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喀斯特地区黄壤和石灰土剖面化学组成变化与风化成土过程
引用本文:刘文景,涂成龙,郎赟超,冯家毅,李龙波,汪齐连,刘丛强.喀斯特地区黄壤和石灰土剖面化学组成变化与风化成土过程[J].地球与环境,2010,38(3).
作者姓名:刘文景  涂成龙  郎赟超  冯家毅  李龙波  汪齐连  刘丛强
作者单位:1. 中国科学院,地球化学研究所,环境地球化学国家重点实验室,贵阳,550002;中国科学院,研究生院,北京,10049
2. 中国科学院,地球化学研究所,环境地球化学国家重点实验室,贵阳,550002
基金项目:国家重点基础研究发展计划(973计划)项目,国家自然科学基金创新群体项目,中科院西部之光项目 
摘    要:对西南喀斯特地区典型黄壤和石灰土剖面土壤主量和微量元素组成变化特征进行了研究,提供了有关岩石风化和土壤形成过程的信息。所研究的土壤相对于上地壳普遍富集P和Mn,而亏损Na、K、Ca、Mg元素。与黄壤相比,石灰土具有较高含量的K、Rb和较低含量的Sr元素,同时具有较高Th/Ta,Rb/Sr比值和CIA的特征,指示两类土壤成土母质的差别和石灰土较强的风化程度。不同地区同种类型土壤以及同一地区不同类型土壤的化学组成具有显著差别,反映了不同区域和不同类型土壤在成土母质、风化成土过程和程度上的差异。

关 键 词:喀斯特地区  黄壤剖面  石灰土剖面  主量元素  微量元素成土过程

Major and Trace Element Compositions of Yellow and Limestone Soils in the Karst Area of Southwest China:Implications for Weathering and Soil-formation Processes
LIU Wen-jing,TU Cheng-long,LANG Yun-chao,FENG Jia-yi,LI Long-bo,WANG Qi-lian,LIU Cong-qiang.Major and Trace Element Compositions of Yellow and Limestone Soils in the Karst Area of Southwest China:Implications for Weathering and Soil-formation Processes[J].Earth and Environment,2010,38(3).
Authors:LIU Wen-jing  TU Cheng-long  LANG Yun-chao  FENG Jia-yi  LI Long-bo  WANG Qi-lian  LIU Cong-qiang
Institution:LIU Wen-jing1,2,TU Cheng-long1,LANG Yun-chao1,FENG Jia-yi1,LI Long-bo1,WANG Qi-lian1,LIU Cong-qiang1 (1. State Key Laboratory of Environmental Geochemistry,Institute of Geochemistry,CAS,Guiyang 550002,China,2. Graduate University of Chinese Academy of Sciences,Beijing,100049,China)
Abstract:Typical yellow and limestone soil profiles in the karst areas of Southwest China,were studied for major and trace element contents,which provides the information about the crustal weathering and soil formation process. The soils studied showed that the contents of P and most Mn in the samples are higher than the average values of upper continental crust (UCC),while the contents of Na,K,Ca,Mg are lower. Compared with the yellow soil profiles,the limestone soil profiles have higher contents of K and Rb,but lo...
Keywords:karst area  yellow soil profile  limestone soil profile  major element  trace element  soil-formation process  
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