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| 黄土区坡面侵蚀时空分布与上坡来水作用的实验研究 | |
| 引用本文： | 王文龙,雷阿林,李占斌,唐克丽. 黄土区坡面侵蚀时空分布与上坡来水作用的实验研究[J]. 水利学报, 2004, 35(5): 0025-0030 |
| 作者姓名： | 王文龙 雷阿林 李占斌 唐克丽 |
| 作者单位： | 1. 中国科学院水利部,水土保持研究所黄土高原土壤侵蚀与旱地农业国家重点实验室,陕西,杨凌,712100;西北农林科技大学,水土保持研究所,陕西,杨凌,712100 2. 水利部,国家环保局长江流域水资源保护局,湖北,武汉,430051 3. 中国科学院水利部,水土保持研究所黄土高原土壤侵蚀与旱地农业国家重点实验室,陕西,杨凌,712100;西安理工大学,水资源研究所,陕西,西安,710048 |
| 基金项目： | 中国科学院知识创新工程项目(KZCX1 10 04)，国家自然科学基金(49671052)，黄土高原土壤侵蚀与旱地农业国家重点实验室重点基金(10501 78) |
| 摘 要： | 本文采用多坡段模型，运用模拟降雨实验方法研究了坡面侵蚀时空分布特征和上坡来水来沙的侵蚀作用，结果表明：坡面各部位的侵蚀方式与雨强密切对应。定量分析得出径流量、产沙量与坡度呈对数关系，与坡长呈线性关系，与雨强呈幂函数关系，建立了产沙量与坡度、雨强及径流量的关系式。同时也建立了产沙量、产沙增量与上坡来水来沙的关系方程，上坡来水使梁峁坡和谷坡产沙量增大了20.2%～63.5%和42.9%～74.5%。 |
| 关 键 词： | 黄土区；土壤侵蚀；时空分布特征；上坡来水作用 |
| 文章编号： | 0559-9350(2004)05-0025-07 |
Experimental study on spatial and temporal distribution of erosion on loess slope |
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| WANG Wen-long. Experimental study on spatial and temporal distribution of erosion on loess slope[J]. Journal of Hydraulic Engineering, 2004, 35(5): 0025-0030 | |
| Authors: | WANG Wen-long |
| Affiliation: | State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau. Institute of Soil and Water Conservation, Chinese Academy Sciences and Ministry of Water Resources, Yangling 712100, China; Northwest Sci-Tech University of Agriculture and Forestry, Yangling 712100, China |
| Abstract: | The spatial and temporal distributions of erosion on loess slope were studied by simulated rainfall experiment. The experimental hillslope model was consisted of four segments of loess slope with different gradients. The results showed that the evolution of erosion processes along different positions of the slope is closely related to rainfall intensity. The runoff and sediment yield are logarithmically related to slope gradient, linearly related to slope length and exponentially related to rainfall intensity. A formula for calculating the sediment yield according to the slope gradient, rainfall intensity and runoff was established. Furthermore, the effects of inflow from upperslope segment on runoff and sediment yield was also studied. It is found that the sediment yield increased by 20%-63% on hill slope and 43%-75% on gully slope respectively. |
| Keywords: | loess slope soil erosion spatial and temporal distribution runoff sediment yield inflow from upper slope |
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