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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 ˑ min–1. In case of LD, a rough etch depth estimation corresponds to a range 0.06–0.18 μm ˑ min–1 with median at 0.13 μm ˑ min–1. Microscope IA gives a 0.03–0.09 μm ˑ min–1 with a median at 0.05 μm ˑ 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.
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Opis fizyczny
Bibliogr. 31 poz., rys.
Twórcy
autor
- Division of Geochronology and Environmental Isotopes, Institute of Physics – Centre for Science and Education, Silesian University of Technology Gliwice, Poland
autor
- Division of Geochronology and Environmental Isotopes, Institute of Physics – Centre for Science and Education, Silesian University of Technology Gliwice, Poland
autor
- Division of Geochronology and Environmental Isotopes, Institute of Physics – Centre for Science and Education, Silesian University of Technology Gliwice, Poland
autor
- Division of Geochronology and Environmental Isotopes, Institute of Physics – Centre for Science and Education, Silesian University of Technology Gliwice, Poland
autor
- Division of Geochronology and Environmental Isotopes, Institute of Physics – Centre for Science and Education, Silesian University of Technology Gliwice, Poland
autor
- Division of Geochronology and Environmental Isotopes, Institute of Physics – Centre for Science and Education, Silesian University of Technology Gliwice, Poland
autor
- Division of Geochronology and Environmental Isotopes, Institute of Physics – Centre for Science and Education, Silesian University of Technology Gliwice, Poland
autor
- Division of Geochronology and Environmental Isotopes, Institute of Physics – Centre for Science and Education, Silesian University of Technology Gliwice, Poland
Bibliografia
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- 12. Durcan JA, King GE and Duller GAT, 2015. DRAC: Dose rate and age calculator for trapped charge dating. Quaternary Geochronology 28: 54–61, DOI 10.1016/J.QUAGEO.2015.03.012.
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- 14. Duval M, Guilarte V, Campana I, Arnold LJ, Miguens L, Iglesias J and Gonzalez-Sierra S, 2018. Quantifying hydrofluoric acid etching of quartz and feldspar coarse grains based on weight loss estimates: Implication for ESR and luminescence dating studies. Ancient TL 36(1): 14.
- 15. Fleming S, 1979. Thermoluminescence techniques in archaeology. Clarendon Press, Oxford.
- 16. Fleming SJ, 1970. Thermoluminescent dating: Refinement of the quartz inclusion method. Archaeometry 12(2): 133–143, DOI 10.1111/j.1475-4754.1970.tb00016.x.
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- 24. Moska P, Bluszcz A, Poręba G, Tudyka K, Adamiec G, Szymak A and Przybyła A, 2021. Luminescence dating procedures at the Gliwice luminescence dating laboratory. Geochronometria 48(1): 1–15, DOI 10.2478/geochr-2021-0001.
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- 26. Poręba G, Śnieszko Z, Moska P and Mroczek P, 2019. Deposits of Neolithic water soil erosion in the loess region of the Małopolska Upland (S Poland) – A case study of the settlement micro-region in Bronocice. Quaternary International 502: 45–59, DOI 10.1016/j.quaint.2018.09.018.
- 27. Schaetzl RJ, Forman SL and Attig JW, 2014. Optical ages on loess derived from outwash surfaces constrain the advance of the Laurentide Ice Sheet out of the Lake Superior Basin, USA. Quaternary Research 81(2): 318–329, DOI 10.1016/j.yqres.2013.12.003.
- 28. Tudyka K, Koruszowic M, Osadnik R, Poręba G, Moska P, Szymak A, Bluszcz A, Zhang J, Kolb T and Adamiec G, 2021. μRate. https://miu-rate.polsl.pl/, v2021.0.4, Gliwice, Poland, Accessed 2021 November 23.
- 29. Wintle AG and Adamiec G, 2017. Optically stimulated luminescence signals from quartz: A review. Radiation Measurements 98: 10–33, DOI 10.1016/j.radmeas.2017.02.003.
- 30. Wintle AG and Murray AS, 2006. A review of quartz optically stimulated luminescence characteristics and their relevance in single-aliquot regeneration dating protocols. Radiation Measurements 41(4): 369–391, DOI 10.1016/j.radmeas.2005.11.001.
- 31. Zheng W, Hu X, Tannant DD, Zhang K and Xu C, 2019. Characterization of two- and three-dimensional morphological properties of fragmented sand grains. Engineering Geology 263: 105358, DOI 10.1016/j.enggeo.2019.105358.
Uwagi
Opracowanie rekordu ze środków MEiN, umowa nr SONP/SP/546092/2022 w ramach programu "Społeczna odpowiedzialność nauki" - moduł: Popularyzacja nauki i promocja sportu (2022-2023).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-b0f4d8d6-f20d-4530-8729-7dd72276f71b