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The grain size influence on the E1'centre observed in quartz of atmospheric deposition at two Japanese cities : a preliminary study

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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The grain size influence on the number of oxygen vacancies in quartz was investigated by ESR in atmospheric deposition collected at two Japanese cities, Fukuoka and Akita, in 1969 and 1971. The finer grain size fraction shows the highest value of concentration of oxygen vacancies, most closely resembling dust originating in the Taklamakan desert. Month to month and year to year variation of the dependence was also observed which could possibly be attributed to the variation of the mixture ratio of at least two dust sources in China, A conclusive statement can not be made at this stage.
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Wydawca
Czasopismo
Rocznik
Tom
Strony
9--12
Opis fizyczny
Bibliogr. 13 poz., rys., tab.
Twórcy
autor
autor
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Bibliografia
  • Feigl FJ, Fowler WB and Yip KL, 1974. Oxygen vacancy model for the E1′ centre in SiO2. Solid State Communications 14: 225-229. DOI 10.1016/0038-1098(74)90840-0
  • Jani MG, Bossoli RB and Halliburton LE, 1983. Further characterization of the E1′ centre in crystalline SiO2. Physical Review B 27: 2285–2293. DOI 10.1103/PhysRevB.27.2285
  • Nagashima K, Tada R, Tani A, Toyoda S, Sun Y 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): Q02Q04, DOI 10,1029/2006GC001364.
  • Naruse T, Ono Y, Hirakawa K, Okashita M and Ikeya M, 1997. Source areas of eolian dust quartz in East Asia: a tentative reconstruction of prevailing winds in isotope stage 2 using electron spin resonance. Geographical Review of Japan. 70A-1: 15–27 (in Japanese).
  • Igarashi Y, Inomata Y, Aoyama M, Hirose K, Takahashi H, Shinoda Y, Sugimoto N, Shimizu A and Chiba M, 2009. Possible change in Asia dust source suggested by atmospheric anthropogenic radionuclides during the 2000s. Atmospheric Environment 43: 2971-2980. DOI 10.1016/j.atmosenv.2009.02.018.
  • Ono Y, Naruse T, Ikeya M, Konho H and Toyoda S, 1998. Origin and derived courses of eolian dust quartz deposited during marine isotope stage2 in East Asia, suggested by ESR signal intensity. Global and Planetary Change 18(3-4): 129-135. DOI 10.1016/S0921-8181(98)00012-5.
  • Silsbee RH, 1961. Electron Spin Resonance in Neutron-Irradiated Quartz. Journal of Applied Physics 32: 1459-1462. DOI 10.1063/1.1728379.
  • Toyoda S, 1992. Production and decay characteristics of Paramagnetic defects in quartz: application to ESR dating. Ph.D. Thesis, Osaka University, Japan, 106p.
  • Toyoda S and Hattori W, 2000. Formation and decay of the E1’ centre and of its precursor. Applied Radiation and Isotopes 47: 1351-1356. DOI 10.1016/S0969-8043(00)00094-4.
  • Toyoda S and Ikeya M, 1991. Thermal stabilities of paramagnetic defect and impurity centres in quartz: Basis for the ESR dating of thermal history. Geochemical Journal 25(6): 437-445.
  • Toyoda S and Naruse T, 2002. Eolian dust from the Asian deserts to Japanese Islands since the lost Glacial Maximum; the basis for the ESR method. Transactions, Japanese Geomorphological Union 23: 811-820.
  • Toyoda S, Takeuchi D, Asai T, Komuro K and Horikawa Y, 2005. Spin-spin relaxation time of E1’centre in quartz with and without irradiation: implications for the formation process of the oxygen vacancies in nature. Radiation Measurements 39: 503-508. DOI 10.1016/j.radmeas.2004.09.002.
  • Weeks R A and Nelson C N, 1960. Trapped electrons in irradiated quartz and silica. II. Electron Paramagnetic Resonance. Journal of the American Ceramic Society 43: 399-404. DOI 10.1111/j.1151-2916.1960.tb13682.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BATA-0012-0026
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