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Fractals in topography: Application to geoarchaeological studies in the surroundings of the necropolis of Dahshur, Egypt

机译:分形在地形中的应用:在埃及Dahshur墓地周围的地质考古研究中的应用

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The necropolis of Dahshur in northern Egypt witnessed human-environment interaction on a millennial scale but to an unknown extent. The present study aims to decipher ephemeral channel networks, which are common landscape features in the surroundings of the necropolis, from landforms that were subject to human influence. The analysis was carried out on the basis of surface geometry as derived from a digital elevation model (DEM). The hypothesis is tested that the natural fractal patterns of channel networks lead to fractal surface topography, when fluvial processes are the main factors for relief evolution. Therefore, the estimated fractal dimension of channel networks is correlated with the fractal dimension of surface topography to determine the mutual functional relationship. A high degree of functional relationship within some areas of the DEM shows that channel networks are self-similar branching trees that imprint their geometry on to surface topography in a scale range of ~15 to ~ 190 m. A low correlation of fractal patterns of channel network and surface topography in the vicinity of the pyramid district of the necropolis is interpreted as channel beds modified or induced by human impact, either due to the usage of the channel beds as transport ways for building material leading to an acceleration of processes like soil erosion or due to direct activities like mining or landscape architecture.
机译:埃及北部达赫舒(Dahshur)的墓地见证了人类与环境的互动,但其影响程度已达到千禧年规模,但程度未知。本研究旨在从受人类影响的地貌中解密临时通道网络,这些通道网络是大墓地周围常见的景观特征。分析是基于从数字高程模型(DEM)得出的表面几何形状进行的。检验了假设,当河流过程是浮雕演化的主要因素时,渠道网络的自然分形图案会导致分形表面形貌。因此,将通道网络的估计分形维数与表面形貌的分形维数相关联,以确定相互的功能关系。 DEM某些区域内的高度功能关系表明,通道网络是自相似的分支树,在约15至190 m的范围内将其几何形状压印到表面地形上。在大墓地的金字塔区域附近,通道网络的分形图案与表面形貌的低相关性被解释为通道层是人为影响所修饰或诱发的,这可能是由于通道层被用作建筑材料的运输途径加速土壤侵蚀等过程,或者由于采矿或景观建筑等直接活动而加速。

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  • 来源
    《Quaternary International》 |2012年第17期|p.34-46|共13页
  • 作者单位

    Department of Earth Sciences, Physical Geography, Freie Universitat Berlin, Malteserstrajie 74-100, 12249 Berlin, Germany;

    Department of Earth Sciences, Physical Geography, Freie Universitat Berlin, Malteserstrajie 74-100, 12249 Berlin, Germany;

    Department of Earth Sciences, Physical Geography, Freie Universitat Berlin, Malteserstrajie 74-100, 12249 Berlin, Germany;

    Department of Earth Sciences, Physical Geography, Freie Universitat Berlin, Malteserstrajie 74-100, 12249 Berlin, Germany;

    German Archaeological Institute, 31, Abu el Feda, 11211 Cairo-Zamalek, Egypt;

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