摘要
A two-dimensional kinematic wave model was developed for simulating runoff generation and flow concentration on an experimental infiltrating hillslope receiving artificial rainfall. Experimental observations on runoff generation and flow concentration on irregular hillslopes showed that the topography of the slope surface controlled the direction and flow lines of overland flow. The model-simulated results satisfactorily compared with experimental observations. The erosive ability of the concentrated flow was found to mainly depend on the ratio of the width and depth of confluent grooves.
| 源语言 | 英语 |
|---|---|
| 页(从-至) | 28-41 |
| 页数 | 14 |
| 期刊 | Journal of Hydrology |
| 卷 | 291 |
| 期 | 1-2 |
| DOI | |
| 出版状态 | 已出版 - 31 5月 2004 |
| 已对外发布 | 是 |
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