高寒矿区排土场边坡植被恢复年限对产流产沙的影响
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X169,S152.7

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中国地质调查局项目“黄河源鄂陵湖-扎陵湖地区生态保护修复支撑调查”(DD20220960)


Effects of vegetation restoration duration on runoff and sediment yield in slopes of waste dumps in alpine mining areas
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    摘要:

    [目的] 明确高寒矿区排土场边坡植被恢复年限对产流产沙特征的影响,为后续高效开展人工植被修复及水土保持工作提供科学依据。[方法] 以青海省果洛藏族自治州德尔尼铜矿区不同恢复期的排土场边坡为研究对象,通过开展植物样方调查和模拟降雨试验,分析植被恢复年限对产流产沙特征的影响。[结果] ①随着恢复年限的增加,植被覆盖度、凋落物量、地上生物量等植物生长特征指标均显著上升(p<0.05),物种多样性和植物根系呈“量—质—结构”的阶梯式恢复模式。②6 a恢复样地土壤颗粒密度、含水率、紧实度和黏聚力较1 a样地分别提升23.70%,80.26%,152.96%和171.17%,土壤容重与孔隙度分别降低36.30%和74.46%。③降雨后9~15 min是排土场边坡土壤侵蚀的敏感期,产沙率随降雨时间呈现出先增后减的变化趋势,产流率呈现先急剧增大后稳定波动的变化趋势;降雨强度与恢复年限均显著影响产流产沙量,且恢复年限可减弱降雨强度的侵蚀效应。④冗余分析(RDA)表明,植物根系表面积密度(p<0.01)、Shannon-Wiener指数(p<0.05)和孔隙度(p<0.05)是影响土壤侵蚀的关键环境因子。结构方程模型(SEM)表明植物群落特征(路径系数为-0.892)和植物根系特征(路径系数为-0.733)直接或通过土壤物理力学性质(路径系数为-0.839)间接影响土壤侵蚀。[结论] 高寒矿区排土场边坡上开展人工植被恢复措施可明显提升土壤抗侵蚀能力,并且随恢复年限的增大,植被群落功能结构通过改良土壤物理力学性质,可有效降低水土流失风险。

    Abstract:

    [Objective] The influence of vegetation restoration duration on runoff and sediment yield characteristics on the slopes of waste dumps in alpine mining areas was clarified in order to provide a scientific basis for the subsequent efficient implementation of artificial vegetation restoration and soil and water conservation efforts. [Methods] Taking the slopes of waste dumps at different restoration stages in the Delni copper mine area, Guoluo Xizang Autonomous Prefecture, Qinghai Province, as the research subjects, this study analyzed the influence of vegetation restoration duration on runoff and sediment yield characteristics through plant plot surveys and simulated rainfall tests. [Results] ① As the restoration duration increased, vegetation coverage, litter mass, aboveground biomass, and other plant growth characteristic indicators showed significant increases(p<0.05). Species diversity and plant root systems exhibited a stepwise recovery pattern characterized by ‘quantity-qualitystructure'.② Compared with the 1-year restoration plot, the 6-year restoration plot exhibited increases of 23.70%, 80.26%, 152.96%, and 171.17% in soil particle density, moisture content, firmness, and cohesion, respectively. Conversely, soil bulk density and porosity decreased by 36.30% and 74.46%, respectively, compared with the 1-year plot.③ The period of 9—15 minutes after rainfall was the sensitive phase for soil erosion on the slopes of waste dumps. The sediment yield rate showed a trend of initially increasing and then decreasing with rainfall duration, while the runoff yield rate showed a sharp initial increase followed by stable fluctuations. Both rainfall intensity and restoration duration significantly influenced runoff and sediment yield, with restoration duration mitigating the erosive effects of rainfall intensity.④ Redundancy analysis(RDA) indicated that root surface area density(p<0.01), Shannon-Wiener index(p<0.05), and porosity(p<0.05) were key environmental factors influencing soil erosion. Structural equation modeling(SEM) revealed that plant community characteristics(path coefficient=-0.892) and plant root characteristics(path coefficient=-0.733) directly or indirectly influenced soil erosion through soil physical and mechanical properties(path coefficient=-0.839). [Conclusion] Implementing artificial vegetation restoration measures on the slopes of waste dumps in alpine mining areas can significantly enhance soil erosion resistance. As the restoration duration increases, the functional structure of the vegetation community improves soil physical and mechanical properties, thereby effectively reducing the risk of soil erosion.

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李洪军,童生春,徐得忠,彭海月,陈丽,陈燿.高寒矿区排土场边坡植被恢复年限对产流产沙的影响[J].水土保持通报,2026,46(2):1-13

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  • 收稿日期:2025-09-11
  • 最后修改日期:2025-11-09
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  • 在线发布日期: 2026-04-01
  • 出版日期: 2026-02-15