Evaluating the Effect of Hydrofluoric Acid Etching on Quartz Grains using Microscope Image Analysis, Laser Diffraction and Weight Loss Particle Size Estimate

IF 1.2 4区 地球科学 Q3 Earth and Planetary Sciences
G. Poręba, K. Tudyka, A. Szymak, Julia Pluta, Joanna Rocznik, J. Swiatkowski, R. Osadnik, P. Moska
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Abstract

Abstract In this work we investigate the quartz etching process using hydrofluoric acid for trapped charge dating (TCD) applications. It is done using material collected from an active sand mine in Bełchatów Nowy Świat, central Poland. Approximately 20 kg of material was collected and prepared using routine procedures that are applied in TCD laboratories. The material was sieved using 180–200 μm meshes, and the selected fraction was etched for various time intervals. Sieved samples were etched for durations from 0 min up to 180 min and measured with microscope image analysis (IA), laser diffraction (LD), and mass loss which were used to estimate the depths of etching. Our results show statistical data on how non-uniform the etching process is. We estimate this as a function of etching time from IA, LD and mass loss. In our investigation, mass loss measurements with the assumption of spherical grains correspond to the decrease of radius of ca. 0.151 ± 0.003 μm · min−1. In case of LD, a rough etch depth estimation corresponds to a range 0.06–0.18 μm · min−1 with median at 0.13 μm · min−1. Microscope IA gives a 0.03–0.09 μm · min−1 with a median at 0.05 μm · min−1. Moreover, quartz grains are fractured into smaller pieces while etching. It means that assumptions that are used in etch depth estimation from mass loss are not correct. They incorrect not only because grains are not spheres but also because the number of grains is not constant. Therefore, the etch depth estimated from mass loss might be overestimated. Using microscope IA we report etch depth ranges that might be used to roughly estimate the etch depth uncertainty.
利用显微镜图像分析、激光衍射和失重粒度评估氢氟酸蚀刻对石英颗粒的影响
摘要在这项工作中,我们研究了使用氢氟酸进行捕获电荷测年(TCD)应用的石英蚀刻工艺。它是使用从波兰中部Bełchatów Nowyćwiat一个活跃的砂矿收集的材料完成的。使用技合实验室采用的常规程序收集和制备了大约20公斤材料。使用180–200μm筛网对材料进行筛分,并在不同的时间间隔内蚀刻选定的部分。将筛分的样品蚀刻0分钟至180分钟的持续时间,并用显微镜图像分析(IA)、激光衍射(LD)和质量损失进行测量,用于估计蚀刻深度。我们的结果显示了蚀刻过程不均匀程度的统计数据。我们根据IA、LD和质量损失估计这是蚀刻时间的函数。在我们的研究中,假设球形晶粒的质量损失测量对应于约0.151±0.003μm·min−1的半径减小。在LD的情况下,粗略蚀刻深度估计对应于0.06–0.18μm·min−1的范围,中值为0.13μm•min−1。显微镜IA给出0.03–0.09μm·min−1,中值为0.05μm·min-1。此外,石英颗粒在蚀刻时会断裂成更小的碎片。这意味着在根据质量损失估计蚀刻深度时使用的假设是不正确的。它们不正确,不仅因为晶粒不是球体,还因为晶粒的数量不是恒定的。因此,根据质量损失估计的蚀刻深度可能被高估。使用显微镜IA,我们报告了可用于粗略估计蚀刻深度不确定性的蚀刻深度范围。
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来源期刊
Geochronometria
Geochronometria 地学-地球科学综合
CiteScore
2.20
自引率
0.00%
发文量
1
审稿时长
>12 weeks
期刊介绍: Geochronometria is aimed at integrating scientists developing different methods of absolute chronology and using them in different fields of earth and other natural sciences and archaeology. The methods in use are e.g. radiocarbon, stable isotopes, isotopes of natural decay series, optically stimulated luminescence, thermoluminescence, EPR/ESR, dendrochronology, varve chronology. The journal publishes papers that are devoted to developing the dating methods as well as studies concentrating on their applications in geology, palaeoclimatology, palaeobiology, palaeohydrology, geocgraphy and archaeology etc.
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