Analysis on Spatial Distribution Feature of Landscape of Karst RockyDesertification in Liuzhi Special Zone of GuiZhou

MA Shi-bin,ZHANG Yong-rong AN Yu-lun,ZHANG Yue-hong

Journal of Changjiang River Scientific Research Institute ›› 2015, Vol. 32 ›› Issue (12) : 30-35.

PDF(1857 KB)
PDF(1857 KB)
Journal of Changjiang River Scientific Research Institute ›› 2015, Vol. 32 ›› Issue (12) : 30-35. DOI: 10.11988/ckyyb.20140529
WATERSOILCONSERVATIONANDECOCONSTRUCTION

Analysis on Spatial Distribution Feature of Landscape of Karst RockyDesertification in Liuzhi Special Zone of GuiZhou

  • MA Shi-bin 1,2,3,ZHANG Yong-rong1,2 AN Yu-lun 3, ZHANG Yue-hong 4
Author information +
History +

Abstract

In order to obtain spatial distribution and evolution characteristics of rocky desertification,we used topographic position index and distribution index,as well as remote sensing and GIS technologies.Liuzhi special zone of Guizhou province from 1990 to 2010 was taken as an example.Topographic position can be divided into 3 intervals according to elevation and slope:low interval,middle interval,and high interval,and there are 6 levels for rocky desertification:none,potential,slight,moderate,severe,and extra severe.The results indicate that:Firstly,none,potential,slight,and extra severe rocky desertification regions are mainly located in the high interval,whereas moderate and severe rocky desertification regions are mainly located in the middle interval,with none rocky desertification regions in the low interval.Subsequently,the distribution of topographic position interval varied with different causes such as human activities and nature which lead to rocky desertification.Potential,slight,and moderate rocky desertification regions caused by human activities are mainly located in low and middle intervals of topographic position,whereas severe and extra severe rocky desertification regions caused by nature are distributed in high interval.Furthermore,the distribution of rocky desertification is easy to be seen in middle interval of topographic position.Finally,more attention should be paid to low and middle intervals, where the levels are potential,slight,moderate,or severe, whereas natural ecological restoration should be highlighted in the severe and extra severe rocky desertification areas in the high interval driven by natural factors.

Key words

Karst rocky desertification / spatial feature / topographic position index / distribution index / remote sensing data

Cite this article

Download Citations
MA Shi-bin,ZHANG Yong-rong AN Yu-lun,ZHANG Yue-hong. Analysis on Spatial Distribution Feature of Landscape of Karst RockyDesertification in Liuzhi Special Zone of GuiZhou[J]. Journal of Changjiang River Scientific Research Institute. 2015, 32(12): 30-35 https://doi.org/10.11988/ckyyb.20140529

References

[1] 杨青青,王克林,岳跃民.桂西北石漠化空间分布及尺度差异[J].生态学报,2009,29(7):3629-3640.(YANG Qing-qing,WANG Ke-lin,YUE Yue-min.Spatial Distribution of Rocky Desertification and Its Difference Between Scales in Northwest Guangxi[J].Acta Ecologica Sinica,2009,29(7):3629-3640.(in Chinese))
[2] 杨胜天,王 冰,王玉娟.喀斯特地区水土流失遥感监测现状与发展趋势[J].水土保持通报,2007,27(1):62-66.(YANG Sheng-tian,WANG Bing,WANG Yu-juan.Trend and State of Remote Sensing Monitoring of Soil and Water Loss in Karst Region[J].Bulletin of Soil and Water Conservation,2007,27(1):62-66.(in Chinese))
[3] YUAN D X.Rock Desertification in the Subtropical Karst of South China[J].Zeitschrift für Geomorphologie,1997,108:81-90.
[4] WANG S J,LIU Q M,ZHANG D F,et al.Karst Rocky Desertification in Southwestern China:Geomorphology,Land Use,Impact and Rehabilitation[J].Land Degradation & Development,2004,15(2):115-121.
[5] 李阳兵,白晓永,周国富,等.中国典型石漠化地区土地利用与石漠化的关系[J].地理学报,2006,61(6):624-632.(LI Yang-bing,BAI Xiao-yong,ZHOU Guo-fu,et al.The Relationship of Land Use with Karst Rocky Desertification in A Typical Karst Area,China[J].Acta Geographica Sinica,2006,61(6):624-632.(in Chinese))
[6] 熊康宁,黎 平,周忠发,等.喀斯特石漠化的遥感-GIS典型研究[M].北京:地质出版社,2002.(XIONG Kang-ning,LI Ping,ZHOU Zhong-fa,et al.Remote Sensing and GIS-based Studies on Karst Rocky Desertification:An Example of Guizhou Province[M].Beijing:Geological Publishing House,2002.(in Chinese))
[7] 张勇荣,周忠发,马士彬,等.基于Markov的石漠化景观演变特征分析与预测[J].长江科学院院报,2015,32(1):52-69.(ZHANG Yong-rong,ZHOU Zhong-fa,MA Shi-bin,et al.Analysis and Forecast of the Evolution Features of Rocky Desertification Landscape by Markov Model[J].Journal of Yangtze River Scientific Research Institute,2015,32(1):52-69.(in Chinese))
[8] 喻 红,曾 辉,江子瀛.快速城市化地区景观组分在地形梯度上的分布特征研究[J].地理科学,2001,21(1):64-69.(YU Hong,ZENG Hui,JIANG Zi-ying.Study on Distribution Characteristics of Landscape Elements along the Terrain Gradient[J].Scientia Geographica Sinica,2001,21(1):64-69.(in Chinese))
[9] 马士彬,张勇荣,安裕伦.山区城市土地利用动态空间分布特征——以贵州省六盘水市为例[J].自然资源学报,2010,27(3):489-496.(MA Shi-bin,ZHANG Yong-rong,AN Yu-lun.Spatial Pattern of Urban Land Use in the Mountain Area:A Case Study of Liupanshui in Guizhou Province[J].Journal of Natural Resources,2010,27(3):489-496.(in Chinese))
[10]陈利顶,杨 爽,冯晓明.土地利用变化的地形梯度特征与空间扩展——以北京市海淀区和延庆县为例[J].地理研究,2008,27(6):1225-1235.(CHEN Li-ding,YANG Shuang,FENG Xiao-ming.Land Use Change Characteristics along the Terrain Gradient and the Spatial Expanding Analysis:Case Study of Haidian District and Yanqing County,Beijing[J].Geographical Research,2008,27(6):1225-1235.(in Chinese))
PDF(1857 KB)

Accesses

Citation

Detail

Sections
Recommended

/