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《Chinese Journal of Geophysics》 1999-06
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MAGNETIC MEASUREMENT CHARACTERISATION OF RED EARTH PROFILE IN EASTERN CHINA AND ITS ENVIRONMENTAL IMPLICATIONS

LU SHENG-GAO;DONG RUI-BIN;YU JIN-YAN(College of Environment and Natural Resources, Zhejiang University, Hangzhou 310029)ZHANG WEI-GUO;YU LI-ZHONG(National Key Laboratory of River Mouth and Coast, East China Normal University Shanghai 200062)  
Environmental magnetism parameters, including magnetic susceptibility (X),anhysteretic remanent magnehzation (ARM), saturation isothermal remanentmagnetization (SIRM), Frequency dependent susceptibility (Xfd), magnetization parameters (F+xmT and demagnetization parameters (F-xmT), have been measured on a redearth profile from eastern China. The variation curves of ferrimagnetic mineralconcentration, mineralogy assemblages and grain size of red earth profile with depthbefore and after iron oxides were removed by dithionite-citrons system buffered withsodium bicarbonate (DCB) were illustrated. On the basis of the magnetic properties ofred earth, three distinctive stratigraphic horizons have been identified. The spheruliticmagnetic particles were separated by magnetic separation method, indicating that thecontribution of magnetism in red earth is maghemite, hematite and goethite. Resultssuggested that enhancement of magnetism and shift in magnetic domain andmineralogy assemblage are correlated with pedogenic environments. Frequencydependent susceptibility and the fraction of magnetic susceptibility that is removed byDCB treatment are attributed to the pedogenic ferrimagnetic component suggestingthat they are index of soil development degree. Thus, magnetism of red earth, aneasily measured soil attribute, can be used to evaluate the environmental change ofQuaternary in southern China.
【Fund】: 国家自然科学基金!49301010
【CateGory Index】: X144
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