刘洪延, 宋维峰, 马建刚. 哈尼梯田核心区麻栗寨河流域水系结构特征及分维数分析[J]. 西南林业大学学报(自然科学), 2020, 40(2): 143–148 . DOI: 10.11929/j.swfu.201901036
引用本文: 刘洪延, 宋维峰, 马建刚. 哈尼梯田核心区麻栗寨河流域水系结构特征及分维数分析[J]. 西南林业大学学报(自然科学), 2020, 40(2): 143–148 . DOI: 10.11929/j.swfu.201901036
Hongyan Liu, Weifeng Song, Jiangang Ma. Structural Characteristics and Fractal Dimension Analysis of the Water Network in the Malizhai River Basin in the Core Area of Hani Terrace[J]. Journal of Southwest Forestry University, 2020, 40(2): 143-148. DOI: 10.11929/j.swfu.201901036
Citation: Hongyan Liu, Weifeng Song, Jiangang Ma. Structural Characteristics and Fractal Dimension Analysis of the Water Network in the Malizhai River Basin in the Core Area of Hani Terrace[J]. Journal of Southwest Forestry University, 2020, 40(2): 143-148. DOI: 10.11929/j.swfu.201901036

哈尼梯田核心区麻栗寨河流域水系结构特征及分维数分析

Structural Characteristics and Fractal Dimension Analysis of the Water Network in the Malizhai River Basin in the Core Area of Hani Terrace

  • 摘要: 运用ArcGIS的水文分析工具、数据管理工具,定量分析哈尼梯田核心区麻栗寨河流域水系的结构特征;并利用网格计算法以及基于Horton理论计算了其水系分维数,对比分析得出阈值为400时与实际最符合。结果表明:麻栗寨河流域河网密度整体较大,随流域流向逐渐减小,大小河流发育程度差异较大,水系结构发育完整;分维数均在1.6<D≤1.89内,流域处于地貌侵蚀发育的壮年期,并向老年期发展,河流下蚀作用逐渐减弱,侧蚀成为主要侵蚀类型。

     

    Abstract: The hydrological analysis tool and data management tool of ArcGIS were used to quantitatively analyze the structural characteristics of the water system of the Malizhai River Basin in the core area of Hani terrace; The fractal dimension of the water system is calculated by the grid method and Horton theory. The comparison analysis shows that the threshold value of 400 is the most consistent with the actual situation. The results show that the river network density in the Malizhai River Basin is larger as a whole and decreases with the flow direction. The development of large and small rivers is obviously different, and the water network is well developed; The fractal dimensions were all within 1.6<D≤1.89, the basin was in the prime period of geomorphologic erosion development, and developed towards the old age, the downstream erosion gradually weakened, and the lateral erosion became the main erosion type.

     

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