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长江口邻近海域夏季溶解态稀土元素的含量及配分模式

Contents and partition pattern of dissolved rare earth elements in the Yangtze River Estuary adjacent sea area in summer

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【作者】 李锐郑爱榕朱祖浩陈丁郑雪红

【Author】 LI Rui;ZHENG Airong;ZHU Zuhao;CHEN Ding;ZHENG Xuehong;College of Ocean and Earth Sciences,Xiamen University;Fourth Institute of Oceanography,Ministry of Natural Resources;

【通讯作者】 朱祖浩;

【机构】 厦门大学海洋与地球学院自然资源部第四海洋研究所

【摘要】 海水中溶解态稀土元素由于其含量极低且水体干扰较多,少有研究.采取流动注射分离富集加上电感耦合等离子体质谱技术,测定了2016年7月长江口邻近海域水体中稀土元素含量,并研究了稀土元素的配分模式和分馏特征.结果表明,研究海域海水中稀土元素含量为0.20ng/kg(Lu)~39.45ng/kg (Y),重稀土元素相对轻稀土元素富集、轻稀土元素亏损的特征十分明显.所有站位的Ce均表现为负异常,表明该海域处于氧化环境;Ho/Y均值在0.024~0.027,高于海水均值,表明水体中Y相对于重稀土元素优先析出.

【Abstract】 There have been few researches on dissolved rare earth elements in seawater due to their extremely low levels in seawater.In this paper,using the flow injection in separation-enrichment and inductively coupled plasma mass spectrometry technology in determination,we measured the concentration of dissolved rare earth elements in seawater collected in the sea area adjacent to the Yangtze River Estuary in July,2016,and results showed the contents varied from 0.20 ng/kg(Lu)to 39.45 ng/kg(Y).The data analysis showed significant scavenge of LREEs;HREEs were more enriched than LREEs in this area.The Ce-anomaly at all stations was negative,indicating that this area was an oxidized environment.The Ho/Y mean value was 0.024 to 0.027,which was higher than the average of seawater.

【基金】 国家自然科学基金海洋科学基地野外实践能力提高项目(J1310037);广西科技基地和人才专项(2018AD19280);广西自然科学基金(2018JJB150102);北海市科技计划项目(201995037)
  • 【文献出处】 厦门大学学报(自然科学版) ,Journal of Xiamen University(Natural Science) , 编辑部邮箱 ,2020年S1期
  • 【分类号】P734
  • 【被引频次】1
  • 【下载频次】114
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