Slope runoff study in situ using rainfall simulator in mountainous area of north china
文献类型：期刊论文
| 作者 | Yu Jingjie1; Yang Cong2; Liu Changming1; Song Xianfang1; Hu Shanshan1,3; Li Fadong1,4; Tang Changyuan4 |
| 刊名 | Journal of geographical sciences
 |
| 出版日期 | 2009-08-01 |
| 卷号 | 19期号:4页码:461-470 |
| 关键词 | Simulated rainfall Slope plot Runoff generation process Mountainous area of north china |
| ISSN号 | 1009-637X |
| DOI | 10.1007/s11442-009-0461-x |
| 通讯作者 | Yu jingjie(yujj@igsnrr.ac.cn) |
| 英文摘要 | Simulated rainfall is a valid tool to examine the runoff generation on the slope. 13 simulated rainfall experiments with different rainfall intensities and durations are completed in a 5 m x 10 m experimental plot in mountainous area of north china. simultaneously, rainfall, surface runoff, soil-layer flow, mantel-layer flow and soil moisture are monitored respectively. from the results, it is found that the hydrographs in all layers have the characteristics of rapid rise and fall. the recessions of surface flow and soil-layer flow are much faster than that of mantel-layer flow. surface flow, the main contributor, makes up more than 60% of the total runoff in the study area. it even exceeds 90% in the cases of high intensity rainfall events. runoff coefficient (ratio of total runoff to rainfall amount) is mainly influenced by rainfall amount, rainfall intensity and antecedent soil moisture, and the relationship can be well expressed by a multiple linear regression function alpha = 0.002p + 0.182i + 4.88w(a) - 0.821. the relation between the rainfall intensity and the lag time of three flows (surface runoff, soil-layer flow and mantel-layer flow) is shown to be exponential. then, the result also shows that the recession constant is 0.75 for surface runoff, is 0.94 for soil-layer and mantel-layer flow in this area. in this study area, the dominant infiltration excess runoff is simulated by horton model. about 0.10 mm/min percolation is observed under the condition of different rainfall intensities, therefore the value is regarded as the steady infiltration rate of the study area. |
| WOS关键词 | SOIL ; INFILTRATION |
| WOS研究方向 | Geology |
| WOS类目 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000268246700007 |
| 出版者 | SCIENCE PRESS |
| URI标识 | http://www.irgrid.ac.cn/handle/1471x/2404054 |
| 专题 | 中国科学院大学 |
| 通讯作者 | Yu Jingjie |
| 作者单位 | 1.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Water Cycle & Related Land Surface Proc, Beijing 100101, Peoples R China 2.Minist Water Resources, Bur Comprehens Dev, Beijing 100053, Peoples R China 3.Chinese Acad Sci, Grad Univ, Beijing 100039, Peoples R China 4.Chiba Univ, Chiba 2638522, Japan |
| 推荐引用方式 GB/T 7714 | Yu Jingjie,Yang Cong,Liu Changming,et al. Slope runoff study in situ using rainfall simulator in mountainous area of north china[J]. Journal of geographical sciences,2009,19(4):461-470. |
| APA | Yu Jingjie.,Yang Cong.,Liu Changming.,Song Xianfang.,Hu Shanshan.,...&Tang Changyuan.(2009).Slope runoff study in situ using rainfall simulator in mountainous area of north china.Journal of geographical sciences,19(4),461-470. |
| MLA | Yu Jingjie,et al."Slope runoff study in situ using rainfall simulator in mountainous area of north china".Journal of geographical sciences 19.4(2009):461-470. |
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来源：中国科学院大学
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