彭清娥, 刘兴年, 黄尔, 赵明辉. 四川紫色土区强降雨情况下泥沙输移突增的临界条件[J]. 水科学进展, 2018, 29(2): 204-212. DOI: 10.14042/j.cnki.32.1309.2018.02.007
引用本文: 彭清娥, 刘兴年, 黄尔, 赵明辉. 四川紫色土区强降雨情况下泥沙输移突增的临界条件[J]. 水科学进展, 2018, 29(2): 204-212. DOI: 10.14042/j.cnki.32.1309.2018.02.007
PENG Qing'e, LIU Xingnian, HUANG Er, ZHAO Minghui. Critical conditions for sudden increase of sediment transport under heavy rainfall in purple soil regions of Sichuan[J]. Advances in Water Science, 2018, 29(2): 204-212. DOI: 10.14042/j.cnki.32.1309.2018.02.007
Citation: PENG Qing'e, LIU Xingnian, HUANG Er, ZHAO Minghui. Critical conditions for sudden increase of sediment transport under heavy rainfall in purple soil regions of Sichuan[J]. Advances in Water Science, 2018, 29(2): 204-212. DOI: 10.14042/j.cnki.32.1309.2018.02.007

四川紫色土区强降雨情况下泥沙输移突增的临界条件

Critical conditions for sudden increase of sediment transport under heavy rainfall in purple soil regions of Sichuan

  • 摘要: 探明强降雨下泥沙输移突增的关键特征因子及其临界条件对预防泥沙灾害及减少水土流失将起到至关重要的作用。选取典型的四川紫色土试验区鹤鸣观小流域为研究对象,采用数据分类统计对比分析方法,对试验站近10年降雨径流输沙资料进行分析,研究强降雨情况下次降雨量、降雨强度和降雨历时等对泥沙输移突增的影响,找出导致泥沙输移突增的关键特征因子及其临界条件。研究结果表明:四川紫色土区强降雨情况下泥沙输移突增的关键特征因子为次降雨量、降雨强度以及最大径流模数;同时各关键因子的临界值分别为降雨强度5.3 mm/h,次降雨量130 mm,以耕作方式为主的坡地最大径流模数临界值为6 000 dm3/(km2·s),以种植林草为主的坡地最大径流模数临界值为3 000 dm3/(km2·s)。

     

    Abstract: Understanding key factors affecting sediment transport and the threshold of sediment transport in a heavy rainfall is crucial to preventing sediment disasters and reducing soil erosions. In this study, the small watershed of Hemingguan, a purple soil region in Sichuan Province, is chosen as a typical area for research. The methods of statistical classification and comparison are used to analyze sediment transport data in recent 10 years. The influence of sub-rainfall and rainfall intensity and duration on the sudden increase of sediment transport is studied. The key factors and the threshold leading to the sudden increase of sediment transport are clarified. The results indicate that, in a typical Sichuan purple soil area, key factors for a sudden increase in sediment transport are sub-rainfall, rainfall intensity and the maximum runoff modulus. The threshold for rainfall intensity is 5.3 mm/h. The threshold for rainfall is 130 mm, and the threshold for the maximum runoff modulus of slope land is 6 000 dm3/(km2·s), based on tillage. The threshold for the maximum runoff modulus of slope land is 3 000 dm3/(km2·s), based on planting grass and trees.

     

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