风水交互作用下乌兰布和沙漠东缘地表沉积物粒度特征
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李思瑶(1998-),女,硕士研究生,主要从事荒漠化防治研究。E-mail:1109405178@qq.com

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P931.3

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内蒙古自治区科技计划项目(2022YFHH0076);国家重点研发计划项目(2024YFF1306300);内蒙古自治区直属高校基本科研业务项目(BR22-13-03)


Grain Size Characteristics of Surface Sediments at the Eastern Margin of Ulan Buh Desert under the Interaction of Wind and Water
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    摘要:

    [目的]为揭示黄河上游乌兰布和沙漠段沿岸风沙入黄的物质输运特征与空间分异模式。[方法]选取沙漠-河流直接接触的典型过渡区,基于地表湿度梯度与沉积物粒度分异,将研究区域细分为边缘区(X1)、过渡区(X2)和近岸区(X3)3个子区域,系统分析表层沉积物粒度组成和输沙特征。[结果]边缘区以中细沙为主,平均粒径145.03μm,风蚀作用强烈;过渡区中沙主导,平均粒径217.13μm;近岸区以粉粒为主,平均粒径24.95μm,水动力影响明显。各区域地表沉积物分选性差,偏度为极负偏-近对称-极负偏,峰态为尖窄-中等-尖窄。边缘区跃移组分占比>95%,呈两段式分布,表征长距离风沙搬运,过渡区以跃移为主,悬移组分仅占3%,近岸区悬移、跃移和蠕移组分分别占26.1%、67.2%和6.7%。风沙流垂向分选显著,输沙量随高度呈指数衰减,0~10 cm土层贡献率达62%~78%。边缘区、过渡区和近岸区易蚀颗粒粒径分别为170.3~446.5、137.5~401.2、123.6~291.0μm。[结论]边缘区是风蚀治理的重点区域,可通过布设沙障和提高植被盖度等方式削弱其风蚀作用,减少颗粒的释放。

    Abstract:

    [Objective] This study aimed to reveal the material transport characteristics and spatial differentiation pattern of wind-blown sand into the Yellow River along the Ulan Buh Desert in the upper reaches of the Yellow River. [Methods] A typical transition zone where the desert directly contacts the river was selected. Based on surface humidity gradients and sediment grain size differentiation, the study area was subdivided into three subregions, i.e. the marginal zone(X1), transition zone(X2), and nearshore zone(X3). The grain size composition and sediment transport characteristics of surface sediments were systematically analyzed. [Results] The marginal zone was dominated by medium-fine sand, with an average particle size of 145.03 μm and strong wind erosion. The transition zone was dominated by sand, with an average particle size of 217.13 μm. The nearshore area was dominated by silt, with an average particle size of 24.95 μm, and the hydrodynamic influence was obvious. The sorting of surface sediments in each region was poor, the skewness was extremely negative deviation-near symmetry-extremely negative deviation, and the kurtosis was narrow-medium-narrow. The proportion of saltation components in the marginal zone was more than 95%, showing a two-stage distribution indicative of long-distance aeolian sand transport. The transition zone was dominated by saltation, and the suspended component accounted for only about 3%. The suspended, saltation, and creep components in the near-shore area accounted for 26.1%, 67.2% and 6.7%, respectively. The contribution rate of 0-10 cm layer was 62%-78%, and the near surface was the core area of wind-blown sand activity. The particle size ranges of the erodible particles in the marginal zone, the transition zone, and the nearshore zone were 170.3-446.5, 137.5-401.2 and 123.6-291.0 μm, respectively. [Conclusion] The marginal zone is the key area for wind erosion control. The wind erosion effect can be weakened and the release of particles can be reduced by setting sand barriers and increasing vegetation coverage.

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李思瑶, 蒙仲举.风水交互作用下乌兰布和沙漠东缘地表沉积物粒度特征[J].水土保持学报,2025,39(4):139~147

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  • 收稿日期:2025-01-25
  • 最后修改日期:2025-03-21
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  • 在线发布日期: 2025-09-10
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