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姫川水系浦川流域における斜面崩壊と土石流について : その2
http://hdl.handle.net/10191/39028
http://hdl.handle.net/10191/3902801547579-386e-4a39-85a2-189a8a9864b4
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 | 2016-03-03 | |||||
タイトル | ||||||
タイトル | 姫川水系浦川流域における斜面崩壊と土石流について : その2 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | 姫川水系浦川流域における斜面崩壊と土石流について : その2 | |||||
言語 | ||||||
言語 | jpn | |||||
資源タイプ | ||||||
資源 | http://purl.org/coar/resource_type/c_6501 | |||||
タイプ | departmental bulletin paper | |||||
その他のタイトル | ||||||
その他のタイトル | Geological and geochemcical studies on the slope failures and debris flows in the Ura river basin, Nagano Prefecture : part 2 | |||||
著者 |
青木, 滋
× 青木, 滋× 佐藤, 修× 藤田, 至則× 茅原, 一也× 霜鳥, 重雄× 小田島, 一久× 松沢, 伸× 鈴木, 幸治 |
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著者別名 | ||||||
識別子 | 161992 | |||||
識別子Scheme | WEKO | |||||
姓名 | Aoki, Shigeru | |||||
著者別名 | ||||||
識別子 | 161993 | |||||
識別子Scheme | WEKO | |||||
姓名 | Sato, Osamu | |||||
著者別名 | ||||||
識別子 | 161994 | |||||
識別子Scheme | WEKO | |||||
姓名 | Fujita, Yukinori | |||||
著者別名 | ||||||
識別子 | 161995 | |||||
識別子Scheme | WEKO | |||||
姓名 | Chihara, Kazuya | |||||
著者別名 | ||||||
識別子 | 161996 | |||||
識別子Scheme | WEKO | |||||
姓名 | Shimotori, Shigeo | |||||
著者別名 | ||||||
識別子 | 161997 | |||||
識別子Scheme | WEKO | |||||
姓名 | Odajima, Kazuhisa | |||||
著者別名 | ||||||
識別子 | 161998 | |||||
識別子Scheme | WEKO | |||||
姓名 | Matsuzawa, Shin | |||||
著者別名 | ||||||
識別子 | 161999 | |||||
識別子Scheme | WEKO | |||||
姓名 | Suzuki, Koji | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | This second paper as continued first paper (AOKI et al 1982) deals with the results of research in the Ura river basin carried out in1981. The results can be summarized as follows: 1. Pyroclastic deposits exposed along the Kanayama river were hitherto recorded as the sliding mass from mt. Hieda in 1912. From our studies, these deposits are not the sliding mass but are the lowerest part of the andesite group exposed at the cliff of mt. Hieda, (Fig. 1) 2. From the water content and consistency of soils, three types of soil can be recognized in this area. The soil of sliding mass occurred in 1981 (Fig. 10 and Photos 11~16) belongs to the A-type as shown in Fig. 3. 3. From the chemical analyses of spring water, the servyed area is divided into 9 zones as shown in Fig. 6. 4. During about 50 days in 1981, we could observe several debris flows by T.Ⅴ. as shown in Fig. 7, Table. 2 and Phot. 1. The observed data clearly shows the interrelation between the features of rain fall and occurrence of debris flows (Figs. 8 and 9.) 5. In 1981, abnormal change of patterns of electrolyte of river water was observed during rain fall or before occurrence of debris flows as shown in Fig. 11 to 16. | |||||
書誌情報 |
新潟大学積雪地域災害研究センター研究年報 en : 新潟大学積雪地域災害研究センター研究年報 巻 5, p. 1-32, 発行日 1984-01 |
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出版者 | ||||||
出版者 | 新潟大学積雪地域災害研究センター | |||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 03877892 | |||||
書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00183327 | |||||
著者版フラグ | ||||||
値 | publisher |