高寒草甸退化秃斑地土壤风蚀规律研究
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青海大学地质工程系

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the Soil Wind Erosion law of Degraded Bare Patches in Alpine Meadows
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    摘要:

    [目的]探究高寒草甸退化秃斑地土壤风蚀规律,为退化草甸区的植被恢复和生态环境保护提供科学依据。[方法] 本研究选取青海省河南县因高原鼠兔活动而退化形成的秃斑地作为研究对象,在9、12、15 m/s三种风速条件下,对不同植被覆盖度(0%、20%、40%、60%、80%)的退化秃斑地进行原位模拟风力侵蚀试验,以探究植被盖度在不同风速下对土壤风蚀的影响。[结果]①退化秃斑地的土壤风蚀速率随时间推移呈现先急剧下降后趋于平缓的变化趋势(p < 0.05)。在总时长为60 min的风蚀试验下,前10 min是土壤风蚀速率变化的敏感期。②3种风速下,植被盖度与总输沙量之间均呈显著负相关的指数函数关系(R2 = 0.98),其指数系数绝对值越大,在较高风速下植被覆盖度对风蚀的抑制作用越弱。③随着植被盖度的增加,0-5cm高度范围内输沙量显著降低,且各植被盖度的输沙量均随高度增加而逐渐减少。[结论] 增加植被盖度能够有效降低风蚀速率和输沙高度,但在较高风速下,植被盖度对风蚀的抑制效果显著减弱,且植被盖度抑制土壤风蚀的关键阈值在40%左右,并随着植被盖度的持续增大,风蚀减少的边际效益逐渐降低。

    Abstract:

    [ Objective ] To explore the law of soil wind erosion in degraded bare patches of alpine meadow, and to provide scientific basis for vegetation restoration and ecological environment protection in degraded meadow area. [ Methods ] In this study, we selected the bald patches formed by the degradation of plateau pika activity in Henan County, Qinghai Province as the research object. Under the three wind speeds of 9,12 and 15 m / s, the degraded bald patches with different vegetation coverage ( 0 %, 20 %, 40 %, 60 %, 80 % ) were subjected to in-situ simulated wind erosion experiments to explore the effects of vegetation coverage on soil wind erosion under different wind speeds. [ Results ] ① The soil wind erosion rate of degraded bare land showed a trend of rapid decline and then tended to be gentle over time ( p < 0.05 ). ② Under the wind erosion test with a total duration of 60 min, the first 10 min is the sensitive period of soil wind erosion rate change. Under the three wind speeds, there was a significant negative exponential function relationship between vegetation coverage and total sediment discharge ( R2 = 0.98 ). The greater the absolute value of the exponential coefficient, the weaker the inhibitory effect of vegetation coverage on wind erosion at higher wind speeds.③ With the increase of vegetation coverage, the sediment transport in the height range of 0-5cm decreased significantly, and the sediment transport of each vegetation coverage decreased gradually with the increase of height. [ Conclusion ] Increasing vegetation coverage can effectively reduce the wind erosion rate and sand transport height, but at higher wind speeds, the inhibition effect of vegetation coverage on wind erosion is significantly weakened, and the key threshold of vegetation coverage to inhibit soil wind erosion is about 40 %. With the continuous increase of vegetation coverage, the marginal benefit of wind erosion reduction gradually decreases.

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  • 收稿日期:2024-11-12
  • 最后修改日期:2025-01-09
  • 录用日期:2025-01-09
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