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黄铁矿 Re-Os 同位素定年化学前处理若干条件初探
引用本文:黄小文,漆亮,刘莹莹,王怡昌.黄铁矿 Re-Os 同位素定年化学前处理若干条件初探[J].地球化学,2012(4):380-386.
作者姓名:黄小文  漆亮  刘莹莹  王怡昌
作者单位:1. 中国科学院地球化学研究所矿床地球化学国家重点实验室,贵州贵阳550002
2. 中国科学院研究生院,北京100049
基金项目:国家自然科学基金(40773070);中国科学院“百人计划”(KZCX2-YW-BR-09)
摘    要:对黄铁矿 Re-Os 同位素定年化学前处理过程中的溶样温度、溶样酸介质及溶样时间进行了条件实验.温度实验结果表明,溶样温度对 Re 的测定结果影响不大,而对 Os 的测定结果影响较明显.溶样温度在120~220℃之间时,无论是 HNO3还是逆王水溶样, Re 含量在误差范围内都是一致的,但在120℃、150℃时, Os 的含量偏离真实值,可能是样品和稀释剂中的 Os 同位素并未完全达到平衡,在180℃、200℃和220℃时, Os 的含量基本一致且接近真实值.溶样酸介质实验表明, HNO3和逆王水溶样对 Re 的测定影响不大,而对 Os 的测定影响较明显.无论是用 HNO3还是逆王水溶样,在不同温度下所得到的 Re 含量是一致的,而在120℃、150℃时,逆王水溶样较 HNO3溶样所得到的 Os 含量更加接近真实值,180℃、200℃和220℃时,两种酸介质溶样得到的 Os 含量基本一致且接近真实值.用逆王水在200℃时溶样,时间为5 h、8 h、12 h、18 h所得到的 Re、187Os 含量基本一致,说明较高温度下在较短的时间内便能达到较好的溶样效果.Fe3+浓度对Re 的阴离子交换效率实验表明, Re 的回收率随着 Fe3+浓度的不断升高而逐渐下降.当黄铁矿取样量为3 g时,上柱体积控制在40 mL 左右可获得较高的 Re 回收率

关 键 词:溶样温度  溶样介质  溶样时间  回收率  黄铁矿  Re-Os  同位素

Preliminary study on sample-preparation for Re-Os isotopic dating of pyrite
HUANG Xiao-wen,QI Liang,*,LIU Ying-ying,and WANG Yi-chang.Preliminary study on sample-preparation for Re-Os isotopic dating of pyrite[J].Geochimica,2012(4):380-386.
Authors:HUANG Xiao-wen  QI Liang    LIU Ying-ying  and WANG Yi-chang
Institution:1,21. State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China;2. Graduate University of Chinese Academy of Sciences, Beijing 100049, China
Abstract:Different digestion conditions, including temperature, acids and time, were tested for Re-Os isotopic dating of pyrite. The results show that the digestion temperature and different acids medium have no effect on Re results but have significant effect on Os. The results of Os are much lower than the true values, when digestion temperature at 120~150 ℃, this may probably due to isotope disequilibrium between 190Os spike and Os in samples. When temperature at 180 ℃, 200 ℃ and 220 ℃, the results are basically the same and in agreement with the true values. Re results are similar to each other within error using HNO3 or inverse aqua regia as digestion medium at different temperatures, whereas Os concentrations are much closer to the true values under inverse aqua regia digestion than HNO3 digestion at 120 ℃ and 150 ℃. Os concentrations are similar to each other within error from 180 ℃ to 220 ℃, irrespective of the digestion acids. Coincident Re, 187Os contents have been obtained by digesting with inverse aqua regia at 200 ℃ for 5 h, 8 h, 12 h and 18 h, indicating that good results can be obtained for a relatively short time of digestion. The experiments of c(Fe3+) on anion-exchange efficiency of Re show that the recovery of Re decrease sharply with increasing c(Fe3+). When the sampling weight of pyrite reaches three grams, diluting the solution to 40 mL will get a good recovery of Re.
Keywords:digestion temperature  digestion acids  digestion time  recovery  pyrite  Re-Os isotope
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