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首页> 外文期刊>The American mineralogist >Analyst and etching protocol effects on the reproducibility of apatite confined fission-track length measurement, and ambient-temperature annealing at decadal timescales
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Analyst and etching protocol effects on the reproducibility of apatite confined fission-track length measurement, and ambient-temperature annealing at decadal timescales

机译:分析人和蚀刻协议对磷灰石狭窄裂变轨道长度测量的再现性的影响,以及在Decadal Timescalles时的环境 - 温度退火

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摘要

Previous inter-laboratory experiments on confined fission-track length measurements in apatite have consistently reported variation substantially in excess of statistical expectation. There are two primary causes for this variation: (1) differences in laboratory procedures and instrumentation, and (2) personal differences in perception and assessment between analysts. In this study, we narrow these elements down to two categories, etching procedure and analyst bias. We assembled a set of eight samples with induced tracks from four apatite varieties, initially irradiated between 2 and 43 years prior to etching. Two mounts were made containing aliquots of each sample to ensure identical etching conditions for all apatites on a mount. We employed two widely used etching protocols, 5.0 M HNO_3 at 20 °C for 20 s and 5.5 M HNO_3 at 21 °C for 20 s. Sets of track images were then captured by an automated system and exchanged between two analysts, so that measurements could be carried out on the same tracks and etch figures, in the same image data, allowing us to isolate and examine the effects of analyst bias. An additional 5 s of etching was then used to evaluate etching behavior at track tips. In total, 8391 confined fission-track length measurements were performed; along with 1480 etch figure length measurements. When the analysts evaluated each other's track selections within the same images for suitability for measurement, the average rejection rate was ~14%. For tracks judged as suitable by both analysts, measurements of 2D and 3D length, dip, and c-axis angle were in excellent agreement, with slightly less dispersion when using the 5.5 M etch. Lengths were shorter in the 5.0 M etched mount than the 5.5 M etched one, which we interpret to be caused by more prevalent under-etching in the former, at least for some apatite compositions. After an additional 5 s of etching, 5.0 M tracks saw greater lengthening and more reduction in dispersion than 5.5 M tracks, addition
机译:以前的实验室内实验对磷灰石中限制的狭窄裂变轨道长度测量的实验始终报告的变化基本上超过统计期望。这种变异有两种主要原因:(1)实验室程序和仪器的差异,以及(2)分析师之间的感知和评估中的个人差异。在这项研究中,我们将这些元素缩小到两类,蚀刻程序和分析师偏见。我们组装了一组八个样本,其中诱导轨道来自四个磷灰石品种,最初在蚀刻前2和43年之间辐照。制备两个安装件,其中每个样品的等分试样,以确保安装在安装上的所有散热物的相同蚀刻条件。我们使用两种广泛使用的蚀刻方案,在20℃下为5.0μmHNO_3,在21℃下为20℃,5.5M HNO_3 20秒。然后通过自动化系统捕获一组轨道图像并在两个分析人员之间交换,因此可以在相同的图像数据中在相同的轨道和蚀刻数字上进行测量,允许我们隔离和检查分析师偏置的效果。然后使用另外的5S蚀刻来评估轨道提示处的蚀刻行为。总共,执行8391个限制裂变轨道长度测量;以及1480蚀刻图长测量。当分析师在同一图像内评估彼此的轨道选择以进行适合测量时,平均抑制率为约14%。对于由分析人员判断为合适的曲目,2D和3D长度,倾角和C轴角度的测量非常好,使用5.5M蚀刻时的色散略差。在5.0μm的蚀刻安装座上比5.5M蚀刻的安装件短较短,我们解释前者在前者中的蚀刻率更普遍,至少用于一些磷灰石组合物。在额外的5秒蚀刻后,5.0米的轨道看到比5.5米的分散延长更大,更低更低

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