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《Chinese Journal of Geophysics》 2003-01
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RELATIONSHIP BETWEEN IRON OXIDES AND MAGNETIC PROPERTIES IN INTERTIDAL SEDIMENTS OF THE YANGTZE ESTUARY,CHINA

ZHANG WEIGUO1 YU LIZHONG1 LU MIN2 l State Key Laboratory of Estuarine and Coastal Research,East China Normal University,Shanghai 200062,China 2 Department of Geography,East China Normal University,Shanghai 200062,China  
DCB (Dithionite-Citrate-Carbonate) and AOD (Ammonium Oxalate in the Dark) extractions as well as magnetic measurements were conducted on intertidal sediments of the Yangtze estuary,China.The results are used to explore the relationship between iron oxides and magnetic properties,estimate different iron oxide pools semi-quantitatively,and investigate the impact of DCB extraction on the variations of magnetic properties.It is revealed that magnetic susceptibility and SIRM(Saturation Isothermal Remanent Magnetization)show significant correlations with DCB-and AOD-extractable iron oxides.A semi-quantitative estimation reveals a dominance by amorphous iron oxides,with magnetite occupies only 1 2 percent of the total iron oxides.The efficiency of DCB extraction relies on the grain size as well as the content of magnetic minerals.DCB extraction removes a large fraction of fine-grained (2μm) iron oxides.Coame magnetite can also be dissolved by DCB extraction.The differences between pre-and post-DCB values of S -100 and HIRM (Hard Isothermal Remanent Magnetization)suggest that anti-ferromagnetic iron oxides are more abundant than magnetite in the clay fraction (2μm).
【Fund】: 国家自然科学基金 (40 0 0 1 0 2 0、40 1 31 0 2 0 );; 上海市科委青年科技启明星项目 (0 1QCl40 1 6);; 上海市重点学科项目 .
【CateGory Index】: P736.2
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