@article{oai:repository.lib.tottori-u.ac.jp:00001226,
 author = {吉谷, 昭彦 and 中村, 治夫 and 山本, 恒久 and 大縄, 覺 and 八幡, 勇治 and 加藤, 光昭 and 安村, 節 and 住田, 享啓 and Yoshitani, Akihiko and Nakamura, Haruo and Yamamoto, Tsunehisa and Oonawa, Satoru and Yahata, Yuji and Katoh, Mitsuaki and Yasumura, Misao and Sumita, Akihiro},
 issue = {2},
 journal = {鳥取大学教育学部研究報告. 自然科学, The Journal of the Faculty of Education, Tottori University. Natural science},
 month = {Sep},
 note = {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.},
 pages = {91--103},
 title = {平野部に分布する完新統と河川堤外伏流水の水質との関係について : 鳥取県の主要河川,日野川および千代川の堤外取水を例として},
 volume = {47},
 year = {1998},
 yomi = {ヨシタニ, アキヒコ and ヨシタニ, アキヒコ}
}