黄丘区野外坡面产流产沙过程对不同植被覆盖结构的响应

秦东远; 肖培青; 郝仕龙; 杨春霞

doi:10.13870/j.cnki.stbcxb.2019.02.012

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黄丘区野外坡面产流产沙过程对不同植被覆盖结构的响应

更新时间：2025-03-12

- 黄丘区野外坡面产流产沙过程对不同植被覆盖结构的响应
- Response of Slope Runoff and Sediment Yield to Different Vegetation Cover Structures in the Loess Hilly Region
- 水土保持学报 2019年33卷第2期页码：73-78
- 作者机构：
  
  1. 华北水利水电大学资源环境学院,郑州,450045
  2. 黄河水利科学研究院, 水利部黄土高原水土流失过程与控制重点实验室,郑州,450003
- 作者简介：
  
  [ "秦东远(1992-),男,在读硕士研究生,主要从事土壤侵蚀模拟与监测研究。E-mail:dongyuanqin16@163.com" ]
- 基金信息：
  
  国家自然科学基金项目（41571276，41701326）河南省创新型科技人才队伍建设工程项目（162101510004）中央级公益性科研院所基本科研业务费专项（HKY-JBYW-2016-33）
- DOI：10.13870/j.cnki.stbcxb.2019.02.012
  中图分类号：
- 纸质出版：2019
- 稿件说明：
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秦东远, 肖培青, 郝仕龙, 等. 黄丘区野外坡面产流产沙过程对不同植被覆盖结构的响应[J]. 水土保持学报, 2019,33(2):73-78.

QIN Dongyuan, XIAO Peiqing, HAO Shilong, et al. Response of Slope Runoff and Sediment Yield to Different Vegetation Cover Structures in the Loess Hilly Region[J]. 2019, 33(2): 73-78.
秦东远, 肖培青, 郝仕龙, 等. 黄丘区野外坡面产流产沙过程对不同植被覆盖结构的响应[J]. 水土保持学报, 2019,33(2):73-78. DOI： 10.13870/j.cnki.stbcxb.2019.02.012.

QIN Dongyuan, XIAO Peiqing, HAO Shilong, et al. Response of Slope Runoff and Sediment Yield to Different Vegetation Cover Structures in the Loess Hilly Region[J]. 2019, 33(2): 73-78. DOI： 10.13870/j.cnki.stbcxb.2019.02.012.

摘要

植被覆盖结构是影响坡面侵蚀过程的重要因素，通过在黄丘区罗玉沟流域开展自然植被覆盖坡面野外模拟降雨试验，分析了90 mm/h雨强条件下地下根系、地下根系+地表结皮层和地下根系+地表结皮层+植被冠层3种不同覆盖结构对坡面产流产沙过程影响。结果表明：植被根系层次对增强土壤入渗起主导作用，使土壤入渗量增加67%，稳定入渗率增加39.7%；3种植被覆盖结构中，地表结皮层对产流和产沙具有最好的调控作用，减流贡献率和减沙贡献率分别为43%和67%；根系小区和裸地小区累积产流量与累积产沙量之间呈幂函数关系，随着植被覆盖结构的叠加，累积产流量与累积产沙量之间呈线性函数的关系；多层次植被覆盖结构能够延长坡面侵蚀过程的发育期，缩短活跃期。研究结果对定量评价植被措施的减水减沙作用具有重要意义。

Abstract

Vegetation cover structure is a key factor affecting slope erosion process. Based on the simulated rainfall experiment carried out on a slope covered by natural vegetation in Luoyugou watershed of loess hilly region

the effects of three different cover structures on slope runoff and sediment yield were studied under the condition of 90 mm/h rainfall intensity. These three cover structures included the underground root system

the underground root system plus the surface crust

as well as the combination of underground root system

the surface crust and the vegetation canopy. The results were as follows:(1) The root system of the vegetation played a leading role in enhancing soil infiltration

the amount of soil infiltration and the steady infiltration rate on the vegetation root slope increased by 67% and 39.7%

respectively

compared with those on bare slope. (2) For the three vegetation cover structures

the surface crust had the best regulation effect on the runoff and sediment yield

and the contribution rate of runoff reduction and sand reduction was 43% and 67%

respectively. (3) There was a power function relationship between the accumulative runoff yield and accumulative sediment yield in the vegetation root plot and the bare plot

and the relationship turned out to be linear function with the superposition of vegetation cover structure. (4) The multi-level vegetation cover structure could prolong the development period and shorten the active period of the slope erosion process. The research results were important for quantitative evaluation of the effects of vegetation measures on water and sediment reduction.

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Keywords

references

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