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Three quartz samples extracted from different origins were collected for ESR evaluation to appreciate the optical bleaching characteristics of the E1’ centre in a long time scale. After exposure of about 400 hours to artificial sunlight, the E1’ centre were bleached to a steady increasing level, about 2.5 times of its natural level, and the increase level also exhibit a small variability among different sample origins. The constant increasing level provide a significantly evidence for the potential use of the natural signal intensities of quartz E1’ centre in tracing sediment provenance. The results show that the signal intensity of E1’ centre increased within beginning 84 h and decreased after 202 h as previous researches have partly predicted. After long time exposed to sunlight, there is no correlation between irradiated samples’ dose rate and its E1’ centre ESR signal intensity. Thus, no new convenient indication shed light on the possible use of the E1’ centre for ESR sediment dating.
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Czasopismo
Rocznik
Tom
Strony
79--86
Opis fizyczny
Bibliogr. 34 poz., rys., tab.
Twórcy
autor
- State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China
- School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
autor
- State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China
autor
- School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
- State Key Laboratory of Biogeology and Environmental Geology, Wuhan 430074, China
autor
- State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China
autor
- Institute of Geophysics and Geomatics, China University of Geosciences, Wuhan 430074, China
autor
- State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China
autor
- Shandong Provincial Key Laboratory of Water and Soil Conservation and Environmental Protection, School of Resource and Environmental Sciences, Linyi University, Linyi, China, 276000
Bibliografia
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- 2. Chappell BW, 1999. Aluminium saturation in I- and S-type granites and the characterization of fractionated haplogranites. Lithos 46(3): 535–551, DOI 10.1016/S0024-4937(98)00086-3.
- 3. Chappell BW and White AJR, 1992. I- and S-type granites in the Lachlan Fold Belt[J]. Transactions of the Royal Society of Edinburgh – Earth Sciences 83(1–2): 1–26, DOI 10.1017/S0263593300007720.
- 4. Crook NP, Hoon SR, Taylor KG and Perry CT, 2002. Electron Spin Resonance as a High Sensitivity Technique for Environmental Magnetism: Determination of Contamination in Carbonate Sediments. Geophysical Journal International 149(2): 328–337, DOI 10.1046/j.1365-246X.2002.01647.x.
- 5. Duval M, Arnold LJ, Guilarte V, Demuro M, Santonja M and PerezGonzalez A, 2017. Electron spin resonance dating of optically bleached quartz grains from the Middle Palaeolithic site of Cuesta de la Bajada (Spain) using the multiple centres approach. Quaternary Geochronology 37: 82–93, DOI 10.1016/j.quageo.2016.09.006.
- 6. Falgueres C, Miallier D, Sanzelle S, Fain J, Laurent M, Montret M, Pilleyre T and Bahain JJ, 1994. Potential use of the E1’ centre as an indicator of initial resetting in TL/ESR dating of volcanic materials. Quaternary Science Reviews 13(5–7): 619–623, DOI 10.1016/0277-3791(94)90088-4.
- 7. Fukuchi T, 1992. ESR studies for absolute of fault movements. Journal of the Geological Society 149(9): 265–272, DOI 10.1144/gsjgs.149.2.0265.
- 8. Jani MG, Bossoli RB and Halliburton, 1983. Further characterization of the E1’ centre in crystalline SiO2. Physical Review B 27(4): 2285– 2293, DOI 10.1103/PhysRevB.27.2285.
- 9. Jin SZ, Deng Z and Huang PH, 1991. A response study of E1’ centre of loess quartz to light. Chinese Science Bulletin 36(10): 741–744. (in Chinese).
- 10. Jin SZ, Deng Z and Huang PH, 1993. A comparative study on optical effects of E1’ centre in quartz grains from loess and fault. Applied Radiation and Isotopes 44(1–2): 175–178, DOI 10.1016/0969- 8043(93)90215-V.
- 11. Liu CR, Yin GM, Gao L, Bahain JJ, Li JP, Lin M and Chen SM, 2010. ESR dating of Pleistocene archaeological localities of the Nihewan Basin, North China- Preliminary results. Quaternary Geochronology 5(2): 385–390, DOI 10.1016/j.quageo.2009.05.006.
- 12. Nagashima K, Tada R, Tani A, Toyoda S, Sun YB and Isozaki Y, 2007. Contribution of Aeolian Dust in Japan Sea Sediments Estimated from ESR Signal Intensity and Crystallinity of Quartz. Geochemistry, Geophysics, Geosystems 8(2) DOI 10.1029/2006GC001364.
- 13. Nagashima K, Tada R, Tani A, Sun YB, Isozaki Y, Toyoda S and Hasegawa H, 2011. Millennial-Scale Oscillations of the Westerly Jet Path During the Last Glacial Period. Journal of Asian Earth Sciences 40(6): 1214–1220 DOI 10.1016/j.jseaes.2010.08.010.
- 14. Ono Y, Naruse T, Ikeya M, Kohnoc H and Toyoda S, 1998. Origin and Derived Courses of Eolian Dust Quartz Deposited during Marine Isotope Stage 2 in East Asia, Suggested by ESR Signal Intensity. Global and Planetary Change 18(3): 129–135, DOI 10.1016/S0921-8181(98)00012-5.
- 15. Rink WJ, 1997. Electron spin resonance (ESR) dating and ESR applications in Quaternary science and archaeometry. Radiation Measurements 27(5–6): 975–1025, DOI 10.1016/S1350- 4487(97)00219-9.
- 16. Rink WJ, Bartoll J, Schwarcz HP, Shane P and Bar-Yosef O, 2007. Testing the reliability of ESR dating of optically exposed buried quartz sediments. Radiation Measurements 42 (10): 1618–1626, DOI 10.1016/j.radmeas.2007.09.005.
- 17. Shimada A, Takada M and Toyoda S, 2013. Characteristics of ESR Signals and TLCLs of Quartz Included in Various Source Rocks and Sediments in Japan: A Clue to Sediment Provenance. Geochronometria 40(4): 334–340, DOI 10.2478/s13386-013-0111-z.
- 18. Sun YB, Chen H, Tada R, Weiss D, Lin M, Toyoda S, Yan Y and Isozaki Y, 2013. ESR Signal Intensity and Crystallinity of Quartz from Gobi and Sandy Deserts in East Asia and Implication for Tracing Asian Dust Provenance. Geochemistry, Geophysics, Geosystems 14(8): 2615–2627, DOI 10.1002/ggge.20162.
- 19. Sun YB, Tada R, Chen J, Chen HZ, Toyoda S, Tani A, Isozaki Y, Nagashima K, Hasegawa H and Ji JF, 2007. Distinguishing the Sources of Asian Dust Based on Electron Spin Resonance Signal Intensity and Crystallinity of Quartz. Atmospheric Environment 41(38): 8537–8548, DOI 10.1016/j.atmosenv.2007.07.014.
- 20. Sun YB, Tada R, Chen J, Liu QS, Toyoda S, Tani A, Ji JF and Isozaki Y, 2008. Tracing the Provenance of Fine-Grained Dust Deposited on the Central Chinese Loess Plateau. Geophysical Research Letters 35(1): L01804, DOI: 10.1029/2007GL031672.
- 21. Tissoux H, Falgueres C, Voinchet P, Toyoda S, Bahain JJ and Despriee, 2007. Potential use of Ti-centre in ESR dating of fluvial sediment. Quaternary Geochrology 2(1): 367–372, DOI 10.1016/j.quageo.2006.04.006.
- 22. Toyoda S and Hattori W, 2000. Formation and decay of the E1’ centre and of its precursor. Applied Radiation and Isotopes 52(5): 1351– 1356, DOI 10.1016/S0969-8043(00)00094-4.
- 23. Toyoda S and Ikeya, 1991. Thermal stabilities of paramagnetic defect and impurity centres in quartz: basis for ESR dating of thermal history. Geochemical Journal 25: 437–445, DOI 10.2343/geochemj.25.437.
- 24. Toyoda S and Schwarcz, 1997. Counterfeit E1’ signal in quartz. Radiation Measurements 27(1): 59–66, DOI 10.1016/S1350- 4487(96)00073-X.
- 25. Toyoda S and Naruse T, 2002. Eolian Dust from the Asian Deserts to the Japanese Islands since the Last Glacial Maximum: the Basis for the ESR Method. Transactions, Japanese Geomorphological Union 23: 811–820.
- 26. Toyoda S, Voinchet P, Falgueres C, Dolo JM and Laurent M, 2000. Bleaching of ESR signals by the sunlight: a laboratory experiment for establish the ESR dating of sediments. Applied Radiation and Isotopes 52(5): 1357–1362, DOI 10.1016/S0969-8043(00)00095-6.
- 27. Toyoda S, 2011. The E1’ centre in Natural Quartz: Its Formation and Applications to Dating and Provenance Researches. Geochronometria 38(3): 242–248, DOI 10.2478/s13386-011-0035-4.
- 28. Toyoda S, Nagashima K and Yamamoto Y, 2015. ESR Signals in Quartz: Applications to Provenance Research–a Review. Quaternary International 397: 258–266, DOI 10.1016/j.quaint.2015.05.048.
- 29. Voinchet P, Falgueres C, Laurent M, Toyoda S, Bahain JJ and Dolo JM, 2003. Artificial optical bleaching of the Aluminium centre in quartz implications to ESR dating of sediments. Quaternary Science Reviews 22(10): 1335–1338, DOI 10.1016/S0277- 3791(03)00062-3.
- 30. Wei CY, Li CA, Liu CR, Li WP, Zhang ZJ, Zhang HS, Zhao JX and Zhang LY, 2017. Nature ESR signals of quartz E1’ centre shed new light on river sediments provenance: a case study in southeast margin of the Tibet Plateau. Quaternary International 10(454): 38–44, DOI 10.1016/j.quaint.2017.08.044.
- 31. Yamamoto Y, Toyoda S, Nagasima K, Igarashi Y and Tada R, 2013. Investigation of the Temporal Change of the Sources of Aeolian Dust Delivered to East Asia Using Electron Spin Resonance Signals in Quartz. Geochronometria 40(4): 355–359, DOI 10.2478/s13386-013-0121-x.
- 32. Yang SY, Wang ZB, Guo Y, Li CX, Cai JG, 2009. Heavy mineral compositions of the Changjiang (Yangtze River) sediments and their provenance-tracing implication. Journal of Asian Earth Sciences 35(1): 56–65, DOI 10.1016/j.jseaes.2008.12.002.
- 33. Yokoyama Y, Falgueres C and Quaegebeur JP, 1985. ESR dating of quartz from Quaternary sediments: first attempt. Nuclear Tracks and Radiation Measurements (1982) 10(4–6): 921–928, DOI 10.1016/0735-245X(85)90109-7.
- 34. Zhao XT, Gao H, Li DS, Ding ZZ and Yang BM, 1991. Effect of light irradiation on E1’ centre ESR signal measurement of quartz samples. Nuclear Techniques 14(2): 87–89. (in Chinese with English abstract).
Uwagi
Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2019).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-a0ca33cd-bb28-41b2-9cf6-1b0f92042138