暴雨条件下典型红壤区生物结皮坡面水土流失过程研究

陈诗婷; 查轩; 黄少燕; 毛兰花; 姜兴雪; 吴洁玲; 黄博文; 周飞华; 张柳

doi:10.13870/j.cnki.stbcxb.2022.06.013

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暴雨条件下典型红壤区生物结皮坡面水土流失过程研究

更新时间：2025-03-12

- 暴雨条件下典型红壤区生物结皮坡面水土流失过程研究
- Soil Erosion Process on Slope with Biological Soil Crusts Under Rainstorm in Typical Red Soil Region
- 水土保持学报 2022年36卷第6期页码：95-100
- 作者机构：
  
  1. 福建师范大学地理科学学院,福州,350007
  2. 福建省亚热带资源与环境重点实验室,福州,350007
- 作者简介：
- 基金信息：
  
  国家重点研发计划项目"南方红壤低山丘陵区水土流失综合治理"(2017YFC05054);国家科技支撑计划项目"福建红壤区生态修复和持续经营关键技术集成和示范"(2014BAD15B02)
- DOI：10.13870/j.cnki.stbcxb.2022.06.013
  中图分类号： S157.1
- 纸质出版：2022
- 稿件说明：
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陈诗婷, 查轩, 黄少燕, 等. 暴雨条件下典型红壤区生物结皮坡面水土流失过程研究[J]. 水土保持学报, 2022,36(6):95-100.

CHEN Shiting, ZHA Xuan, HUANG Shaoyan, et al. Soil Erosion Process on Slope with Biological Soil Crusts Under Rainstorm in Typical Red Soil Region[J]. 2022, 36(6): 95-100.
陈诗婷, 查轩, 黄少燕, 等. 暴雨条件下典型红壤区生物结皮坡面水土流失过程研究[J]. 水土保持学报, 2022,36(6):95-100. DOI： 10.13870/j.cnki.stbcxb.2022.06.013.

CHEN Shiting, ZHA Xuan, HUANG Shaoyan, et al. Soil Erosion Process on Slope with Biological Soil Crusts Under Rainstorm in Typical Red Soil Region[J]. 2022, 36(6): 95-100. DOI： 10.13870/j.cnki.stbcxb.2022.06.013.

摘要

为探明暴雨条件下典型红壤区生态恢复工程实施后生物结皮覆盖对坡面水土流失过程的影响

通过模拟降雨和室内分析试验

探究不同结皮覆盖度(0

20%

40%

60%

80%)坡面的土壤物理属性、水动力学特征及产流产沙过程。结果表明:(1)生物结皮覆盖下的红壤坡面土壤黏结力平均增加13.26%

土壤容重与穿透阻力平均分别减小8.97%和61.51%

表明生物结皮可有效增强红壤区坡面土壤稳定性

提升土壤抗蚀能力;(2)相较对照坡面

其余盖度坡面均可有效改善水流流态

坡面径流剪切力介于0.08~0.12。水流功率和断面单位能量分别减小12.22%~78.89%

8.32%~53.15%

坡面阻力系数增大1.09~1.50倍;(3)各生物结皮盖度坡面减流、减沙效益分别介于12.50%~78.76%

17.03%~94.31%

其中高覆盖度(80%)坡面土壤侵蚀强度较小。研究结果为有效防治红壤区坡面水土流失工作提供理论依据和实践参考。

Abstract

In order to reveal the effect of biological soil crusts on process of soil and water loss on the slope after the implementation of ecological restoration project in typical red soil region under rainstorm

simulated rainstorm experiments and indoor experiments were conducted. In this research

the soil physical properties

hydrodynamic characteristics

runoff and sediment yield processes of slopes with different biological soil crusts coverages (0

20%

40%

60% and 80%) were explored. The results showed that: (1) Under different coverages of biological soil crusts

the soil cohesion of red soil slope increased by 13.26% on average

while the soil bulk density and penetration resistance decreased by 8.97% and 61.51% on average

respectively

indicating that biological soil crusts effectively enhanced soil stability and soil anti-erodibility in red soil area. (2) Compared with the control slope

biological soil crusts effectively improved the flow pattern of slope

and the values of runoff shear stress ranged from 0.08 to 0.12. The water flow power and section unit energy reduced by 12.22%~78.89% and 8.32%~53.15%

respectively

and the slope resistance coefficient increased by 1.09~1.50 times. (3) The benefits of runoff reduction and sediment reduction on the slope surface of each biological crust coverage were between 12.50% and 78.76%

17.03% and 94.31%

respectively

in which the soil erosion intensity of the slope with high coverage (80%) was the lowest. The results provided theoretical basis and practical references for effective prevention and control of soil and water loss on slope in red soil area.

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