首页 | 本学科首页   官方微博 | 高级检索  
     检索      

中国黄土高原黄土-古土壤序列的红度对古气候的指示意义
作者姓名:HU Xue-Feng  LU Hua-Yu  XU Qi  DONG Li-Jing  HU Xing
作者单位:Department of Environmental Science and Engineering, Shanghai University, Shanghai 200072 (China). E-mail: xfhu@mail.shu.edu.cn;State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710075 (China);Department of Environmental Science and Engineering, Shanghai University, Shanghai 200072 (China). E-mail: xfhu@mail.shu.edu.cn;Department of Environmental Science and Engineering, Shanghai University, Shanghai 200072 (China). E-mail: xfhu@mail.shu.edu.cn;Department of Environmental Science and Engineering, Shanghai University, Shanghai 200072 (China). E-mail: xfhu@mail.shu.edu.cn
基金项目:*1Project supported by the National Natural Science Foundation of China (No.40101013) and the Outstanding Overseas Chinese Scholars Fund of the Chinese Academy of Sciences (No.2003-1-7).
摘    要:Comparisons of red ratings (RR) with Fed, Fed/Fet, clay content, and magnetic susceptibility (x) of two loess-paleosol sequences at Luochuan and Lingtai on China's Loess Plateau were conducted to study the possible relationship between RR and pedogenic degrees of the two loess-paleosol sequences, and to discuss whether the RR could become new paleo-climatic indicators. Results showed that the RR of the two loess-paleosol sequences had positive, highly significant (P < 0.01) correlations with: 1) citrate-bicarbonate-dithionite (CBD) extracted iron (Fed), 2) ratios of CBD extracted iron to total iron (Fed/Fet), 3) clay (< 2 μm), and 4) magnetic susceptibility (x). This suggested that the RR of these loess-paleosol sequences could indicate degrees of loess weathering and pedogenesis and were potential paleo-climatic proxies. The strong correlations of RR to Fed and x also implied that during pedogenic processes, pedogenic hematite in loess and paleosols were closely related to the amount of total secondary iron oxides and pedogenic ferrimagnetic minerals (predominantly maghemite).

关 键 词:hematite    loess-paleosol  sequences    Loess  Plateau    magnetic  susceptibility    red  ratings

Red Ratings for Loess-Paleosol Sequences on China's Loess Plateau and Their Paleo-Climatic Implications
HU Xue-Feng,LU Hua-Yu,XU Qi,DONG Li-Jing,HU Xing.Red Ratings for Loess-Paleosol Sequences on China''s Loess Plateau and Their Paleo-Climatic Implications[J].Pedosphere,2004,14(4):433-440.
Authors:HU Xue-Feng  LU Hua-Yu  XU Qi  DONG Li-Jing and HU Xing
Institution:Department of Environmental Science and Engineering, Shanghai University, Shanghai 200072 (China). E-mail: xfhu@mail.shu.edu.cn;State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710075 (China);Department of Environmental Science and Engineering, Shanghai University, Shanghai 200072 (China). E-mail: xfhu@mail.shu.edu.cn;Department of Environmental Science and Engineering, Shanghai University, Shanghai 200072 (China). E-mail: xfhu@mail.shu.edu.cn;Department of Environmental Science and Engineering, Shanghai University, Shanghai 200072 (China). E-mail: xfhu@mail.shu.edu.cn
Abstract:
Keywords:hematite  loess-paleosol sequences  Loess Plateau  magnetic susceptibility  red ratings
本文献已被 万方数据 等数据库收录!
点击此处可从《土壤圈》浏览原始摘要信息
点击此处可从《土壤圈》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号