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《Geochimica》 2004-01
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Major element geochemistry of sediments from Chinese and Korean rivers

YANG Shou-ye 1 ,Jung Hoi-soo 2 ,LI Cong-xian 1 ,Lim Dong-il 2 (1.Laboratory of Marine Geology,Tongj i University,Shanghai 20009 2,China;2.Korea Ocean Research and Developmen t Institute,Ansan,Seoul 4 25-600,Korea)  
Compositions of major elements of Chinese and Korean river sedimen ts were characterized on the basis of identical sample collections,processes an d measurements.The Korean r iver sediments have much lower TIC,C a and carbona te contents than Chinese river sediments,whereas the Changjiang sediment is cha racterized by hi gh Ti content and the Huanghe sediment by h igh Ca,Na and car bonate contents.The acid-leachable fractions of P,Ca,Fe and Mg account for 30%~66%of the bulk contents of the Korean river sedim ents,whereas K,Al and Ti primarily reside in the residual fra ctions.The Korean river sediments a re mainly sourced from Jurassic-Cre taceous granite which underwent fairly s tro ng chemical weathering,and the drainage basins lack carbonate rocks,which results in the very low Ca contents in river sediments.It is suggested that bul k Ca composition is not appropriate for discriminating Chinese and Korean r iver sediments because of biogenic C aCO 3 in marine environment,whereas non-carbonate-bound Ca  contents and ratios of K/Ca  and Al/Ca  can discriminate sediment sources i n view of their stable behaviors and dis tinct compositions between these river se diments.
【Fund】: 国家自然科学基金(49976016;40206008);; 韩国自然科学和科技部基金资助项目(KOSEF和KIST)
【CateGory Index】: P595
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