Journal of Jilin University(Earth Science Edition)

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Chemical Separation of the Sample with High REE-Nb-Fe-Mn Contents for Mg Isotope Ratio Measurements

Li Shizhen1, Fang Nan1,2, Sun Jian1,2, Chen Yuelong2, Zhu Xiangkun1   

  1. 1.Institute of Geology,Chinese Academy of Geological Sciences/Laboratory of Isotope Geology MLR/State Key Laboratory for Continental Tectonics and Dynamics,Beijing100037,China;
    2.School of Earth Science and Mineral Resources,China University of Geosciences,Beijing100083,China
  • Received:2012-04-16 Online:2013-01-26 Published:2013-01-26

Abstract:

The measured values of Mg isotope ratios using multi-collector inductively coupled plasma mass spectrometry may be effected by matrix elements to certain extent. Some geological samples such as those from the Baiyan Obo ore deposit may have exceptionally high contents of REE, Nb, Fe and Mn. An investigation of effects of matrix elements on Mg isotope ratio measurement has been carried out. The results show that the measured δ26Mg deviates from true value when the matrix/Mg(mass fraction) is over 0.2. Thus it is necessary to resolve these matrix elements before determining the δ26Mg value. Firstly, the protocols established for Mg purification are using AG MP-1 anion exchange resin and 2.5 mL 10 mol/L HCl+0.001% H2O2 reagents as loading medium and eluant, the first 2.5 mL eluant contains Mg but no Fe and Mn; and then using AG50W-X12 cation exchange resin and 2 mol/L HCl as loading medium and eluants, the eluant from 2-7 mL 2 mol/L contain Mg but no REE,Nb and other matrix elemts.

Key words: matrix effects, separation, Mg isotope, the sample with high REE-Nb-Fe-Mn;isotopes, Bayan Obo

CLC Number: 

  • P595
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