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Analysis of ultra-low level rare earth elements in magnetite samples from banded iron formations using HR-ICP-MS after chemical separation

机译:化学分离后使用HR-ICP-MS分析带状铁层磁铁矿样品中的超低含量稀土元素

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We have investigated two methods for the separation of rare earth elements (REEs) and Fe in magnetites from banded iron formations (BIFs), employing cation- and anion-exchange chromatography. The separated REEs were subsequently determined using a high resolution inductively coupled plasma mass spectrometer (HR-iCP-MS). Our results indicated that 10 mL concentrated HCI was sufficient to completely separate all REES from Fe using anion exchange chromatography, whereas more than 30 mL of 6 mol L~(-1) HCl was required using cation-exchange. The recovery of REEs using both methods was 100% ± 5%. The procedure blanks for the REEs using the anion method were lower than those using the cation method. Our results indicated that the anion exchange method has advantages over cation exchange for the analysis of ultra-low level REEs in magnetites. The proposed methods were tested using the reference material FER-2.
机译:我们已经研究了两种利用阳离子交换和阴离子交换色谱法从带状铁层(BIF)中分离磁铁矿中稀土元素(REE)和Fe的方法。随后使用高分辨率感应耦合等离子体质谱仪(HR-iCP-MS)确定分离的REE。我们的结果表明,使用阴离子交换色谱法,用10 mL浓盐酸足以将所有REES与Fe完全分离,而使用阳离子交换法则需要超过30 mL的6 mol L〜(-1)HCl。两种方法的稀土元素回收率均为100%±5%。使用阴离子方法的REE的方法空白值低于使用阳离子方法的REE。我们的结果表明,阴离子交换法在分析磁铁矿中超低含量稀土元素方面优于阳离子交换。建议的方法使用参考材料FER-2进行了测试。

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