技术说明:剂量测年用天然样品中铀系不平衡的定量测定。第1部分:伽马光谱法

IF 2.7 Q2 GEOCHEMISTRY & GEOPHYSICS
B. Mauz, P. Nolan, P. Appleby
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引用次数: 3

摘要

摘要剂量测年技术依赖于对环境放射性的精确测定。伽马能谱法是测定238U、232Th和40K活度的首选方法。为了使伽马光谱测定程序标准化,以确定自然样品中准确的母核素活性,我们在这里概述了伽马光谱测定的基础知识和实际的实验室程序。这包括伽马辐射和仪器,样品制备,为给定的探测器找到合适的测量几何形状和样品大小,以及在伽马光谱中使用最合适的能量峰。强调了正确的效率校准问题。所概述的程序是估计当代母核素活度所必需的。为了估计埋葬期间变化的活动,需要具体的数据分析,这些也被强调。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Technical note: Quantifying Uranium-series disequilibrium in natural samples for dosimetric dating – Part 1: gamma spectrometry
Abstract. Dosimetric dating techniques rely on accurate and precise determination of environmental radioactivity. Gamma spectrometry is the method of choice for determining the activity of 238U, 232Th and 40K. With the aim to standardise gamma-spectrometric procedures for the purpose of determining accurate parent nuclide activities in natural samples, we outline here basics of gamma spectrometry and practical laboratory procedures. This includes gamma radiation and instrumentation, sample preparation, finding the suitable measurement geometry and sample size for a given detector and using the most suitable energy peaks in a gamma spectrum. The issue of correct efficiency calibration is highlighted. The procedures outlined are required for estimating contemporary parent nuclide activity. For estimating changing activities during burial specific data analyses are required and these are also highlighted.
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来源期刊
Geochronology
Geochronology Earth and Planetary Sciences-Paleontology
CiteScore
6.60
自引率
0.00%
发文量
35
审稿时长
19 weeks
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