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首页> 外文期刊>Clean >Effects of Vegetation Restoration on Soil Physical Properties in the Wind-Water Erosion Region of the Northern Loess Plateau of China
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Effects of Vegetation Restoration on Soil Physical Properties in the Wind-Water Erosion Region of the Northern Loess Plateau of China

机译:黄土高原北部风水侵蚀区植被恢复对土壤物理性质的影响

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摘要

In the northern Loess Plateau that has been severely affected by wind-water erosion, shifts from arable land to forest or grasslands have been promoted since 1998, using both native and introduced vegetation. However, there is little knowledge of the ecological consequences and effectiveness of the vegetation restoration in the region. Therefore, relationships between watershed-scale soil physical properties and plant recovery processes were analyzed. The results show that soil physical properties such as bulk density, hydraulic conductivity, mean weight diameter, and the stability of >1 mm macro-aggregates have been significantly ameliorated in the 0-20 cm soil layer under secondary natural grasslands. In contrast, re-vegetation with introduced species such as Caragana korshinski or Medicago sativa had adversely affected the soil physical properties, probably due to the deterioration of soil water conditions and lower organic matter inputs resulting from severe erosion. Reductions in bulk density and increases in saturated hydraulic conductivity could be used as indicators of soil structure amelioration since they are closely related to most other measured properties. Practical considerations for future re-vegetation projects are suggested, particularly that native species with lower water consumption rates than the introduced species should be used to avoid further soil degradation.
机译:在遭受风水侵蚀严重影响的黄土高原北部,自1998年以来,人们一直在利用原生和引进的植被促进从耕地向森林或草原的转变。但是,对该地区的生态后果和植被恢复的有效性知之甚少。因此,分析了流域尺度的土壤物理性质与植物恢复过程之间的关系。结果表明,在次生天然草地下,0-20 cm土层的土壤物理性质,例如堆积密度,水力传导率,平均重径和> 1 mm宏观聚集体的稳定性已得到明显改善。相反,引入的物种(例如柠条锦鸡儿或紫花苜蓿)的重新植被对土壤物理特性产生了不利影响,这可能是由于土壤水质恶化和严重侵蚀导致有机物输入减少所致。堆积密度的降低和饱和水力传导率的提高可以用作土壤结构改善的指标,因为它们与大多数其他测量特性密切相关。建议对未来的再植被项目进行实际考虑,特别是应该使用耗水率低于引入物种的本地物种,以避免土壤进一步退化。

著录项

  • 来源
    《Clean》 |2012年第1期|p.7-15|共9页
  • 作者单位

    The Chinese Institute of Water-saving Agriculture, Northwest A & F University, Yangling, Shaanxi,R R. China,State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, CAS & MWR,Yangling, Shaanxi, R R. China,Northwest A & F University,No. 26, Xinong Road, Yangling 712100, P. R. China;

    College of Forestry, Northwest A & F University, Yangling, Shaanxi,R R. China;

    The Chinese Institute of Water-saving Agriculture, Northwest A & F University, Yangling, Shaanxi,R R. China;

    The Chinese Institute of Water-saving Agriculture, Northwest A & F University, Yangling, Shaanxi,R R. China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    aggregate stability; bulk density; C. korshinskir; natural recovery; re-vegetation;

    机译:骨料稳定性堆密度C. korshinskir​​;自然恢复;再植被;

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