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Variation of OSL residual doses in terms of coarse and fine grain modern sediments along the Hungarian section of the Danube

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Warianty tytułu
Konferencja
Conference Proceedings of the 12th International Conference “Methods of Absolute Chronology” May 11-13th, 2016, Gliwice-Paniówki, Poland
Języki publikacji
EN
Abstrakty
EN
Reliable OSL dating of fluvial sediments requires an assessment of incomplete bleaching and consequent residual dose in samples. A well-established way of this is determining the equivalent dose of modern samples from similar sedimentary environments as in the case of palaeo-samples. Meanwhile, relatively low, or close to zero doses are also greatly affected by the thermal transfer phenomenon, which can also lead to a palaeodose overestimation. The present study attempts to quantify both factors in coarse and fine grain modern sediments along the Hungarian section of the Danube River, with the aim of determining their significance when dating both young and palaeo-sediments. Investigations were performed at 30 sites along a 417 km long river section with varying morphological and erosive character. The studied samples were deposited during the record flood of 2013, mobilising and relocating a vast amount of sediment in the system. Tests have shown that thermal transfer can be minimized successfully by choosing preheat temperatures below 200°C, however it remains a significant factor when dating young or modern sediments. Based on equivalent dose measurements, coarse grain samples proved to be relatively well bleached, and residual doses showed only a minor spatial variation. Although in terms of fine grain samples residual doses were obviously much higher, results can enhance the reliability of dates retrieved later from fine grain palaeo-samples. In the meantime, the higher spatial variability of fine grain residual doses may also allow the assessment of the erosive character of different river reaches.
Słowa kluczowe
Wydawca
Czasopismo
Rocznik
Strony
319--330
Opis fizyczny
Bibliogr. 27 poz., rys.
Twórcy
autor
  • Department of Physical Geography and Geoinformatics, University of Szeged, Egyetem u. 2-6, H-6722 Szeged, Hungary
autor
  • Department of Physical Geography and Geoinformatics, University of Szeged, Egyetem u. 2-6, H-6722 Szeged, Hungary
autor
  • Department of Physical Geography and Geoinformatics, University of Szeged, Egyetem u. 2-6, H-6722 Szeged, Hungary
autor
  • Department of Physical Geography and Geoinformatics, University of Szeged, Egyetem u. 2-6, H-6722 Szeged, Hungary
Bibliografia
  • 1. Aitken MJ, 1998. An Introduction to Optical Dating. Oxford University Press. London.
  • 2. Alexanderson H, 2007. Residual OSL signals from modern Greenlandic river sediments. Geochronometria 26: 1–9.
  • 3. Bogárdi J, 1971. Sediment transport of streams. Academic Press, Budapest.
  • 4. Colls AE, Stokes S, Blum MD and Straffin E, 2001. Age limits on the Late Quaternary evolution of the upper Loire River.Quaternary Science Reviews 20: 743–750.
  • 5. Fiebig M and Preusser F, 2007. Investigating the amount of zeroing in modern sediments of River Danube, Austria.Quaternary Geochronology 2: 143–149.
  • 6. Fuchs M and Lang A, 2001. OSL dating of coarse-grain fluvial quartz using single-aliquot protocols on sediments from NE Peloponnese, Greece. Quaternary Science Reviews 20: 783–787.
  • 7. Galbraith RF, 2005. Statistics for Fission Track Analysis. 240. p. Chapman and Hall, London.
  • 8. Galbraith RF, Roberts RG, Laslett GM, Yoshida H and Olley JM, 1999. Optical dating of single and multiple grains of quartz from Jinmium rock shelter, northern Australia. Part I: Experimental design and statistical models. Archeometry 41: 339–364.
  • 9. Hu G, Zhang J-F, Qui W-L and Zhou L-P, 2010. Residual OSL signals in modern fluvial sediments from Yellow River (HuangHe) and the implications for dating young sediments. Quaternary Geochronology 5: 187–193.
  • 10. Jain M, Thomsen KJ, Botter-Jensen L and Murray AS, 2004. Thermal transfer and apparent-dose distribution in poorly bleached mortar samples: Results from single grains and small aliquots of quartz. Radiation Measurements 38: 101–109,.
  • 11. Jaiswal MK, Chen YG, Kale VS and Achyuthan H, 2009. Residual luminescence in quartz from slack water deposits in Kaveri Basin, South India: a single aliquot approach. Geocronometria 33: 1–8.
  • 12. Lepper K, Larsen NA and McKeever SWS, 2000. Equivalent dose distribution analysis of Holocene eolian and fluvial quartz sands from central Oklahoma. Radiation Measurements 32: 603–608.
  • 13. Li B and Li S-H, 2006. Correcting for thermal transfer in OSL measurements of young sediment samples. Radiation Measurements 41: 855–861.
  • 14. Mezősi G, 2011. Geography of Hungary. Academic Press, Budapest.
  • 15. Murray AS, Olley JM and Caitcheon GG, 1995. Measurements of equivalent doses in quartz from contemporary water-lain sediments using optically stimulated luminescence. Quaternary Science Reviews 14: 365–371.
  • 16. Murray AS and Wintle AG, 2003. The single aliquot regenerative dose protocol: potential for improvements in reliability.Radiation Measurements 37(4): 377–381.
  • 17. Olley J, Caitcheon G and Murray A, 1998. The distribution of apparent dose as determined by optically stimulated luminescence in small aliquots of fluvial quartz: Implications for dating young sediments. Radiation Measurements 30: 207–217.
  • 18. Rittenour TM, 2008. Luminescence dating of fluvial deposits: applications to geomorphic palaeoseismic and archaeological research. Boreas 37: 613–635.
  • 19. Sipos G, Kiss T and Tóth O, 2016. Constraining the age of floodplain levels along the lower section of River Tisza, Hungary.Journal of Environmental Geography 9(1–2): 39–44.
  • 20. Stokes S, Bray HE and Blum MD, 2001. Optical resetting in large drainage basins: tests of zeroing assumptions using single-aliquot procedures. Quaternary Science Reviews 20: 879–885.
  • 21. Treulsen JL and Wallinga J, 2003. Zeroing of the OSL signal as a function of grain size: investigatting bleaching and thermal transfer for a young fluvial sample. Geochronometria 22: 1–8.
  • 22. Vandenberghe D, Derese C and Houbrechts G, 2007. Residual doses in recent alluvial sediments from Ardenne (S Belgium). Geochronometria 28: 1–8.
  • 23. VITUKI – Vizgzdálkodási Tudományos Kutató Intézet (Hungarian Water Resources Research Centre), 1971. Hydrographic Atlas Series 11. Danube 4. (Hydrography, geomorphology). Budapest.
  • 24. Wallinga J, Murray AS, Duller GAT, Törnqvist TR, 2001. Testing optically stimulated luminescence dating of sand-sized quartz and feldspar from fluvial deposits. Earth and Planetery Science Letters193: 617–630.
  • 25. Wang XL, Wintle AG and Lu YC, 2006. Thermally transferred luminescence in fine-grained quartz from Chinese loess: Basic observations. Radiation Measurements 41: 649–658.
  • 26. Ward S, Stokes S, Bailey R, Singarayer J, Goudie A and Bray H, 2003. Optical dating of quartz from young samples and the effects of pre-heat temperature. Radiation Measurements 37: 401–407.
  • 27. 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: 369–391.
Uwagi
Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2018).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-a09e8003-b3da-4b55-b563-4d5d22ec1893
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