模拟降雨条件下崩积体坡面产流产沙特征及其响应关系

朱高立; 肖泽干; 刘晓静; 黄炎和; 邹伟; 林金石; 蒋芳市

doi:10.13961/j.cnki.stbctb.2016.06.001

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模拟降雨条件下崩积体坡面产流产沙特征及其响应关系

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- 模拟降雨条件下崩积体坡面产流产沙特征及其响应关系
- Processes and Responses of Runoff and Sediment Yield on Colluvial Deposits Under Simulated Rainfall
- 水土保持通报 2016年36卷第6期页码：1-7
- 作者机构：
  
  1. 福建农林大学资源与环境学院,福建,福州,350002
  2. 南京农业大学公共管理学院,江苏,南京,210095
- 作者简介：
- 基金信息：
  
  国家自然科学基金项目“花岗岩崩岗土体胶结物质与抗剪强度的关系”（41571272），“组合指纹法分析花岗岩崩岗侵蚀产沙运移规律研究”（41001169）;国家科技支撑计划项目（2014BAD15B0303）
- DOI：10.13961/j.cnki.stbctb.2016.06.001
  中图分类号：
- 纸质出版：2016
- 稿件说明：
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朱高立, 肖泽干, 刘晓静, 等. 模拟降雨条件下崩积体坡面产流产沙特征及其响应关系[J]. 水土保持通报, 2016,36(6):1-7.

ZHU Gaoli, XIAO Zegan, LIU Xiaojing, et al. Processes and Responses of Runoff and Sediment Yield on Colluvial Deposits Under Simulated Rainfall[J]. Bulletin of Soiland Water Conservation, 2016, 36(6): 1-7.
朱高立, 肖泽干, 刘晓静, 等. 模拟降雨条件下崩积体坡面产流产沙特征及其响应关系[J]. 水土保持通报, 2016,36(6):1-7. DOI： 10.13961/j.cnki.stbctb.2016.06.001.

ZHU Gaoli, XIAO Zegan, LIU Xiaojing, et al. Processes and Responses of Runoff and Sediment Yield on Colluvial Deposits Under Simulated Rainfall[J]. Bulletin of Soiland Water Conservation, 2016, 36(6): 1-7. DOI： 10.13961/j.cnki.stbctb.2016.06.001.

摘要

[目的] 研究崩积体坡面产流产沙特征及其响应关系，为崩岗治理提供理论基础与科学依据。[方法] 通过室内模拟降雨试验，探讨不同覆盖度（0%，25%，50%，75%，100%）和坡度（25°，30°，35°）组合坡面在90 mm/h雨强条件下的产流产沙时空特征及其响应关系。[结果] 不同覆盖度和坡度条件下，坡面产流时间的变化范围在33~292 s；同一坡度条件下，坡面产流时间与覆盖度呈线性正相关关系；同一覆盖度条件下，坡面产流时间与坡度呈幂函数关系。通过双因素方差分析可知，坡度对径流量的影响达到极显著水平，覆盖度对产沙量的影响达到显著水平。当坡度为25°时，坡面产沙总量的临界覆盖度为50%；当坡度为30°时，坡面产沙总量的临界覆盖度为75%；当坡度为35°时，坡面径流量的临界覆盖度为50%。[结论] 针对不同坡度崩积体坡面，可以选择合适的秸秆覆盖度以达到较好的水土保持效果。

Abstract

[Objective] The erosion mechanism of colluvial deposits was researched to provide a theoretical basis and scientific evidence for the treatment of collapsing hills.[Methods] An indoor rainfall simulation experiment on slopes of colluvial deposits under 90 mm/h rainfall

and with the treatments of coverages(0

25%

50%

75%

100%) and slopes(25°

30°

35°) was carried out. Runoff and sediment were measured.[Results] The initiating time of runoff under different conditions changed from 33 to 292 s. Under the same slope gradient

there was a linear positive correlation between the initiating time of runoff and the straw coverage

and the initiating time of runoff had a power function with slope as independent variable. Through two-way variance analysis

the influence of slope on runoff was very significant and the influence of coverage on sediment yield was significant. The critical straw coverage of sediment yield was 50% under 25°

the critical straw coverage of sediment yield was 75% under 30°

the critical straw coverage of runoff was 50% under 35°.[Conclusion] For different slope gradients of colluvial deposits

we can choose optimal coverage of straw to reduce sediment yield and runoff effectively.

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references

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