• Included in CSCD
  • Chinese Core Journals
  • Included in WJCI Report
  • Included in Scopus, CA, DOAJ, EBSCO, JST
  • The Key Magazine of China Technology
Volume 29 Issue 3
Sep.  2010
Turn off MathJax
Article Contents
WANG Di, XU Mo, QI Ji-hong, ZHANG Qiang. Analysis on morphologic features of the peak-cluster depression in Qiubei, Southeast Yunnan[J]. CARSOLOGICA SINICA, 2010, 29(3): 239-245. doi: 10.3969/j.issn.1001-4810.2010.03.004
Citation: WANG Di, XU Mo, QI Ji-hong, ZHANG Qiang. Analysis on morphologic features of the peak-cluster depression in Qiubei, Southeast Yunnan[J]. CARSOLOGICA SINICA, 2010, 29(3): 239-245. doi: 10.3969/j.issn.1001-4810.2010.03.004

Analysis on morphologic features of the peak-cluster depression in Qiubei, Southeast Yunnan

doi: 10.3969/j.issn.1001-4810.2010.03.004
  • Received Date: 2010-04-12
  • Publish Date: 2010-09-25
  • Qiubei peak-cluster depression in southeast Yungui Plateau, about 40km2 in area , is chosen as the sample region for karst landform fractal geometry analysis. Statistical method is used to analyze the characteristic parameters of 48 karst depressions and peaks; fractal theory is chosen to calculate fractal dimensions at different elevation contours and surface water network. The results indicate that: (1) the average area of the depressions is 0.8 km2, the mean boundary-namber is 5.6 and the average perimeter is 3.4km; (2) depressions grow in breadth and in depth near-synchronously, and the development of corrosion surface is restricted by the elevation of initial surface; (3) fractal characteristics of peak-cluster depression are well response to the karst evolution, and the average fractal dimension of contour in limestone region and non- limestone region is 1.30 and 1.16 respectively, and the dimension of surface water network is 1.07, which reflect topographic change are complicate, underground hydrographic net are quite developed and the relative degree of karst development is high in this karst region; (4) the karst in Qiubei is in the young or mature stage, and will continue to develop slowly.

     

  • loading
  • [1]
    王妍, 刘洪斌, 武伟等. 基于GIS的三峡库区地貌形态信息统计分析[J]. 测绘科学, 2006: 31(2): 93-95.
    [2]
    胡宁, 傅瓦利, 马志敏等. 岩溶石漠化山地不同退耕模式土壤抗蚀性及其与结构体分形关系研究[J].中国岩溶, 2008, 27(2): 115-121.
    [3]
    朱德浩, 谭鹏家,房玲昌. 对峰丛洼地形态和演化的几点认识——以广西几个地区为例[C].喀斯特地貌与洞穴.科学出版社, 1985: 57-64.
    [4]
    宋林华, 房金福.喀斯特洼地的分形特性研究[J].地理研究, 1995,14(01): 8-14.
    [5]
    蒋忠信.黔西南高原区峰丛洼地的形态特征与发育规律[J].热带地理, 1997,17(3): 267-274.
    [6]
    胡章喜, 沈继方.岩溶形态系统的分形特征及其机理探讨[J].地球科学——中国地质大学学报, 1994, 19(1): 102-107.
    [7]
    陈颙, 陈凌. 分形几何学[M].北京: 地震出版社, 1998.
    [8]
    朱德浩.桂林地区峰丛洼地的形态量计及其演化[J].中国岩溶, 1982: 127-134.
    [9]
    倪化勇. 泥石流流域地貌形态的统计分形[J]. 水土保持研究, 2006,13(6): 92-93.
  • 加载中

Catalog

    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索

    Article Metrics

    Article views (2162) PDF downloads(1505) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return