Stability analysis unit and spatial distribution pattern of the terrain texture in the northern Shaanxi Loess Plateau Stability analysis unit and spatial distribution pattern of the terrain texture in the northern Shaanxi Loess Plateau

最小化 最大化

Vol15 No.3: 577-589 

【Title】Stability analysis unit and spatial distribution pattern of the terrain texture in the northern Shaanxi Loess Plateau

AuthorDING Hu1,2,3; NA Jia-ming1,2,3; HUANG Xiao-li1,2,3; TANG Guo-an1,2,3*; LIU Kai4

Addresses1 Key Laboratory of Virtual Geographic Environment (Ministry of Education), Nanjing Normal University, Nanjing 210023, China; 2 Jiangsu Center for Collaborative Innovation in Geographical Information Resource Development and Application, Nanjing 210023, China; 3 State Key Laboratory Cultivation Base of Geographical Environment Evolution (Jiangsu Province), Nanjing 210023, China; 4 Key Laboratory of Watershed Geographic Sciences, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China

Corresponding authortangguoan@njnu.edu.cn

CitationDing H, Na JM, Huang XL, et al. (2018) Stability analysis unit and spatial distribution pattern of the terrain texture in the northern Shaanxi Loess Plateau. Journal of Mountain Science 15(3). https://doi.org/10.1007/s11629-017-4551-4

DOIhttps://doi.org/10.1007/s11629-017-4551-4

AbstractTerrain texture analysis is an important method of digital terrain analysis in quantitative geomorphological research and in the exploration of the spatial heterogeneity and autocorrelation of terrain features. However, a major issue often neglected in previous studies is the calculation unit of the terrain texture, that is, the stability analysis unit. As the test size increases, the derived terrain textures become increasingly similar so that their differences can be ignored. The test size of terrain texture is defined as the stability analysis unit. This study randomly selected 48 areas within the Loess Plateau in northern Shaanxi in China as the study sites and used the gray level co-occurrence matrix to calculate the terrain texture. The stability analysis unit of the terrain texture was then extracted, and its spatial distribution pattern in the Loess Plateau was studied using spatial interpolation method. Four terrain texture metrics, i.e., homogeneity, energy, correlation, and contrast, were extracted on the basis of the stability analysis unit, and the spatial variation patterns of these parameters were studied. Results showed that the spatial distribution pattern and the terrain texture metrics reflected a trend of high–low–high from north to south, which correlated with the spatial distribution of the landforms at the Loess Plateau. In addition, the terrain texture measures was significantly correlated with the terrain factors of gully density and slope, and this relationship showed that terrain texture measures based on the stability analysis unit could reflect the basic characteristics of terrain morphology. The stability analysis unit provided a reasonable analytical scale for terrain texture analysis and could be used as a measure of the regional topography to accurately describe basic terrain characteristics.

KeywordsDigital terrain analysis; Terrain texture; Stability analysis unit; Spatial distribution; Loess Plateau