黄土坡面细沟侵蚀形态特征及横断面分异性
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刘庆(1995—),男,硕士研究生,主要从事土壤侵蚀与水土保持研究。E-mail:2200902206@cnu.edu.cn

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S157.1

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国家自然科学基金项目(52179071,41977069)


Morphological Characteristics and Cross-sectional Heterogeneity of Rill Erosion on Loess Slope
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    摘要:

    [目的] 为探究细沟侵蚀及其形态特征的变化规律和横断面分布特征。[方法] 通过室内人工模拟降雨试验和三维激光扫描技术,分析不同降雨强度和坡度条件下细沟侵蚀产流产沙和细沟形态分布特征。[结果] 1)降雨强度增大时,坡面产流产沙增幅显著,90 mm/h降雨强度时,细沟侵蚀量对总侵蚀量的贡献率达90%以上。2)细沟宽度、深度和细沟割裂度受降雨强度的影响明显,且均呈不同程度的增加,细沟割裂度、细沟最大深度与细沟侵蚀量呈极显著正相关。3)细沟横断面沿坡向变化较大,沟壁崩塌现象明显,60 mm/h降雨强度时细沟横断面多呈“窄浅”型分布,90 mm/h降雨强度时,细沟总体表现为沟头和细沟下部横断面呈“窄浅”型,在细沟中部表现为“宽深”型,细沟中部侵蚀较为严重。4)60 mm/h降雨强度时,细沟横断面指标总体为0.46~0.79,90 mm/h降雨强度时总体为0.41~0.85;90 mm/h降雨强度时,随着坡度的增加,细沟横断面指标波动性增强,表明细沟横断面空间分异性更加明显,细沟横断面形态的变化趋于不规则。[结论] 研究结果为细沟侵蚀防治提供一定理论支持。

    Abstract:

    [Objective] To explore the variation patterns and cross-sectional distribution characteristics of rill erosion and its morphological features. [Methods] Indoor artificially simulated rainfall experiments and 3D laser scanning were conducted to analyze the distribution of runoff,sediment yield and rill morphological characteristics of rill erosion under different rainfall and slope conditions. [Results] 1)When the rainfall intensity increased,the runoff and sediment yield increased significantly. When the rainfall intensity was 90 mm/h,the contribution rate of rill erosion to total erosion could reach more than 90%. 2)Rill width,depth,width-to-depth ratio and rill splitting degree were significantly affected by rainfall intensity,and all showed varying degrees of increase. Rill splitting degree and the maximum depth of rill showed a significant positive correlation with the amount of rill erosion. 3)Rill cross section varied greatly along the slope direction,the collapse of the gully wall was obvious. When the rainfall intensity was 60 mm/h,the rill cross section was mostly distributed in a "narrow and shallow" shape,When the rainfall intensity was 90 mm/h,the head and bottom of the rill were "narrow and shallow",the middle of the rill was "wide and deep" in general. The rill erosion in the middle was more severe. 4)When the rainfall intensity was 60 and 90 mm/h,the overall value range of rill cross-sectional index were 0.46—0.79 and 0.41—0.85,respectively. When the rainfall intensity was 60 mm/h,the volatility of rill cross-sectional index increased with the increase of slope gradient,indicating that spatial differentiation of rill cross section was more obvious,and variation of the rill cross section tended to be irregular. [Conclusion] The research results can provide some theoretical support for rill erosion prevention and control.

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刘庆, 沈东辉, 和继军, 刘壮壮, 孙莉英, 蔡强国.黄土坡面细沟侵蚀形态特征及横断面分异性[J].水土保持学报,2025,39(2):30~39,47

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  • 收稿日期:2024-08-11
  • 最后修改日期:2024-11-19
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  • 在线发布日期: 2025-05-07
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