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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:陕北黄土高原坡谱的定量分析及空间分布

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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:斜率频谱被定义为特定区域中的斜率分布的统计模型。以前的研究主要关注斜坡谱的形态学;其空间分布尚不清楚,特别是在黄土高原中。信息熵和统计数据的理论和方法适用于定量分析山西省黄土高原的坡度分析坡度分析及其空间分布。实验结果表明,斜坡谱的信息熵(H),斜坡谱的偏斜度和地形驱动力因子(T_D)可以适当地描绘与不同的观点不同的斜率谱及其空间分布。斜坡谱的空间分布代表黄土地形类型的空间分布,它与黄土高原土壤侵蚀强度的空间分布是相关的。 H,T_D和GULLY密度,表面切口深度显示阳性相关性:沟壑密度和表面切口随着H,T_D增加而增加。相反,S和GULLY密度,表面切口深度显示出负相关。最后,Slope Spectrum和黄土地形类型之间的空间关系也是定性分析的,以及黄土地形演进。

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