Soil Erosion Process on Slope with Biological Soil Crusts Under Rainstorm in Typical Red Soil Region

CHEN Shiting; ZHA Xuan; HUANG Shaoyan; MAO Lanhua; JIANG Xingxue; WU Jieling; HUANG Bowen; ZHOU Feihua; ZHANG Liu

doi:10.13870/j.cnki.stbcxb.2022.06.013

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Soil Erosion Process on Slope with Biological Soil Crusts Under Rainstorm in Typical Red Soil Region

更新时间：2025-03-12

- Soil Erosion Process on Slope with Biological Soil Crusts Under Rainstorm in Typical Red Soil Region
- Vol. 36, Issue 6, Pages: 95-100(2022)
- 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：
- DOI：10.13870/j.cnki.stbcxb.2022.06.013
  CLC： S157.1
- Published：2022
- 稿件说明：
移动端阅览
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：

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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references

李金峰,孟杰,叶菁,等.陕北水蚀风蚀交错区生物结皮的形成过程与发育特征[J].自然资源学报,2014,29(1):67-79.

王国鹏,肖波,李胜龙,等.黄土高原水蚀风蚀交错区生物结皮的地表粗糙度特征及其影响因素[J].生态学杂志,2019,38(10):3050-3056.

王浩,张光辉,刘法,等.黄土丘陵区生物结皮对土壤入渗的影响[J].水土保持学报,2015,29(5):117-123.

Maier S, Schmidt T, Zheng L J, et al. Analyses of dryland biological soil crusts highlight lichens as an important regulator of microbial communities[J].Biodiversity Conservation,2014,23:1735-1755.

郝旺林,夏彬,许明祥.黄土丘陵区侵蚀坡面CO

通量空间分异格局驱动机制[J].中国环境科学,2021,41(12):5875-5884.

张思琪,张科利,曹梓豪,等.喀斯特坡面生物结皮发育特征及其对土壤水分入渗的影响[J].应用生态学报,2021,32(8):2875-2885.

李林,赵允格,王一贺,等.不同类型生物结皮对坡面产流特征的影响[J].自然资源学报,2015,30(6):1013-1023.

Gao L Q, Sun H, Xu M X, et al. Biocrusts resist runoff erosion through direct physical protection and indirect modification of soil properties[J].Journal of Soil and Sediments,2020,20(1):133-142.

张光辉.退耕驱动的近地表特性变化对土壤侵蚀的潜在影响[J].中国水土保持科学,2017,15(4):143-154.

欧阳帅,项文化,陈亮,等.南方山地丘陵区森林植被恢复对水土流失调控机制[J].水土保持学报,2021,35(5):1-9.

中华人民共和国水利部.SL 419—2007水土保持试验规程[S].北京:北京科文图书业信息技术有限公司,2008:5-9.

中华人民共和国水利部.GB/T 15774—2008水土保持综合治理效益计算方法[S].北京:中国标准出版社,2009:11-13.

李新荣,谭会娟,回嵘,等.中国荒漠与沙地生物土壤结皮研究[J].科学通报,2018,63(23):2320-2334.

孙丽丽,査轩,黄少燕,等.花岗岩红壤区不同治理模式土壤抗冲性因素试验[J].水土保持学报,2019,33(5):34-40,49.

杨凯,赵军,赵允格,等.生物结皮坡面不同降雨历时的产流特征[J].农业工程学报,2019,35(23):135-141.

易婷,张光辉,王兵,等.退耕草地近地表层特征对坡面流流速的影响[J].山地学报,2015,33(4):434-440.

吉静怡,赵允格,杨凯,等.黄土丘陵区生物结皮坡面产流产沙与其分布格局的关联[J].生态学报,2021,41(4):1381-1390.

冉茂勇,赵允格,刘玉兰.黄土丘陵区不同盖度生物结皮土壤抗冲性研究[J].中国水土保持科学,2011,12(12):43-45,67.

Rey A, Carrascal L M, Báez G G, et al. Impact of climate and land degradation on soil carbon fluxes in dry semiarid grasslands in SE Spain[J].Plant and Soil,2021,461(1/2):1-17.

许欢欢,张宝琦,汪建芳,等.黄土高原典型生物结皮对坡面产流产沙过程的影响[J].水土保持通报,2020,40(6):8-13.

张冠华,易亮,丁文峰,等.三峡库区生物结皮对土壤分离过程的影响及其机制[J].土壤,2021,53(3):630-639.

高丽倩,赵允格,秦宁强,等.黄土丘陵区生物结皮对土壤可蚀性的影响[J].应用生态学报,2013,24(1):105-112.

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