期刊文献+

电感耦合等离子体质谱法测量铼和锇同位素比值的质量分馏校正 被引量:12

The Correction of Mass Fractionation in the Measurement of Rhenium and Osmium Isotope Ratios by ICP-MS
下载PDF
导出
摘要 用Re标准溶液测定出X Series-7电感耦合等离子体质谱(ICP-MS)检测器的死时间为43ns。由于Re和Ir的对数分馏系数线性相关,可以用Ir对Re进行在线分馏校正。利用配制的Re同位素比值标准溶液检验该方法,大多数校正值对标准值的相对偏差在±0.1%以下。ICP-MS测量时,Os的分馏系数与中位质量数成正比,采用由迭代方法得到的样品和稀释剂混合物的同位素比值(192Os/188Os)mix作为标准化值对其他Os同位素比值进行分馏校正。用已知Os同位素比值的标准溶液对该方法进行检验,结果表明,经校正后,大多数校正值与标准值的相对偏差在±0.3%以下。上述Re-Os同位素分馏校正方法将改善用ICP-MS进行Re-Os定年时的精密度和准确度。 The dead-time of the detector of inductively coupled plasma-mass spectrometry (ICP-MS) is 43 ns obtained by measuring Re standard solution. Since there is a liner correlation between isotopic fractionation factors of Re and Ir, Ir can be used to correct Re isotope fractionation. The test by measuring Re standard solution suggests that the relative deviations between corrected and standard values are, in most cases, less than ±0.1%. The isotopic fractionation factors of Os are proportional with the middle-mass of the isotopic pairs in the ICP-MS measurement. In this study, the Os isotope ratio of the mixture of the sample and spike Os (^192Os/^188OS)mix, obtained by iteration method is used as the normalization value to correct the isotope fractionation of other isotope ratios of Os. The test by measuring known Os isotopic solution suggests that the relative deviations between corrected and the reference values are less than ±0.3% in most cases. The correction method for Re-Os isotope fractionation presented by this paper will improve the precision and accuracy of the Re-Os dating by using ICP-MS.
出处 《岩矿测试》 CAS CSCD 2007年第1期4-8,共5页 Rock and Mineral Analysis
基金 国土资源地质大调查资助项目(200020190118-04)
关键词 质量分馏校正 电感耦合等离子体质谱法 mass fractionation correction inductively coupled plasma-mass spectrometry rhenium osmium
  • 相关文献

参考文献7

二级参考文献48

  • 1杜安道,何红蓼,殷宁万,邹晓秋,孙亚利,孙德忠,陈少珍,屈文俊.辉钼矿的铼-锇同位素地质年龄测定方法研究[J].地质学报,1994,68(4):339-347. 被引量:429
  • 2[1]Shirey SB, Walker RJ. The Re-Os Isotope System in Cosmochemistry and High-temperature Geochemistry[J]. Annu Rev Earth Plant Sci, 1998, 21: 423~500.
  • 3[2]Reisberg L, Meisel T. The Re-Os Isotopic System: A Review of Analytiques[J]. Geostandards Newsletters, 2002, 26(3): 249~267.
  • 4[4]Rosman KJR, Taylor PDP. Isotopic Composition of the Elements [J]. Pure & Appl Chem, 1997,70(1): 217~235.
  • 5[5]Finnigan MAT 262 Application Flash Report. Osmium Isotope Analyses by Negative Thermal Ionization[R]. Application Flash Report, 1995, (10): 1~2.
  • 6[6]Nier AO. A Redetermination of the Relative Ab-undances of the Isotopes of Carbon, Nitrogen, Oxygen, Argon and Potassium[J]. Phys Rev, 1950, 77: 789~793.
  • 7[7]Becker H. Re-Os Fractionation in Eclogites andBlueschists and the Implications for Recycling of Oceanic Crust Into the Mantle[J]. Earth Plant Sci Lett, 2000,177:287~300.
  • 8[8]Finnigan TRITON Application Flash Report. H-igh Precision Osmium Isotope Analyses Negative Thermal Ionization and Static Multiple Ion Collection [R]. Application Flash Report, 2001, (T2):1~2.
  • 9[9]Yin QZ, Jacobsen SB, Lee C-T, et al. A Gravimetric K2OsCl6 Standard: Application to Precise and Accurate Os Spike Calibration[J]. Geochim Cosmochim Acta, 2001, 65(13): 2 113~2 127.
  • 10[10]Tuttas D. The Measurement of Osmium Isotope Ratios Using Negative Thermal Ionization [R]. Finnigan MAT 262 Application News, 1992, (1):1~5.

共引文献606

同被引文献490

引证文献12

二级引证文献278

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部