Rainfall intensity and inflow rate effects on hillslope soil erosion in the Mollisol region of Northeast China
文献类型：期刊论文
| 作者 | Wen, Leilei2,3; Zheng, Fenli2,3; Shen, Haiou2,3; Bian, Feng2,3; Jiang, Yiliang1,2 |
| 刊名 | NATURAL HAZARDS
 |
| 出版日期 | 2015-10-01 |
| 卷号 | 79期号:1页码:381-395 |
| 关键词 | Rainfall Intensity Inflow Rate Soil Erosion Soil Loss Equation Mollisol Region |
| 文献子类 | Article |
| 英文摘要 | Soil erosion in the Mollisol region of Northeast China is increasingly severe and directly affects national food security and sustainable development. However, few attempts have been made to create a clear distinction between the effects of rainfall and inflow on hillslope soil erosion. A laboratory study was conducted to discuss the roles and contributions of rainfall intensity and inflow rate to hillslope soil erosion and to fit equations based on variations of rainfall intensity and inflow rate (RI + IR) for soil erosion. A soil pan (8 m long, 1.5 m wide and 0.6 m deep and with an adjustable slope gradient of 0A degrees-35A degrees) was subjected to designed rainfall intensities (0, 50 and 100 mm h(-1)) and inflow rates (0, 50 and 100 mm h(-1)). The results showed that the effects of RI + IR treatments on hillslope soil loss were significantly greater than those on runoff. Furthermore, the effect of rainfall intensity on hillslope soil loss was significantly greater than the effect of inflow rate. Under the same total water supply, an increase in rainfall intensity resulted in greater average soil loss rates and stronger fluctuations in soil loss than an increase in the inflow rate. The occurrence of rill erosion significantly increased sediment transport capacity on the hillslope, which resulted in an increase in soil loss. Utilizing rainfall intensity and inflow rate, runoff and soil loss equations were generated and validated, and the performances of the two equations were satisfactory. Furthermore, it was determined that both equations are most applicable to the prediction of hillslope soil erosion under long rolling hillslope conditions. For the Mollisol region of Northeast China, the key factor affecting soil erosion on hillslopes is soil particle dispersion caused by rainfall. Therefore, taking measures to cover the soil, such as corn straw mulching, would effectively reduce rainfall erosivity and have significant positive effects on soil erosion prevention and control. |
| 出版地 | 233 SPRING ST, NEW YORK, NY 10013 USA |
| WOS关键词 | SEDIMENT TRANSPORT CAPACITY ; BLACK SOIL ; RAINDROP IMPACT ; LAND-USE ; RUNOFF ; ERODIBILITY ; REGIMES ; WATER ; CONSERVATION ; DEGRADATION |
| WOS研究方向 | Geology ; Meteorology & Atmospheric Sciences ; Water Resources |
| 语种 | 英语 |
| 出版者 | SPRINGER |
| WOS记录号 | WOS:000361060500021 |
| 源URL | [http://ir.iswc.ac.cn/handle/361005/10425]  |
| 专题 | 中国科学院水利部水土保持研究所 |
| 通讯作者 | Zheng, Fenli |
| 作者单位 | 1.Northwest A&F Univ, Inst Soil & Water Conservat, Yangling 712100, Shaanxi, Peoples R China 2.CAS & MWR, Inst Soil & Water Conservat, Yangling 712100, Shaanxi, Peoples R China 3.Northwest A&F Univ, Coll Nat Resources & Environm, State Key Lab Soil Eros & Dryland Farming Loess P, Yangling 712100, Shaanxi, Peoples R China |
| 推荐引用方式 GB/T 7714 | Wen, Leilei,Zheng, Fenli,Shen, Haiou,et al. Rainfall intensity and inflow rate effects on hillslope soil erosion in the Mollisol region of Northeast China[J]. NATURAL HAZARDS,2015,79(1):381-395. |
| APA | Wen, Leilei,Zheng, Fenli,Shen, Haiou,Bian, Feng,&Jiang, Yiliang.(2015).Rainfall intensity and inflow rate effects on hillslope soil erosion in the Mollisol region of Northeast China.NATURAL HAZARDS,79(1),381-395. |
| MLA | Wen, Leilei,et al."Rainfall intensity and inflow rate effects on hillslope soil erosion in the Mollisol region of Northeast China".NATURAL HAZARDS 79.1(2015):381-395. |
入库方式： OAI收割
来源：水土保持研究所
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