1992年裂变径迹车间裂变径迹年龄实验室间比较结果

Donald S. Miller , Kevin D. Crowley , Roy K. Dokka , Rex F. Galbraith , Bart J. Kowallis , Charles W. Naeser
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引用次数: 26

摘要

在1992年7月13日至17日在美国费城举行的裂变轨道研讨会之前,向裂变轨道研究界提供了两颗磷灰石和一颗榍石进行分析。全世界有18个实验室收到了等量的磷灰石和榍石。迄今为止,由33位不同的科学家代表15个不同的实验室进行了分析。与前两次实验室间比较相比,年龄结果的准确性有显著提高(Naeser和Cebula, 1978;Naeser et al., 1981;Miller et al., 1985;Miller et al.1990)。94%的分析使用外部检测器法(EDM)结合zeta技术,其余个体使用种群法(POP)。径迹长度测量(在实验室间比较研究中首次要求)的一致性相对较好。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Results of interlaboratory comparison of fission track ages for 1992 fission track workshop

Two apatites and one sphene were made available to the fission track research community for analysis prior to the 1992 Fission Track Workshop held in Philadelphia, U.S.A., 13–17 July. Eighteen laboratories throughout the world received aliquots of apatite and sphene. To date, analyses by 33 different scientists have been representing 15 different laboratories. With respect to the previous two interlaboratory comparisons, there is a noticeable improvement in the accuracy of the age results (Naeser and Cebula, 1978; Naeser et al., 1981; Miller et al., 1985;Miller et al.1990). Ninety-four percent of the analysis used the external detector method (EDM) combined with the zeta technique while the remaining individuals used the population method (POP). Track length measurements (requested for the first time in the interlaboratory comparison studies) were in relatively good agreement.

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