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Geomorphology of star dunes in the southern Kumtagh Desert,China: control factors and formation

机译:中国南部昆塔格沙漠的星沙地貌:控制因素和形成

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摘要

Star dunes have received less study than other major dune types, though they are widely recognized to represent a major dune type that develops under a multidirectional wind regime. Several types that include simple, compound, and complex star dunes are identified in the south of China's Kumtagh Desert. It is suggested that the formation and development of these star dunes is controlled by wind regime, the underlying and surrounding topography, and sediment availability. A complex wind regime and rich sediment availability are generally required for the development of star dunes. Especially, wind regime appears to be the most important control factor. The wind regime under which star dunes arise is characterized by the drift potential, amount of variability in drift direction, and the direction distribution mode of the drift potential. It is strongly suggested that a rectangular bimodal wind direction distribution mode has unique significance in star dune formation. Under this mode, star dunes can develop in areas with a directional variability index typical of linear dunes or even barchan dunes. A development model is proposed for star dunes based on the following evolution: barchan dunes → transverse ridges → dune networks → simple star dunes → compound star dunes → star dunes atop complex linear dunes.
机译:与其他主要沙丘类型相比,星状沙丘的研究较少,尽管众所周知,它们代表了在多向风况下发展的主要沙丘类型。在中国的古塔格沙漠以南,发现了几种类型,包括简单,复合和复杂的沙丘。建议这些沙丘的形成和发育受风态,下伏和周围地形以及沉积物可利用性的控制。沙丘的形成通常需要复杂的风况和丰富的沉积物。特别是,风况似乎是最重要的控制因素。产生沙丘的风态的特征在于漂移势,漂移方向的变化量以及漂移势的方向分布模式。强烈建议矩形双峰风向分布模式在沙丘形成中具有独特的意义。在这种模式下,星沙丘可以在具有线性沙丘甚至巴昌沙丘典型的方向变化指数的区域发育。提出了一种基于以下演变的沙丘发展模型:Barchan沙丘→横向脊→沙丘网络→简单沙丘→复合沙丘→复杂线性沙丘上的沙丘。

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  • 来源
    《Environmental earth sciences》 |2013年第1期|267-277|共11页
  • 作者单位

    Key Laboratory of Desert and Desertification, Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Sciences, No. 322, West Donggang Road,Lanzhou 730000, Gansu, China;

    Key Laboratory of Desert and Desertification, Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Sciences, No. 322, West Donggang Road,Lanzhou 730000, Gansu, China;

    Key Laboratory of Desert and Desertification, Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Sciences, No. 322, West Donggang Road,Lanzhou 730000, Gansu, China;

    Key Laboratory of Desert and Desertification, Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Sciences, No. 322, West Donggang Road,Lanzhou 730000, Gansu, China;

    Key Laboratory of Desert and Desertification, Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Sciences, No. 322, West Donggang Road,Lanzhou 730000, Gansu, China;

    Key Laboratory of Desert and Desertification, Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Sciences, No. 322, West Donggang Road,Lanzhou 730000, Gansu, China;

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

    Eolian geomorphology; Dune types; Development model of star dunes;

    机译:风尘地貌沙丘类型;星沙丘的发展模式;

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