古地理学报 ›› 2016, Vol. 18 ›› Issue (5): 865-878. doi: 10.7605/gdlxb.2016.05.066

• 地球化学及沉积环境 • 上一篇    下一篇

中国南方网纹红土元素地球化学特征及其对网纹化过程的指示意义*

徐传奇1, 廖富强1, 2, 贾玉连1, 2, 黄思源1, 连丽聪1, 凌超豪1, 龙进1   

  1. 1 江西师范大学地理与环境学院,江西南昌 330022;
    2 鄱阳湖湿地与流域研究教育部重点实验室,江西南昌 330022
  • 收稿日期:2015-10-15 修回日期:2016-02-01 出版日期:2016-10-01 发布日期:2016-10-01
  • 通讯作者: 贾玉连,男,1971年生,江西师范大学教授,主要从事自然地理学与第四纪环境研究。E-mail: 1476288868@qq.com。
  • 作者简介:徐传奇,男,1990年生,江西师范大学硕士研究生,主要从事自然地理学与第四纪环境研究。E-mail: 834630747@qq.com。
  • 基金资助:
    *国家自然科学基金项目(编号:41262007)、江西省重大生态安全问题监控协同创新中心项目(编号:JXS-EW-00)与鄱阳湖湿地与流域研究教育部重点实验室(江西师范大学)开放基金项目(编号:ZK2013003)联合资助

Element geochemical characteristics of the reticulate red clay in southern China and its significance for the formation proccess of reticulated mottles

Xu Chuanqi1, Liao Fuqiang1, 2, Jia Yulian1, 2, Huang Siyuan1, Lian Licong1, Ling Chaohao1, Long Jin1   

  1. 1 Department of Geography and Environment,Jiangxi Normal University,Nanchang 330022,Jiangxi;
    2 Ministry Education Key Laboratory of Poyang Lake Wetland and Watershed Research,Nanchang 330022,Jiangxi
  • Received:2015-10-15 Revised:2016-02-01 Online:2016-10-01 Published:2016-10-01
  • Contact: Xu Chuanqi,born in 1990,is a candidate for master degree in Jiangxi Normal University. He is mainly engaged in physical geography and Quaternary science.E-mail: 834630747@qq.com.About the corresponding author Jia Yulian,born in 1971,is a professor at the Jiangxi Normal University. He is mainly engaged in physical geography and Quaternary environment. E-mail:1476288868@qq.com.
  • Supported by:
    ; [Co-funded by the National Natural Science Foundation of China(No; 41262007), the Project of Collaborative Innovation Center for Major Ecological Security Issues of Jiangxi Province and Monitoring Implementation(No; JXS-EX-00),and the Opening Fund of Key Laboratory of Poyang Lake Wetland and Watershed Research(Jiangxi Normal University),Ministry of Education(No; ZK2013003)]

摘要: 中国南方网纹红土是在季风气候条件下形成的一种特殊地层,对重建南方第四纪气候环境具有特殊重要的意义,但长期以来对网纹化过程的物化特点缺乏足够的认识。对江西九江、彭泽与湖南岳阳3个剖面的黏土质网纹红土中白色网纹和红色基质分离后进行了地球化学元素、游离铁含量等测试,结果表明:(1)白色网纹中,发生了FeMnThGaCuZnCoNiCrV等元素的显著亏损,SiO2ZrHf及轻稀土元素的显著富集,游离铁含量较低;红色基质中则完全相反;(2)网纹中Fe2+含量较高,基质中含量较低,揭示了网纹倾向于还原环境,基质倾向于氧化环境。研究认为网纹和基质这种氧化还原差异,是FeMnCoNiCrVZnThGaCu等元素在网纹中游离淋失,并在基质中的沉淀富集,造成ZrSiO2及轻稀土等在网纹中的相对富集、在基质中“稀释”而呈现亏损的主要原因。

关键词: 红色基质, 白色网纹, 元素地球化学, 网纹发育程度, 干湿交替

Abstract: Reticulate red clay in southern China is a kind of special stratum that formed in a monsoon climate condition,which is of great significance to reconstruct the Quaternary climate environment. For a long time,there is a lack of adequate understanding of physical and chemical characteristics of the formation process of reticulated mottles. Three sections of reticulate red clay,which were located in the Jiujiang and Pengze of Jiangxi Province, and Yueyang of Hunan Province, were studied, and the red matrix and the white reticulated mottles were separated and the geochemical elements,free iron content and so on were analysed. The results show that:(1)In the white reticulated mottles, Fe,Mn,Th,Ga,Cu,Zn,Co,Ni,Cr,V elements are outstanding leaching,while Zr,SiO2,Hf and light rare earth elements are obvious enriched,and the content of free iron are low; in the red matrix, they are reversed. (2)Fe2+ content is higher in the white reticulate,while lower in the matrix,which indicates white reticulate tend to be developed in a reductive environment and matrix tend to be developed in an oxidized environment. The difference of oxidation reduction between white reticulated mottles and red matrix is supposed to be the reason why Fe,Mn,Co,Ni,Cr,V,Zn,Th,Ga,Cu are leaching in the white reticulated mottles and enriched in the matrix, which cause Zr,SiO2 and light rare earth elements relative enriched in the white reticulated mottles and “dilution” in the red matrix.

Key words: red matrix, white reticulated mottles, element geochemistry, development degree of reticulated mottles, alternating wet and dry

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