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21.
Quantification of spatial gradation of slope positions 总被引:6,自引:0,他引:6
Cheng-Zhi Qin A-Xing Zhu Xun Shi Bao-Lin Li Tao Pei Cheng-Hu Zhou 《Geomorphology》2009,110(3-4):152-161
Transition between slope positions (e.g., ridge, shoulder slope, back slope, foot slope, and valley) is often gradual. Quantification of spatial transitions or spatial gradations between slope positions can increase the accuracy of terrain parameterization for geographical or ecological modeling, especially for digital soil mapping at a fine scale. Current models for characterizing the spatial gradation of slope positions based on a gridded DEM either focus solely on the parameter space or depend on too many rules defined by topographic attributes, which makes such approaches impractical. The typical locations of a slope position contain the characteristics of the slope position in both parameter space and spatial context. Thus, the spatial gradation of slope positions can be quantified by comparing terrain characteristics (spatial and parametrical) of given locations to those at typical locations. Based on this idea, this paper proposes an approach to quantifying the spatial gradation of slope positions by using typical locations as prototypes. This approach includes two parts: the first is to extract the typical locations of each slope position and treat them as the prototypes of this position; and the second is to compute the similarity between a given location and the prototypes based on both local topographic attributes and spatial context. The new approach characterizes slope position gradation in both the attribute domain (i.e., parameter space) and the spatial domain (i.e., geographic space) in an easy and practicable way. Applications show that the new approach can quantitatively describe spatial gradations among a set of slope positions. Comparison of spatial gradation of A-horizon sand percentages with the quantified spatial gradation of slope positions indicates that the latter reflects slope processes, confirming the effectiveness of the approach. The comparison of a soil subgroup map of the study area with the maximum similarity map derived from the approach also suggests that the quantified spatial gradation of slope position can be used to aid geographical modeling such as digital soil mapping. 相似文献
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牛福增 《广东海洋大学学报》2004,24(2):17-21
政府作为"公共人"在要素市场培育过程中作用发挥的程度取决于政府效率本身.从政府效率的重要性与紧迫性、政府效率的特殊性、政府效率的层次性三个方面进行必要的界说与分析,并揭示其内在的规定性. 相似文献
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彩色图像的输入指标对层次再现的影响 总被引:1,自引:0,他引:1
马桃林 《武汉大学学报(信息科学版)》2005,30(9):829-832,845
层次和细微层次是评价图像复制质量的重要指标。对两种常用平台式扫描仪的输入指标进行检测,通过分析和对比实验,研究了各指标的作用规律,并分析其对图像层次和细微层次的影响,对不同类型的彩色原稿的扫描指数的设置都具有一定的指导意义。 相似文献
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地球化学负异常及其找矿意义 总被引:7,自引:0,他引:7
地球化学负异常的存在具有普遍性。完整的地球化学异常场应包括正异常场和负异常场。负异常按其规模和找矿意义可分为区域、矿床和矿体3个不同层次。区域负异常,可以指明区域找矿方向,圈定找矿靶区;矿床负异常指出矿床可能存在的地段;矿体负异常具体圈定矿体存在的空间位置。负异常与正异常的综合研究,有助于深化对矿床成因的认识,扩大找矿信息,提高找矿效果。 相似文献
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Based on data of earthquake disaster events during 1954~2005 in the Chinese mainland, the classification and gradation of earthquake disasters have been studied by multivariate statistical analysis. Three fundamental structures of earthquake disasters have been found and an FAPE (factor analysis-principal component-equamax rotation) classification model and an HCWS (hierarchical cluster-ward method-seuclid) gradation model have been constructed. Earthquake disasters are divided into eight classes and five grades respectively in the models, which give a reasonable explanation to the phenomenon of earthquake disasters. 相似文献