Responses of Rain Splash Erosion and Soil Crust Development to Particle Size
文献类型：会议论文
| 作者 | Cheng Q. J. ; Ma W. J. ; Cai Q. G. |
| 出版日期 | 2010 |
| 关键词 | Splash rate Rainfall simulator Key factors Susceptibility seal formation simulated rainfall interrill erosion infiltration-rate detachment |
| 页码 | 3-9 |
| 英文摘要 | Soil particle size is one of the key parameters determining splash erosion and soil crust development. Based on simulated rainfalls with a high intensity of 1.2 mm min-1, the rain splash erosion and soil crust development of Loess soil separates with different diameters are studied and the key factors predicting soil crust formation are discussed. The results indicated that: (1) as the diameter of soil separates increases, the amount of detached particles increases from < 0.038 mm to a maximum amount of 0.15-0.22 mm, and subsequently decreases; (2) the smaller the soil separates, the easier the development of soil crust and the higher the degree of soil crust development; (3) the susceptibility of soil crust formation can be predicted by integrating three indices of soil texture, aggregate stability, and rainfall energy together. |
| 收录类别 | CPCI |
| 会议录出版者 | Aussino Acad Publ House |
| 语种 | 英语 |
| ISBN号 | 978-1-921712-06-7 |
| 源URL | [http://ir.igsnrr.ac.cn/handle/311030/25054]  |
| 专题 | 地理科学与资源研究所_历年回溯文献 |
| 推荐引用方式 GB/T 7714 | Cheng Q. J.,Ma W. J.,Cai Q. G.. Responses of Rain Splash Erosion and Soil Crust Development to Particle Size[C]. 见:. |
入库方式： OAI收割
来源：地理科学与资源研究所
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