[1]LI Yang-bing,WANG Shi-jie,ZHOU Meng-wei,et al.Relationship Between Karst Rocky Desertification Distribution and Slope Under Different Spatial Scales[J].Research of Soil and Water Conservation,2009,16(05):70-72,77.
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Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume:
16
Number of periods:
2009 05
Page number:
70-72,77
Column:
Public date:
2009-10-20
- Title:
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Relationship Between Karst Rocky Desertification Distribution and Slope Under Different Spatial Scales
- Author(s):
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LI Yang-bing1,3, WANG Shi-jie2, ZHOU Meng-wei2, CHENG An-yun2, LI Wei-hai1
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1. School of Geography and Environment Science, Guizhou Normal University, Guiyang 550001, China;
2. National Key Laboratory of Environmental Geochemistry, Geochemistry Institute of Chinese Academy of Science, Guiyang 550002, China;
3. College of Geography Science, Chongqing Normal University, Chongqing 400047, China
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- Keywords:
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karst rocky desertification; slope; spatial scale
- CLC:
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P642.25;X171.1
- DOI:
-
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- Abstract:
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Based on the image of SPOT5 in 2005,karst rocky desertification landscape patterns in Boluo area was classified as: no,latent,slight,moderate,strong,and extremely strong karst rocky desertification types.Furthermore,this paper discussed the relationship between karst rocky desertification and slope.The results show that: the karst rocky desertification land gathered in the slope range of 15° to 25° in Wangjiazhai catchments,and located in areas with slope <5° or 15°~25°.But the occurrence ratio of karst rocky desertification of areas with slope >25° is the biggest in larger spatial scales.The slope range of areas which karst rocky desertification located increases with the spatial scale-up.So,the conclusions derived from macro-scale studies should not apply to the comprehensive melioration the karst rocky desertification in small spatial scales.