黄土坡面细沟侵蚀形态特征及横断面分异性研究
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1.首都师范大学城市环境过程和数字模拟国家重点实验室培育基地 水资源安全北京实验室;2.水利部科技推广中心;3.中国科学院地理科学与资源研究所

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S157.1?????????????

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国家自然科学基金(52179071,41977069)


Study on the morphological characteristics and cross-sectional heterogeneity of rill erosion on loess slope
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Affiliation:

State Key Laboratory of Urban Environmental Processes and Numerical Simulation,Beijing Laboratory of Water Resources Security,Capital Normal University.

Fund Project:

National Natural Science Foundation of China(No.52179071;No.41977069)

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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,90mm/h降雨强度时,细沟侵蚀量对总侵蚀量的贡献率可达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,且均呈现不同程度的增加,细沟割裂度、细沟最大深度与细沟侵蚀量呈极显著的正相关关系。(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,细沟横断面的变化趋于不规则。[结论]该研究结果可为细沟侵蚀防治提供一定的理论支持。

    Abstract:

    [Objective]To explore the variation patterns and cross-sectional distribution characteristics of rill erosion and its morphological features. [Methods]Indoor artificial simulation 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 production increased significantly; When the rainfall intensity is 90mm/h, the contribution rate of rill erosion to the total erosion can 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; The rill splitting degree and the maximum depth of rill showed a significant positive correlation with the amount of rill erosion. (3)The rill cross-sectional varies greatly along the slope direction which the collapse of the gully wall is obvious, When the rainfall intensity is 60mm/h, the rill cross-sectional is mostly distributed in a "narrow shallow" shape, When the rainfall intensity is 90mm/h, the rill head and the bottom are “narrow and shallow”, in the middle is “wide and deep” in general, the rill erosion in the middle is more severe. (4)When the rainfall intensity is 60mm/h, the overall value range of rill cross-sectional index is 0.46~0.79, 0.41~0.85 in 90mm/h rainfall intensity; When the rainfall intensity is 60mm/h, the volatility of rill cross-sectional index increased with the increase of slope gradient, indicate that spatial differentiation of rill cross-sectional is more obvious, also showed that variation of the rill cross-sectional tends to be irregular. [Conclusion]the research results can provide some theoretical support for rill erosion prevention and cure.

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  • 收稿日期:2024-08-11
  • 最后修改日期:2024-11-20
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  • 在线发布日期: 2025-02-21
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