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御坊市附近の地下水
http://hdl.handle.net/11266/00010590
http://hdl.handle.net/11266/00010590b30557dc-836f-4529-a0b2-80099e442750
名前 / ファイル | ライセンス | アクション |
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2022-02-22 | |||||
タイトル | ||||||
タイトル | 御坊市附近の地下水 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | On the Groundwater of Gobo City, Wakayama Prefecture | |||||
言語 | ||||||
言語 | jpn | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
資源タイプ | departmental bulletin paper | |||||
著者 |
角, 幸一
× 角, 幸一× 山本, 荘毅× SUMI, Koichi× YAMAMOTO, Soki |
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抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | The authors carried out the hydrographical study of the groundwater on and around the City of Gobo (御坊), Wakayama Prefecture, Japan. Non-confined water, probably no confinedwater will be expected, exists in the sand and gravel aquifer with 40 meters thickness underlain by Cretaceous shale and sandstone. About 30 dug wells are investigated on July, 1980. The results obtained are as follows : 1) Owing to the existence of remarkable groundwater ridge along the Kishu Railway line, groundwater flows to the west and to the east furnishing the River Hidaka. 2) The groundwater temperature varies from 18° to 25℃. Generally speaking, it is high on the groundwater ridge region. 3) The hydrogen ion concentration (pH) of groundwater ranges from 5.0 to 7.4. Except the coastal region, it shows weak acid on this area. 4) Distribution of conductivity of groundwater indicates sea water invasion into this area along sea coast and river mouth. | |||||
内容記述 | ||||||
内容記述 | 論説, ARTICLES | |||||
書誌情報 |
地域研究 en : REGIONAL STUDY 巻 23, 号 1, p. 1-6, 発行日 1982-06-01 |
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その他の巻号 | ||||||
35 | ||||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 03896641 | |||||
出版タイプ | ||||||
出版タイプ | VoR | |||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||
出版者 | ||||||
出版者 | 立正地理学会 |