楚雄师范学院学报 ›› 2026, Vol. 41 ›› Issue (3): 67-74.

• 地理科学 • 上一篇    下一篇

武定狮子山山地垂直带谱特征及其影响因素研究

刘澄静, 莫涵, 赵英杰, 王玉, 王学良   

  1. 楚雄师范学院 化学与地理科学学院,云南 楚雄 675000
  • 收稿日期:2026-02-23 出版日期:2026-05-20 发布日期:2026-07-22
  • 作者简介:刘澄静(1994-),男,博士,讲师,研究方向为景观生态学、自然地理学。
  • 基金资助:
    云南省地方本科高校(部分)基础研究联合专项-青年项目(No. 202401BA070001-015); 楚雄师范学院博士科研启动项目(No. BSQD2312); 楚雄师范学院大学生科研项目(No. XDKY25067)

Characteristics of Mountain Vertical Zonation and Its Influencing Factors on Shizi Mountain in Wuding County

Liu Chengjing, Mo Han, Zhao Yingjie, Wang Yu, Wang Xueliang   

  1. School of Chemistry and Geographical Sciences, Chuxiong Normal University, Chuxiong, Yunnan Province 675000, China
  • Received:2026-02-23 Online:2026-05-20 Published:2026-07-22

摘要: 为探究山地生态系统垂直带谱特征及其形成机制,本文以武定狮子山为研究对象,通过野外调查与系统分析,揭示了山地垂直带谱结构及其主要影响因素。研究结果表明:(1)山地植被垂直分布特征显著,植被类型以半湿润常绿阔叶林和暖温性针叶林为主,群落沿海拔梯度呈现规律性更替,自低海拔向高海拔依次表现为针叶林-常绿阔叶林、针阔混交林-针叶林的过渡序列。(2)山地土壤垂直分异明显,随海拔升高由红壤过渡为黄棕壤,其中红壤分布幅宽约为560m,黄棕壤带幅宽约为120m。研究表明,狮子山垂直带谱格局是气候、地形与人类活动共同作用的结果:垂直气候带是决定植被-土壤基本类型与宏观分布的主导因素;地形(坡向、坡度)通过对水热条件的再分配,调控着带谱的内部结构与局地变异;人类活动则通过干扰(破坏)与保护(保育),从正反两方面深刻影响着垂直带谱的现状与未来演变趋势。本研究可为深入理解亚热带山地垂直带谱的形成机制及其对全球变化的响应提供区域性实证依据。

关键词: 山地植被, 山地土壤, 垂直带谱, 空间异质性, 武定狮子山

Abstract: To investigate the characteristics and formation mechanisms of vertical zonation in mountain ecosystems, this study focuses on Shizi Mountain in Wuding County, Yunnan Province to reveal the structure of the mountain vertical zonation and its primary underlying factors through field surveys and systematic analysis. The results indicate that: 1) Exhibiting significant vertical distribution characteristics on Shizi Mountain, the mountain vegetation is dominated by semi-humid evergreen broad-leaved forest and warm-temperate coniferous forest; the plant communities show a sequential transition along the altitudinal gradient, manifesting a transition sequence, from low to high elevation, from coniferous forest to evergreen broad-leaved forest, then to coniferous and broad-leaved mixed forest, and ultimately to coniferous forest; and 2) The soil demonstrates distinct vertical differentiation, transitioning from red soil to yellow-brown earth with increasing elevation, which broadly corresponds to the mountain climate zones. The distribution range of red soil is approximately 560 m, while the yellow-brown earth zone has a width of about 120 m. This study demonstrates that the vertical zonation pattern on Shizi Mountain results from the combined effects of climate, topography, and human activities: vertical climate zones are the dominant factor determining the basic types and macro-distribution of vegetation and soil; topography (slope aspect and gradient) regulates the internal structure and local variations of the zonation by redistributing hydrothermal conditions; and human activities, through both disturbance (destruction) and conservation (protection), profoundly influence the current state and future evolution trends of the vertical zonation from both positive and negative aspects. This research provides regional empirical evidence for a deeper understanding of the formation mechanisms of subtropical mountain vertical zonation and its response to global change.

Key words: mountain vegetation, mountain soil, vertical zonation, spatial heterogeneity, Shizi Mountain in Wuding County

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