期刊文献+

Vegetation Spatial Heterogeneity of Different Soil Regions in Inner Mongolia, China

Vegetation Spatial Heterogeneity of Different Soil Regions in Inner Mongolia, China
原文传递
导出
摘要 The vegetation spatial heterogeneity and ecological characteristics in different soil regions were analyzed by surveying the vegetation in 12 different soil regions of Inner Mongolia, China, including coniferous-broadleaf deciduous forests, shrub, grassland, and desert regions with 1122 large 2 cm × 2 cm quadrats (actual size 30 km × 30 km, referred to as L-quadrat hereafter) in about 1.18 million km2. Each L-quadrat was divided into four small 1 cm × 1 cm quadrats (actual size 15 km × 15 km, S-quadrat). The vegetation was analyzed based on the beta-binomial distribution to describe the frequency of occurrence and spatial heterogeneity for each kind of vegetation. The weighted average of the heterogeneity of all vegetation in the same soil region provides a measure of the soil regional landscape level heterogeneity which describes the spatial complexity of the regional landscape composition of the existing vegetation. Comparison of the vegetation characteristics in the 12 soil regions shows that, the calcic gray soil has the highest average vegetation type per quadrat. The largest soil region is calcic chestnut soil and has the most vegetation types. Every soil region has its own dominant vegetation sequence which dominates in occurrence and dominant vegetation types which dominates in spatial heterogeneity. For the Inner Mongolian vegetation, the weighted average of the heterogeneity is 0.60 and the vegetation diversity index is 4.47. The vegetation spatial heterogeneity and ecological characteristics in different soil regions were analyzed by surveying the vegetation in 12 different soil regions of Inner Mongolia, China, including coniferous-broadleaf deciduous forests, shrub, grassland, and desert regions with 1122 large 2 cm × 2 cm quadrats (actual size 30 km × 30 km, referred to as L-quadrat hereafter) in about 1.18 million km2. Each L-quadrat was divided into four small 1 cm × 1 cm quadrats (actual size 15 km × 15 km, S-quadrat). The vegetation was analyzed based on the beta-binomial distribution to describe the frequency of occurrence and spatial heterogeneity for each kind of vegetation. The weighted average of the heterogeneity of all vegetation in the same soil region provides a measure of the soil regional landscape level heterogeneity which describes the spatial complexity of the regional landscape composition of the existing vegetation. Comparison of the vegetation characteristics in the 12 soil regions shows that, the calcic gray soil has the highest average vegetation type per quadrat. The largest soil region is calcic chestnut soil and has the most vegetation types. Every soil region has its own dominant vegetation sequence which dominates in occurrence and dominant vegetation types which dominates in spatial heterogeneity. For the Inner Mongolian vegetation, the weighted average of the heterogeneity is 0.60 and the vegetation diversity index is 4.47.
出处 《Tsinghua Science and Technology》 SCIE EI CAS 2007年第4期413-423,共11页 清华大学学报(自然科学版(英文版)
基金 Partly supported by the Japan Society for the Promotion of Science (No. L-02711)
关键词 spatial heterogeneity soil region beta-binomial distribution VEGETATION Inner Mongolia spatial heterogeneity soil region beta-binomial distribution vegetation Inner Mongolia
  • 相关文献

参考文献12

  • 1Masae Shiyomi,Jin Yoshimura.Measures of spatial heterogeneity for species occurrence or disease incidence with finite-counts[J].Ecological Research.2000(1)
  • 2G. P. Patil,W. M. Stiteler.Concepts of aggregation and their quantification: A critical review with some new results and applications[J].Researches on Population Ecology.1973(1)
  • 3Kawamura K,Akiyama T,Watanabe O, et al.Estimation of aboveground biomass in Xilinggol steppe, Inner Mongolia Using NOAA/NDVI[].Grassland Science.2003
  • 4Okamoto C,Nakamura M,Kabata K, et al.Seasonal changes in the aboveground phytomass of a Stipa bai- calensis community in Northeast China[].Grassland Sci- ence.2000
  • 5Kawanabe S,Nan Y H,Oshida T, et al.Degradation of grassland in Keerqin Sandland, Inner Mongolia, China[].Grassland Science.1998
  • 6Akiyama T,Kawamura K.Grassland degradation in China: Methods of monitoring, management and restoration[].Grassland Science.2007
  • 7Nakamura T,Go T,Yunna W,Hayashi I.Effects of grazing on the composition of grasslands in Baiyinxile, Xilingole, Inner Mongolia[].Grassland Science.2000
  • 8Huang D,Shiyomi M.Spatial heterogeneity of vegetation in the center of Inner Mongolia, China[].Grassland Science.2004
  • 9Yong Shipeng,Li Bo,Cui Haiting.Series Resources Maps of Inner Mongolia Autonomous Region: Vegetation[]..1991
  • 10Li Tianjie,Cai Chengming.Series Resources Maps of In- ner Mongolia Autonomous Region: Soil[]..1991

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部