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高Cr地质样品的Mg同位素分析方法 被引量:2

High Precision Magnesium Isotope Measurement for High-Cr Samples
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摘要 使用多接收等离子体质谱仪测定Mg同位素比值时,Cr元素会干扰测定结果。高Cr地质样品如铬尖晶石和铬铁矿中的Cr/Mg值可高达5︰1。针对这些样品,本研究检测了Cr对Mg同位素测试的干扰程度,评估了实验室流程中Cr和Mg的分离效果,探讨了Cr在淋洗过程中的行为。实验采用1mol/L HNO_3及2.3mL AG50W-X8型阳离子树脂,仅通过一次分离纯化便能将Mg与Cr等其他基质元素有效分离,且Mg的回收率可达99.8%,测试结果可靠。此外,Cr在分离过程中分为两阶段被洗脱,这与其在样品中不同的赋存价态有关。 High chromium contents of samples will significantly interfere results ofthe Mg isotopic analysis using a multicollector inductively coupled plasma mass spectrometry( MC-ICP-MS). There are high-Cr samples,such as chrome spinel and chromite with Cr / Mg ratios up to 5︰1. This study investigates the intensity of interference of Cr on Mg isotopic analyses,evaluates the separation efficiency of Cr from Mg in laboratory process,and discusses the Cr behavior in eluting process. Experiment results show that Mg can be purified efficiently from Cr and other matrix elements through cluting process once with AG50W-X8 cation resin in 1 mol/L HNO_3medium. The recovery of yielded Mg is higher than 99. 8%,ensuring the accuracy and precision of Mg isotope measurement. In addition,the behavior of Cr during elution process is also discussed. During the separation process,chromium was eluted from the column in early and late two stages respectively,owing to different valence states of Cr in solutions.
出处 《矿物岩石地球化学通报》 CAS CSCD 北大核心 2016年第3期441-447,400-401,共7页 Bulletin of Mineralogy, Petrology and Geochemistry
基金 中央高校基本科研业务费专项资金项目(2652014035)
关键词 MG同位素 MC-ICP-MS 高Cr样品 基质元素 Mg isotopic analyses MC-ICP-MS high-Cr samples matrix elements
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  • 1An Y J, Wu F, Xiang Y X, Nan X Y, Yu X, Yang J H, Yu H M, Xie L W, Huang F. 2014. High-precision Mg isotope analyses of low-Mg rocks by MC-ICP-MS. Chemical Geology, 390:9-21.
  • 2Beverskog B, Puigdomenech I. 1997. Revised pourbaix diagrams for chro- mium at 25300C. Corrosion Science, 39(1) : 43-57.
  • 3Bizzarro M, Baker J A, Haack H, Lundgaard K L. 2005. Rapid times- eales for accretion and melting of differentiated planetesimals inferred from 26A1-26Mg chronometry. The Astrophysical JoumalLe- tters, 632(1) : L41-L44.
  • 4Bizzarro M, Paton C, Larsen K, Schiller M, Trinquier A, Ulibeck D. 2011. High-precision Mg-isotope measurements of terrestrial and ex- traterrestrial material by HR-MC-ICPMS: Implications for the relative and absolute Mg-isotope composition of the bulk silicate Earth. Journal of Analytical Atomic Spectrometry, 26(3) : 565-577.
  • 5Chang V T C, Makishima A, Belshaw N S, O'Nions R K. 2003. Purifica- tion of Mg from low-Mg biogenic carbonates for isotope ratio determi- nation using multiple collector ICP-MS. Journal of Analytical Atomic Spectrometry, 18(4) : 296-301.
  • 6Galy A, Belshaw N S, Halicz L, O'Nions R K. 2001. High-precision measurement of magnesium isotopes by multiple-eoneetor inductively coupled plasma mass spectrometry. International Journal of Mass Spectrometry, 208(1) : 89-98.
  • 7Huang F, Zhang Z F, Lundstrom C C, Zhi X C. 2011. Iron and magnesi- um isotopic compositions of peridotite xenoliths from Eastern China. Geoehimica et Cosmochimiea Aeta, 75(12) : 3318-3334.
  • 8Liu S A, Teng F Z, Yang W, Wu F Y. 2011. High-temperature inter- mineral magnesium isotope fractionation in mantle xenoliths from the North China craton. Earth and Planetary Science Letters, 308 ( 1 ) : 131-140.
  • 9Pogge Von Strandmann P A E, Burton K W, James R H, Van Calsteren P, Gislason S R, Sigfllsson B. 2008. The influence of weathering processes on riverine magnesium isotopes in a basaltic terrain. Earth and Planetary Science Letters, 276( 1 ) : 187-197.
  • 10Pogge Von Strandmann P A E, Elliott T, Marschall H R, Coath C, Lai Y J, Jeffcoate A B, lonov D A. 2011. Variations of Li and Mg iso- tope ratios in bulk ehondrites and mantle xenoliths. Geoehimiea et Cosmochimiea Aeta, 75(18) : 5247-5268.

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