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Geomorphological inheritance for loess landform evolution in a severe soil erosion region of Loess Plateau of China based on digital elevation models

机译:基于数字高程模型的黄土高原重度水土流失区黄土地貌演化的地貌遗传

摘要

The influence of pre-quaternary underlying terrain on the formation of loess landforms, i.e., the geomorphological inheritance issue, is a focus in studies of loess landforms. On the basis of multi-source information, we used GIS spatial analysis methods to construct a simulated digital elevation model of a pre-quaternary paleotopographic surface in a severe soil erosion area of the Loess Plateau. To reveal the spatial relationship between underlying paleotopography and modern terrain, an XY scatter diagram, hypsometric curve, gradient and concavity of terrain profiles are used in the experiments. The experiments show that the altitude, gradient and concavity results have significant linear positive correlation between both terrains, which shows a relatively strong landform inheritance relationship, particularly in the intact and complete loess deposit areas. Despite the current surface appearing somewhat changed from the original shape of the underlying terrain under different erosion forces, we reveal that the modern terrain generally smoothes the topographic relief of underlying terrain in the loess deposition process. Our results deepen understanding of the characteristics of geomorphological inheritance in the formation and evolution of loess landforms.
机译:第四纪前陆面地形对黄土地貌形成的影响,即地貌遗传问题,是黄土地貌研究的重点。在多源信息的基础上,我们利用GIS空间分析方法,建立了黄土高原水土流失严重地区第四纪古地形的模拟数字高程模型。为了揭示底层古地形和现代地形之间的空间关系,在实验中使用了XY散布图,测压曲线,地形剖面的梯度和凹度。实验表明,海拔,坡度和凹度结果在两个地形之间都具有显着的线性正相关关系,这表明了相对较强的地形遗传关系,特别是在完整​​和完整的黄土沉积地区。尽管当前表面在不同的侵蚀力下与基础地形的原始形状有所不同,但我们发现,现代地形通常会在黄土沉积过程中平滑基础地形的地形起伏。我们的研究结果加深了对黄土地貌形成和演化过程中地貌遗传特征的认识。

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