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山地河川における河床幅と土砂堆積地の空間分布 : 天竜川支流山室川下流部の事例
http://hdl.handle.net/10091/922
8fc5c81c-72fd-4cd1-b596-9bf25708f6b3
| 名前 / ファイル | ライセンス | アクション | |
|---|---|---|---|
v39_02.pdf (734.2 kB)
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| Item type | 学術雑誌論文 / Journal Article(1) | |||||
|---|---|---|---|---|---|---|
| 公開日 | 2008-01-17 | |||||
| タイトル | ||||||
| タイトル | 山地河川における河床幅と土砂堆積地の空間分布 : 天竜川支流山室川下流部の事例 | |||||
| 言語 | ||||||
| 言語 | jpn | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | 山地河川 | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | 河床幅 | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | 段丘堆積物 | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | 河床堆積土砂量 | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | 年間土砂浸食速度 | |||||
| 資源タイプ | ||||||
| 資源 | http://purl.org/coar/resource_type/c_6501 | |||||
| タイプ | journal article | |||||
| その他（別言語等）のタイトル | ||||||
| その他のタイトル | The Spatial Distribution of Bankful Width and Sediment Deposit in Mountainous Stream : The Case of the Lower Yamamuro Creek, the Branch of Tenryu River, Nagano, Japan | |||||
| 著者 |
土屋, 貞夫
× 土屋, 貞夫× 宮崎, 敏孝 |
|||||
| 出版者 | ||||||
| 出版者 | 信州大学農学部 | |||||
| 引用 | ||||||
| 内容記述タイプ | Other | |||||
| 内容記述 | 信州大学農学部紀要. 39(1-2): 13-21 (2003) | |||||
| 書誌情報 |
信州大学農学部紀要 巻 39, 号 1-2, p. 13-21, 発行日 2003-03-03 |
|||||
| 抄録 | ||||||
| 内容記述タイプ | Abstract | |||||
| 内容記述 | 山岳渓流では河床幅の空間分布が出水時水位や土砂滞留現象の制限要因になっている。本論では，河床幅と土砂堆積地の時空間特性を両者の相互位置・土砂堆積量・土砂浸食量から明らかにすることを試みた。河床形状を測量結果と河岸段丘面に成立した天然生同齢林の解析結果から，調査区間の土砂堆積量を算出した。その結果，土砂堆積量は河床幅の周期変動と同期して増減しており，土砂堆積地は河床幅の広い河道拡幅区間に形成され，土砂堆積量も河床幅に依存していた。しかし，出水時に土砂を堆積させる潜在的可能性は，河床幅が急激に縮小する区間で高い傾向が得られた。河床幅が拡幅する区間と縮小する区間では，後者の土砂浸食速度が速い傾向が認められた。河道拡幅区間に形成された土砂堆積地は，下流側から浸食を受け，堆積土砂量を減少させていることが推察された。 | |||||
| 資源タイプ（コンテンツの種類） | ||||||
| 内容記述タイプ | Other | |||||
| 内容記述 | Article | |||||
| ISSN | ||||||
| 収録物識別子タイプ | ISSN | |||||
| 収録物識別子 | 0583-0621 | |||||
| 書誌レコードID | ||||||
| 収録物識別子タイプ | NCID | |||||
| 収録物識別子 | AN00121352 | |||||
