苔藓覆盖对喀斯特林地碳酸盐岩红土剥蚀过程的影响

蒋娟; 曾昊; 刘冬冬; 车陆禄; 张广映

doi:10.13870/j.cnki.stbcxb.2022.02.012

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苔藓覆盖对喀斯特林地碳酸盐岩红土剥蚀过程的影响

更新时间：2024-11-07

- 苔藓覆盖对喀斯特林地碳酸盐岩红土剥蚀过程的影响
- Effects of Moss Cover on Detachment Process of Carbonate Derived Laterite from Karst Forest Land
- 水土保持学报 2022年36卷第2期页码：92-98
- 作者机构：
  
  1. 贵州大学资源与环境工程学院,贵阳,550025
  2. 喀斯特地质资源与环境教育部重点实验室,贵阳,550025
  3. 湖州南太湖水利水电勘测设计院有限公司宁波分公司,浙江,宁波,315300
- 作者简介：
  
  [ "蒋娟(1998-),女,硕士生,主要从事岩溶区生态水文研究。E-mail:1977164433@qq.com" ]
- 基金信息：
  
  国家自然科学基金项目（41807016）黔科合支撑项目（[2020]4Y010）贵州省水利科技经费项目（KT201803）贵州省研究生基金立项课题项目（黔教合YJSCXJH[2020]094）
- DOI：10.13870/j.cnki.stbcxb.2022.02.012
  中图分类号： S157.1
- 纸质出版：2022
- 稿件说明：
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蒋娟, 曾昊, 刘冬冬, 等. 苔藓覆盖对喀斯特林地碳酸盐岩红土剥蚀过程的影响[J]. 水土保持学报, 2022,36(2):92-98.

JIANG Juan, ZENG Hao, LIU Dongdong, et al. Effects of Moss Cover on Detachment Process of Carbonate Derived Laterite from Karst Forest Land[J]. 2022, 36(2): 92-98.
蒋娟, 曾昊, 刘冬冬, 等. 苔藓覆盖对喀斯特林地碳酸盐岩红土剥蚀过程的影响[J]. 水土保持学报, 2022,36(2):92-98. DOI： 10.13870/j.cnki.stbcxb.2022.02.012.

JIANG Juan, ZENG Hao, LIU Dongdong, et al. Effects of Moss Cover on Detachment Process of Carbonate Derived Laterite from Karst Forest Land[J]. 2022, 36(2): 92-98. DOI： 10.13870/j.cnki.stbcxb.2022.02.012.

摘要

为探究苔藓覆盖对喀斯特山地土壤剥蚀过程影响的机理

通过野外采集原状土样

结合上方来水冲刷剥蚀试验

分析了不同坡度(5°

20°)与不同土壤含水率(饱和含水率、田间含水率)条件下苔藓盖度与土壤分离能力间的定量关系

解析了坡面流水力特征参数对苔藓覆盖的响应规律。结果表明:在5°和20°坡度下

苔藓覆盖下饱和土壤的土壤剥蚀率分别比田间含水率土壤高33.9%和10.8%。与裸土层相比

苔藓覆盖能够在高土壤含水率条件下有效抑制土壤剥蚀率

且在低坡度下效果更显著。田间含水率土壤的剥蚀率随着苔藓盖度的增加呈线性减小趋势(R2>0.995)。此外

苔藓覆盖对5°坡度的坡面流水力特征参数有显著影响

饱和土壤条件下的苔藓覆盖显著改变坡面流流态(P<0.05)。与裸土层相比

苔藓覆盖显著降低坡面流速(20.6%)、雷诺数(0.6%)、弗劳德数(28.6%)和径流功率(0.8%)

显著增加径流深(27.8%)、水流切应力(26.9%)和阻力系数(117.0%)。然而20°坡度下苔藓覆盖对坡面流水力特征参数并没有显著影响。总体而言

苔藓覆盖下碳酸盐岩红土的土壤剥蚀率与坡面流水力特性没有显著相关性。研究结果可为探明苔藓覆盖在喀斯特山地的水土保持效应提供试验依据。

Abstract

The influences of moss cover on detachment process of carbonate derived laterite in karst mountainous lands were explored and analysed. Undisturbed soil samples were collected and subjected to flow scouring in a 3.5 m long hydraulic flume. Two degrees of slope (5°

20°) and two soil water contents (saturated soil water content

field capacity) were selected to quantify the relationship between moss coverage and soil detachment rate. The responses of hydraulic characteristics of slope runoff to moss cover were also analyzed. Compared to the field capacity

the results indicated that the detachment rate of saturated soil under moss cover increased by 33.9% and 10.8% at slopes of 5 and 20 degrees

respectively. The effects of moss cover on reducing soil detachment rate were more effective than that of bare soil without moss cover

and its effects were more obvious at lower slopes. The detachment rate under field capacity soil condition decreased in a linear trend with increasing moss coverage (R2>0.995). The moss cover had significant effects on the hydraulic characteristics of runoff flow at the slope of 5 degrees. The moss cover under saturated soil condition significantly changed the flow regime of surface runoff (P<0.05). Compared to bare soil without moss cover

the moss cover significantly reduced the runoff velocity (-20.6%)

Reynolds number (-0.6%)

Froude number (-28.6%) and runoff power (-0.8%)

increased the runoff depth (+27.8%)

flow shear stress (+26.9%) and Darcy-Weisbach resistance coefficient (+117.0%). Besides

the moss cover had no significant effects on the hydraulic characteristics of slope runoff at the slope of 20 degrees. Overall

no significant correlation exhibited between the hydraulic characteristics of runoff flow and the soil detachment rate of carbonate derived laterite covered with moss. These results can provide the experimental data for the study of applying moss cover to soil and water conservation in karst mountainous lands.

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