黄土高原生物结皮混合群落对坡面流流体阻力特征的影响
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白洁(2000-),女,硕士研究生,主要从事土壤侵蚀研究。E-mail:1608436422@qq.com

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S154.3

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国家重点研发计划项目(2023YFF1305103);国家自然科学基金面上项目(42377352);中国科学院“西部之光”西部青年学者A类项目(XAB2022YW03)


Effects of Mixed Communities of Biological Crusts on Fluid Resistance Characteristics of Overland Flow on the Loess Plateau
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    摘要:

    [目的]为明确生物结皮影响坡面流阻力作用机制,研究不同生物结皮类型组成的混合群落对坡面流颗粒阻力(fg)和形态阻力(ff)的影响。[方法]采集3种(以藻为主、藻藓比例相当、以藓为主)混合生物结皮原状土壤样品84个,设置7组坡度和流量组合,采用变坡水槽冲刷试验,系统研究不同水动力条件下坡面流阻力特征对生物结皮响应。[结果] 1)坡面流流经生物结皮覆盖区流速减少8.5%~57.3%,水深增加5.4%~70.6%;生物结皮混合群落缓流效率随藓类结皮占比的增加显著增强,以藓为主混合生物结皮(T3)缓流效率是其他生物结皮混合群落的1.1~2.5倍。藓类结皮占比的增加降低弗劳德数(Fr),增加雷诺数(Re),未改变流型流态。2)生物结皮混合群落覆盖显著增加总阻力f(Darcy-Weisbach阻力系数),且f随Re和Fr的增加呈幂函数降低(R2≥0.46、p<0.01),与藓生物量(Mmoss)呈显著正相关(p<0.05)。3)生物结皮覆盖显著增加坡面流ff,不同坡度、流量及生物结皮混合群落覆盖条件下,fff的主要部分;fg与泥沙浓度(qs)呈显著相关(p<0.05),ffMmoss呈显著正相关(p<0.05)。4)Savat模型计算的坡面流fg不适用于生物结皮覆盖下的低泥沙浓度坡面流;基于fgff的影响因子,构建生物结皮覆盖下的坡面流f系数方程f=Re-1.021 4×Mmoss0.311×103.793。[结论]生物结皮覆盖下,坡面流ff显著增加是导致其总阻力增加的主要原因,且主要受藓类结皮占比影响。研究结果对深入理解生物结皮影响坡面流阻力作用机制具有重要意义,可为黄土高原生物结皮防控土壤侵蚀提供理论基础。

    Abstract:

    [Objective] This study aimed to clarify the mechanisms by which biological soil crust(BSCs) influence overland flow resistance, focusing on the effects of mixed biocrust communities on grain resistance(fg) and form resistance(ff). [Methods] A total of 84 undisturbed soil samples with three different mixed BSCs compositions(algae-dominated, equal algae-moss ratio, and moss-dominated) were collected, flume scouring experiments under seven combinations of slope gradient and flow discharge were set up, and the response of overland flow resistance characteristics to BSCs was systematically investigate under different hydrodynamic conditions.[Results] 1) Biocrust coverage reduced the velocity of overland flow by 8.5%-57.3% and increased water depth by 5.4%-70.6%. The flow slowing effect of mixed BSCs was enhanced significantly with the increasing proportion of moss crust, with the flow slowing effect of moss-dominated community(T3) being 1.1 to 2.5 times greater than that of other mixed BSCs. Increased moss proportion reduced Froude number(Fr) and increased Reynolds number(Re) without altering the flow pattern or flow regime. 2) Coverage of mixed communities of biological crust significantly increased the total resistance(Darcy-Weisbach resistance coefficient) f, which decreased as a power function with the increase of Re and FrR2≥0.46, p<0.01),and showed a significant positive correlation with the biomass of moss crust(Mmoss)( p<0.05). 3) BSCs coverage significantly increased the ff of overland flow, which was the dominant part of the f of overland flow under different slope gradients, flow discharges, and BSCs coverage conditions. The fg was significantly correlated with sediment load(qs)(p<0.05), and ff was positively correlated with Mmossp<0.05). 4) The fg calculated by Savat model was not applicable to overland flow with low qs under BSCs coverage. Based on the influencing factors of fg and ff, a new equation for the f of overland flow under BSCs coverage was established: f=Re-1.021 4×Mmoss0.311×103.793. [Conclusion] Under BSCs coverage, the main reason for the increase of the f of overland flow is the increase of the ff, which is mainly affected by the proportion of moss crust. The study is of great significance for clarifying the mechanism of BSCs affecting overland flow resistance, and provides a theoretical basis for using BSCs to prevent and control soil erosion on the Loess Plateau.

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白洁, 王兵, 杨艳芬, 李成芳, 王静, 马金龙.黄土高原生物结皮混合群落对坡面流流体阻力特征的影响[J].水土保持学报,2025,39(4):177~186

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  • 收稿日期:2024-12-26
  • 最后修改日期:2025-02-21
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  • 在线发布日期: 2025-09-10
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