Misao
Sumita, Akihiro
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.
Publisher
鳥取大学教育学部
Content Type
Departmental Bulletin Paper
ISSN
03715965
NCID
AN00174585
Journal Title
鳥取大学教育学部研究報告. 自然科学
Current Journal Title
The Journal of the Faculty of Education, Tottori University. Natural science
Volume
47
Issue
2
Start Page
91
End Page
103
Published Date
1998-09-10
Text Version
None
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.
Citation
鳥取大学教育学部研究報告. 自然科学. 1998. 47(2), 91-103.
Department
Faculty of Regional Sciences/Graduate School of Regional Sciences
Language
Japanese