首页> 外文期刊>Indian Journal of Marine Sciences >REE geochemistry of seawater from Afanasy-Nikitin Seamount in North Central Indian Ocean by high resolution inductively coupled plasma mass spectrometry
【24h】

REE geochemistry of seawater from Afanasy-Nikitin Seamount in North Central Indian Ocean by high resolution inductively coupled plasma mass spectrometry

机译:高分辨率电感耦合等离子体质谱法测定印度中北部北部阿凡纳西-尼基丁海山的海水稀土地球化学

获取原文
获取原文并翻译 | 示例
           

摘要

REE (Rare Earth Elements) and yttrium in sea water samples, from the Afanasy-Nikitin Seamount (ANS) located around 3 degrees South latitude and 83 degrees East longitude in the north central Indian Ocean were precisely determined by high resolution inductively coupled plasma mass spectrometry (HR-ICP-MS) method. A modified procedure has been designed for determination of REE and yttrium wherein the water samples were subjected to a pre-concentration step using bis-2-ethylhexyl phosphoric acid (HDEHP) complexing agent. Sea water reference materials such as NASS-5 and SLEW-3 were used for calibration as well as to check the accuracy of the procedure adopted. Samples were analyzed for REE and yttrium by HR-ICP-MS. Precisions achieved for various rare earths and yttrium is better than 8% RSD with comparable accuracies. Limit of detection (3 sigma) were generally in the range of 0.02-1.2 pg/ml range for all these elements. This method facilitates rapid and interference-free determination of REE and yttrium from relatively small volume of sea water (10 ml). Recoveries for different REE and Y were better than 5%, and accuracy and precision of the determinations are within 8% RSD The Ce-negative anomalies with smooth normalized-REE patterns obtained for both certified reference materials and samples further substantiate that the procedure adopted and the data generated are extremely accurate. A slight enrichment of heavy REE were observed in the central Indian Ocean waters which might be attributed to the river flows containing more dissolved trace elements including REE. A sharp negative Ce-anomaly in the normalized REE distribution patterns indicates that the source of REE in particular Ce in marine sediments is seawater. Results of the variation in REE concentrations with depth indicated that the physico-chemical conditions of bottom ocean water follow a very complex mechanism.
机译:来自印度洋中部北纬3度和东经83度的Afanasy-Nikitin海山(ANS)海水样品中的REE(稀土元素)和钇是通过高分辨率感应耦合等离子体质谱法精确测定的(HR-ICP-MS)方法。设计了一种改进的程序来确定REE和钇,其中使用双-2-乙基己基磷酸(HDEHP)络合剂对水样品进行了预浓缩步骤。诸如NASS-5和SLEW-3之类的海水参考材料用于校准以及检查所采用程序的准确性。通过HR-ICP-MS分析样品的REE和钇。各种稀土和钇的精确度均优于可比精度的8%RSD。所有这些元素的检出限(3σ)通常在0.02-1.2 pg / ml的范围内。该方法有助于从相对少量的海水(10毫升)中快速,无干扰地测定稀土元素和钇。不同REE和Y的回收率均优于5%,并且测定的准确性和精密度均在8%RSD之内。对于经认证的参考物质和样品均获得的具有平滑归一化REE模式的Ce阴性异常进一步证实了所采用的程序和生成的数据非常准确。在印度洋中部水域中发现了重稀土元素的少量富集,这可能归因于河流中含有更多溶解的微量元素,包括稀土元素。归一化稀土元素分布模式中急剧的负Ce异常表明,海洋沉积物中稀土元素特别是铈的来源是海水。稀土元素浓度随深度变化的结果表明,底部海水的物理化学条件遵循非常复杂的机制。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号