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《Journal of the Chinese Society of Rare Earths》 2014-01
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Geochemical Characteristics and Granularity Effect of Rare Earth Elements in Soils from Iron Ore Areas Along The Chao River

Qin Fei;Li Qian;Ji Hongbing;Feng Jinguo;Li Cai;Civil & Environment Engineering School,University of Science & Technology Beijing;National Environment & Energy International Cooperation,University of Science & Technology Beijing;The Key Laboratory of Metropolitan Eco-Environmental Processes,College of Resource Environment and Tourism,Capital Normal University;Beijing Geo-Engineering Design and Research Institute;  
This paper researched and evaluated geochemical characteristics and granularity effect of Rare Earth elements in the bulk and size graded soils from iron ore areas along the Chao River. The concentrations of 15 REEs,i. e. La,Ce,Pr,Nd,Sm,Eu, Gd,Tb,Dy,Ho,Er,Tm,Yb,Lu and Y were evaluated by inductively coupled plasma mass spectrometry( ICP-MS). The result showed that the metal concentrations in soil samples,whose mean values changed obviously,exceed those of background levels in mainland China. The trend of the relationship between the concentrations of REEs and size grade was consistent, namely,the concentration of REEs increased with decrease of particle size. With standardization of the soils by six Leedy chondrite average of Masuda( 1973),the distribution patterns of REEs was consistent,being the right dip type of light rare earth enrichment,Eu negative anomaly obviously,Ce slightloss,which is mainly controlled by the terrigenous. The change characteristics of REE were closely related to the adsorption of clay minerals and mineral composition of size grade. This conclusion provides a scientific basis for rare earth elements being selected as tracers. It also provides reference for the further study of REEs in various particle size fractions internationally.
【Fund】: 国家自然科学基金(41173113);; 中国科学院百人计划项目(2010)
【CateGory Index】: P595
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