首页> 外文会议>Conference on Geospatial Information Science; 20070525-27; Nanjing(CN) >Quantitative analysis and spatial distribution of slope spectrum -A case study in the Loess Plateau in north Shaanxi province
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Quantitative analysis and spatial distribution of slope spectrum -A case study in the Loess Plateau in north Shaanxi province

机译:坡度谱的定量分析与空间分布-以陕北黄土高原为例

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Slope spectrum is defined as a statistic model of slope distribution in a certain area. Previous researches mainly focus on morphology depiction of the slope spectrum; its spatial distribution is unknown yet, especially in the Loess Plateau. Theory and methodology of information entropy and statistics are applied for the objective of quantitatively analyzing the slope spectrum and its spatial distribution in the Loess Plateau in North Shaanxi province. Experiment results show that slope spectrum's information entropy (H), skewness of slope spectrum (S) and terrain driving force factor (T_d) can appropriately depict the slope spectrum and its spatial distribution from different points of view. Spatial distribution of the slope spectrum represents spatial distribution of loess landform types, and it is correlatable with spatial distribution of soil erosion intensity in the Loess Plateau. H, T_d and gully density, surface incision depth show positive correlation: gully density and surface incision increase as H, T_d increase. On the contrary, the S and gully density, surface incision depth show negative correlation. Lastly, spatial relationship between slope spectrum and loess landform types are qualitatively analyzed, and loess landform evolution as well.
机译:坡度谱定义为一定区域内坡度分布的统计模型。以往的研究主要集中在坡度谱的形态描述上。其空间分布还未知,特别是在黄土高原。运用信息熵统计理论和方法,对陕北黄土高原坡面光谱及其空间分布进行定量分析。实验结果表明,坡谱的信息熵(H),坡谱的偏度(S)和地形驱动力因子(T_d)可以从不同的角度恰当地描述坡谱及其空间分布。坡度谱的空间分布代表了黄土高原类型的空间分布,并且与黄土高原土壤侵蚀强度的空间分布相关。 H,T_d与沟密度,表面切口深度呈正相关:沟密度和表面切口随H,T_d的增加而增加。相反,S与沟壑密度,表面切口深度呈负相关。最后,定性分析了坡度谱与黄土地貌类型之间的空间关系,以及黄土地貌的演化。

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