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斜面崩壊丘陵地における自然降雨下での土壌水分動態の把握
https://doi.org/10.24561/00016668
https://doi.org/10.24561/00016668c5010f72-4f9e-4ea4-8eda-8d76d807e045
名前 / ファイル | ライセンス | アクション |
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KY-AA11808968-03-30.pdf (264.4 kB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2009-05-21 | |||||
タイトル | ||||||
タイトル | 斜面崩壊丘陵地における自然降雨下での土壌水分動態の把握 | |||||
言語 | ||||||
言語 | jpn | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Soil Water Dynamics | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Field Monitoring | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Macropore | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Preferential Flow | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | hilly Soil | |||||
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 | |||||
ID登録 | ||||||
ID登録 | 10.24561/00016668 | |||||
ID登録タイプ | JaLC | |||||
タイトル(別言語) | ||||||
その他のタイトル | Soil Water Dynamics in a Hilly Soil on a Landslide Site under Natural Precipitation | |||||
著者 |
川本, 健
× 川本, 健 |
|||||
著者 ローマ字 | ||||||
Ken Kawamoto | ||||||
著者 所属 | ||||||
埼玉大学工学部建設工学科 | ||||||
著者 所属(別言語) | ||||||
Department of Civil and Environmental Engineering, Faculty of Engineering, Saitama University | ||||||
書誌情報 |
埼玉大学地域共同研究センター紀要 en : Report of Cooperative Research Center, Saitama University 巻 3, p. 79-84, 発行日 2003 |
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年月次 | ||||||
2002 | ||||||
出版者名 | ||||||
出版者 | 埼玉大学地域共同研究センター | |||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 13474758 | |||||
概要 | ||||||
内容記述タイプ | Other | |||||
内容記述 | Soil water content and water pressure were monitored in a test pit excavated in a forested hilly soil during Dec. 2001 to Nov. 2002. The present monitoring system worked well, and provided us useful information successively on soil water dynamics. Rapid drainage of rainwater occurs not only in a heavy rainfall but also in a small amount of rainfall, suggesting that preferential flow is generated as soon as a rainfall starts. This occurs because a soil matrix is fully saturated with water under the soil moisture condition throughout the monitoring period. Field-measured hydraulic conductivities are larger than those that are laboratory-measured. The reason is explained as follows: that macropores are well connected in macro-scale so that preferential flow paths are easily formed in the field. In a small sample, however, macropores are not fully connected to make preferential flow paths through them. | |||||
資源タイプ | ||||||
内容記述タイプ | Other | |||||
内容記述 | text | |||||
フォーマット | ||||||
内容記述タイプ | Other | |||||
内容記述 | application/pdf | |||||
作成日 | ||||||
日付 | 2009-06-18 | |||||
日付タイプ | Created | |||||
アイテムID | ||||||
KY-AA11808968-03-30 |