[灌草植被和生物结皮对暴雨条件下黄土高原边坡水土流失及水动力特性的影响]。

Q3 Environmental Science
Chen-Xi Dan, Qiong Zhang, Gang Liu, Xiao-Lin Xia
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引用次数: 0

摘要

在黄土高原植被恢复初期,灌草植被能有效缓解强降雨引起的土壤侵蚀,而生物土壤结皮(生物结皮)和植被能共同调节径流产沙过程。然而,它们的综合效应通常被忽视。为了量化灌草植被和生物结皮对径流-泥沙动力学的影响,并阐明它们对侵蚀力学的协同效应,我们进行了短时间、高强度降雨事件的室内人工模拟,采用9种处理:裸露土壤(CK,无植被/生物结皮);草原;灌木;生物外壳覆盖率20%;草地+生物硬壳,覆盖率20%;盖度为20%的灌木+生物硬壳;生物外壳覆盖率40%;草地+生物硬壳,覆盖度40%;灌木+生物硬壳的覆盖率为40%。结果表明:1)在降雨过程中,灌丛、禾草和生物结皮均能显著减少土壤侵蚀,CK的沙积最大;2)与对照相比,灌丛和草地分别减少了21.9%和18.2%的径流量,促进了土壤水分入渗。而盖度为20%和40%时,径流增加幅度分别为9.5%和17.4%,表明盖度对入渗有抑制作用。在植被+生物结皮条件下,植被对土壤入渗的积极影响超过了生物结皮的消极影响。3)覆盖度为20%的草地+生物痂处理和覆盖度为40%的生物痂处理均产生亚临界流,其他处理均为超临界流。各处理的平均流速和流动动能均低于对照,但流动剪应力和阻力系数均高于对照。与对照相比,覆盖度为40%的草地+生物硬壳处理的径流剪切应力和阻力系数最高,分别增加了164.5%和213.8%,径流动能最低,减少了91.9%。这些结果表明,在植被恢复的早期阶段保持适当的生物覆盖有助于加强土壤保持和生态系统的稳定性。在试验条件下,40%盖度的草地+生物硬壳处理对减少土壤侵蚀效果最优。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
[Effects of shrub-grass vegetation and biocrusts on soil and water loss and hydrodynamic characteristics of Loess Plateau slopes under rainstorm conditions].

During the initial stages of vegetation restoration on the Loess Plateau, shrub-grass vegetation effectively mitigates soil erosion caused by intense rainfall, while biological soil crusts (biocrust) and vegetation collectively can regulate runoff and sediment yield processes. However, their combined effects are usually overlooked. To quantify the impacts of shrub-grass vegetation and biocrust on runoff-sediment dynamics and to elucidate their synergistic effects on erosion mechanics, we conducted indoor artificial simulations of short-duration, high-intensity rainfall events, with nine treatments: bare soil (CK, no vegetation/biocrust); grassland; shrub; biocrust with 20% coverage; grassland+biocrust with 20% coverage; shrub+biocrust with 20% coverage; biocrust with 40% coverage; grassland + biocrust with 40% coverage; and shrub + biocrust with 40% coverage. The results showed that: 1) During the rainfall events, CK consistently exhibited the highest sediment volume, while the shrub, grass, and biocrust significantly reduced erosion. 2) Compared to the CK, shrub and grass reduced runoff by 21.9% and 18.2%, respectively, which promoted soil moisture infiltration. In contrast, biocrust with 20% and 40% coverage increased runoff by 9.5% and 17.4%, respectively, indicating that biocrusts inhibited infiltration. The positive effect of vegetation on soil infiltration surpassed the negative impact of biocrusts under vegetation+biocrust conditions. 3) The grassland+biocrust with 20% coverage treatment and all treatments with 40% biocrust generated subcritical flow, while other treatments were supercritical flow. All treatments showed lower average flow velocity and flow kinetic energy than CK, but exhibited higher flow shear stress and resistance coefficients. Compared to the CK, the grassland+biocrust with 40% coverage treatment demonstrated the highest runoff shear stress and resistance coefficient, with 164.5% and 213.8% increases, respectively, while the runoff kinetic energy was the lowest, decreasing by 91.9%. These findings suggested that maintaining appropriate biocrust coverage during the early stages of vegetation recovery could be helpful for enhancing soil conservation and ecosystem stability. Under the experimental conditions, the grassland+biocrust with 40% coverage treatment is optimal for soil erosion reduction.

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来源期刊
应用生态学报
应用生态学报 Environmental Science-Ecology
CiteScore
2.50
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0.00%
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11393
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