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重庆喀斯特地区土地覆被类型对土壤特征的影响
引用本文:李阳兵,谢德体,王世杰,WEI Chaofu.重庆喀斯特地区土地覆被类型对土壤特征的影响[J].地理学报(英文版),2006,16(2):143-154.
作者姓名:李阳兵  谢德体  王世杰  WEI Chaofu
作者单位:1. School of Geography and Biology Science,Guizhou Normal University,Guiyang 550001,China; 2. Resources and Environment College,Southwest Agricultural University,Chongqing 400716,China;3. State Key Laboratory of Environmental Geochemistry,Institute of Geochemistry,CAS,Guiyang 550002,China
基金项目:Supported by the key plan of Chongqing Science and Technology Committee(6759,7355)
摘    要:1 Introduction The karst region of Southwest China, with Guizhou Province as the center, extends across Yunnan Province, Guangxi Zhuang Autonomous Region, Sichuan Province, Chongqing, western Hunan Province, Hubei Province, and Guangdong Province, coveri…

关 键 词:重庆  喀斯特地区  土地覆被类型  土壤特征
收稿时间:2005-10-14
修稿时间:2005-10-142005-12-22

Impact of land cover types on the soil characteristics in karst area of Chongqing
Yangbing Li,Deti Xie,Shijie Wang,Chaofu Wei.Impact of land cover types on the soil characteristics in karst area of Chongqing[J].Journal of Geographical Sciences,2006,16(2):143-154.
Authors:Yangbing Li  Deti Xie  Shijie Wang  Chaofu Wei
Institution:1. School of Geography and Biology Science, Guizhou Normal University, Guiyang 550001, China
2. Resources and Environment College, Southwest Agricultural University, Chongqing 400716, China
3. State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, CAS,Guiyang 550002, China
Abstract:The 26 plots including natural forestland, secondary forestland, shrub-grassland, sloping cropland, artificial forest and abandoned field, were selected to discuss the impact of land cover on the soil characteristics in the three karst districts of Chongqing. The results showed that: (1) After the vegetation turned into secondary vegetation or artificial vegetation, or reclamation, soil physical properties would be degraded. In the surface-layer soil of sloping cropland, the contents of > 2 mm water-stable aggregates decreased obviously with apparent sandification. (2) The contents of soil organic matter and total nitrogen are controlled completely by vegetation type and land use intensity. The increasing trend is rather slow in the early days when over-reclamation is stopped and the land is converted to forest and pasture. (3) Herbaceous species increase and woody plants species decrease with the increase of land use intensity, therefore, the soil seed banks degrade more seriously. (4) The soil degradation index has been set up to describe the relative soil degradation degree under the conditions of different vegetation types. (5) Land cover has a significant effect on karst soil characteristics, land degradation in the karst ecosystem is essentially characterized by the different degradation of soil functions that serve as water banks, nutrient banks and soil seed banks.
Keywords:karst ecosystem  vegetation evolution  soil degradation  soil seed bank  soil-land ecology  Chongqing  
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