• Included in CSCD
  • Chinese Core Journals
  • Included in WJCI Report
  • Included in Scopus, CA, DOAJ, EBSCO, JST
  • The Key Magazine of China Technology
Volume 32 Issue 1
Mar.  2013
Turn off MathJax
Article Contents
LIU Chao, WU Hong. Study on localization of temporal and spatial variation in karst peak cluster in Guilin[J]. CARSOLOGICA SINICA, 2013, 32(1): 100-107. doi: 10.3969/j.issn.1001-4810.2013.01.015
Citation: LIU Chao, WU Hong. Study on localization of temporal and spatial variation in karst peak cluster in Guilin[J]. CARSOLOGICA SINICA, 2013, 32(1): 100-107. doi: 10.3969/j.issn.1001-4810.2013.01.015

Study on localization of temporal and spatial variation in karst peak cluster in Guilin

doi: 10.3969/j.issn.1001-4810.2013.01.015
  • Received Date: 2012-08-03
  • Publish Date: 2013-03-25
  • In order to discuss the impact of local eco environment changes on the entire eco environment in Guilin, 8 zones of peak cluster are selected as the study object from Liucunnan to Jiedi along the north bank of the Lijiang River(No.1~No.8), localization extraction and temporal and spatial variation analysis have been done for the RS habitat index, NDVI and the greenness component ( TC2) of Tasseled Cap in the selected 8 zones by means of localized and quantitative RS in region of interest (ROI) technique with the data come from TM of Landsat 5 in 1986, 1991 and 2006 and other geology and geography information. The results show that,the NDVI and TC2 indexes at the peak clusters are the highest in 2006 and the eco environment is the best; it takes second place in 1986 and worst in 1991 proving the habitat is blighted due to the ignoring of environmental protection during economic develops rapidly in Guilin at the end of the 1980’s and the beginning of 1990’s in the 20th century, however, it is improved obviously in the 21st century with some patches or bands assuming high eco environment rank showed by NDVI and TC2 (i.e. NDVI index>0.4 and TC2 index>20) , which tends to enlarging to the whole area from 1991. The values of NDVI and TC2 are of the tendency low in 1991 and high in 1986 and 2006 in the same region but different time, and there is also difference in NDVI and TC2 value at the same time but different region. From good to bad relationships, the arrangement is,No.5>No.4>No.3>No.8>No.7>No.6>No.2>No.1.

     

  • loading
  • [1]
    袁道先,朱德浩,翁金桃,等..中国岩溶学(第一版)[M].北京:地质出版社,1994.
    [2]
    朱学稳,汪训一,朱德浩,等.桂林岩溶地貌与洞穴研究(第一版)[M].北京:地质出版社,1988.
    [3]
    陈文俊.桂林岩溶地质背景[C]//第二届岩溶学术会议论文集编写组.中国地质学会第二届岩溶学术会议论文集(第一版).北京:科学技术出版社,1982:446-457.
    [4]
    高振西.喀斯特地形论[J].地质评论,1936,1(4):437-450.
    [5]
    李粹中.桂林近郊的喀斯特[C]//水文工程地质论文集编写组.水文工程地质论文集(第一集).北京:科学出版社,1961:311-318.
    [6]
    翁金桃.桂林岩溶与碳酸盐岩[M].重庆:重庆出版社,1987.
    [7]
    邓自强,林玉石,张美良,等.桂林岩溶与地质构造[M].重庆:重庆出版社,1987.
    [8]
    杨奇勇,蒋忠诚,马祖陆,等.基于地统计学和遥感的岩溶区石漠化空间变异特征[J].农业工程学报,2012,28(4):243-247.
    [9]
    杨树文,谢飞,冯光胜,等.基于SPOT5图像的岩溶地貌单元自动提取方法[J].国土资源遥感,2012,2(93):56-60.
    [10]
    梁福源,石玉若,George A Brook.利用ASTER卫星立体像对提取喀斯特数字地形模型——以广西大化高峰丛深洼地喀斯特地貌为例[J].中国岩溶,2011,30(2):234-242.
    [11]
    林俊清.卫星像片上喀斯特地貌及水系的解译[J].贵州科学,2000,18(3):119-224.
    [12]
    李新程.岩溶峰丛区生态环境定域动力学模型[D].桂林理工大学,2012.
    [13]
    贾志强.岩溶峰丛区定域生境指标遥感反演与动态分析研究——以广西6地区为例[C]//单杰,张继贤.第十八届中国遥感大会论文集.北京:科学出版社,2012:826-835.
    [14]
    邓自强,林玉石,张美良,等.桂林岩溶洼地和洞穴发生、发展的构造控制剖析[J].中国岩溶,1987,6(2):137-148.
    [15]
    梁保平,李艺,陈可宙.桂林市NDVI、地表温度的地物特征及相关性研究[J].遥感技术与应用,2012,27(3),430-435.
    [16]
    赵英时.美国中西部沙山地区环境变化的遥感研究[J].地理研究,2001,2(20):213-218.
    [17]
    李辉霞,李森,周红艺.粤北典型岩溶山区土地石漠化程度遥感评价[J].水土保持通报,2011,6(31):155-159.
    [18]
    陈超,江涛,刘祥磊.基于缨帽变换的遥感图像融合方法研究[J].测绘科学,2009,3(34):105-163.
  • 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 (2437) PDF downloads(1220) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return