张静, 吴洁, 秦公伟, 姚祖强. 基于DEM的秦巴山片区地貌特征及形态划分[J]. 云南大学学报(自然科学版), 2021, 43(6): 1147-1155. doi: 10.7540/j.ynu.20200707
引用本文: 张静, 吴洁, 秦公伟, 姚祖强. 基于DEM的秦巴山片区地貌特征及形态划分[J]. 云南大学学报(自然科学版), 2021, 43(6): 1147-1155. doi: 10.7540/j.ynu.20200707
ZHANG Jing, WU Jie, QIN Gong-wei, YAO Zu-qiang. Geomorphic features and morphological classification in Qinling-Bashan Mountains based on DEM[J]. Journal of Yunnan University: Natural Sciences Edition, 2021, 43(6): 1147-1155. DOI: 10.7540/j.ynu.20200707
Citation: ZHANG Jing, WU Jie, QIN Gong-wei, YAO Zu-qiang. Geomorphic features and morphological classification in Qinling-Bashan Mountains based on DEM[J]. Journal of Yunnan University: Natural Sciences Edition, 2021, 43(6): 1147-1155. DOI: 10.7540/j.ynu.20200707

基于DEM的秦巴山片区地貌特征及形态划分

Geomorphic features and morphological classification in Qinling-Bashan Mountains based on DEM

  • 摘要: 秦巴山片区山地地貌典型,地质灾害、水土流失等生态问题突出,加强其地貌特征及形态分析有助于揭示生态问题的成因机理. 文章基于数字高程模型数据,采用领域统计法、均值变点法、ISO聚类非监督分类法和局部空间自相关性等,开展了秦巴山片区地形特征及地貌类型划分研究. 结果表明:①地形起伏度最佳统计窗口是13×13,领域面积为1.3689 km2,平均地形起伏度350.61 m;②研究区最佳地形因子组合为地表切割深度、曲率、高程变异系数和高程,累计贡献率超过92.05%;③空间上地貌呈现西高东低、北高南低的特征,秦岭中西段和巴山东段地形切割深;④基于县域的地形起伏度空间集聚性,表现为秦巴山区西部武都区与巴山东段岚皋县等县(区)呈现H−H型聚集;秦巴山区东部郧县与巴山南麓剑阁县等县(区)呈现L−L型聚集. 受地质构造和岩性的影响,巴山东段和秦岭西段景观更为破碎,对区域水土流失和生态环境造成重要影响.

     

    Abstract: There is a typical mountainous area with prominent ecological problems such as geological disasters and soil erosion in Qinling-Bashan Mountains. It will help reveal the genetic mechanism of ecological problems to strengthen the analysis of geomorphic features and morphology. Based on the DEM data, this paper studies the topographic characteristics and geomorphic classification of Qinling-Bashan Mountains by using the methods of domain statistics, mean change point, ISO clustering unsupervised classification and local spatial autocorrelation. The results show: ① The best statistical window of topographic relief is 13×13, the area of which is 1.3689 km2, and the average topographic relief is 350.61 m; ② The best combination of topographic factors in the study region consists of surface cutting depth, curvature, elevation and its variation coefficient, the cumulative contribution ratio of which is over 92.05%. ③ Spatially, the geomorphic features are high in the West and low in the East, and high in the North and low in the South; besides, the topographic cutting is deep in the middle and West of Qinling Mountains and the East of Bashan Mountains; ④ The spatial clustering of the topographic relief has demonstrated an H-H type of aggregation in Wudu District of the western Qinling-Bashan mountains, and in Langao County and other counties and districts of eastern Bashan Mountains, while an L-L type of aggregation is shown in Yunxian County of the eastern Qinling-Bashan mountains, and in Jiange County and other counties of the southern Bashan Mountains. Due to the influence of geological structure and lithology, the topography is more fragmented in the east of Bashan Mountains and the west of Qinling Mountains, which has an important impact on regional soil erosion and ecological environment.

     

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