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Photo-luminescence of zircons

Research Project

Project/Area Number 60460058
Research Category

Grant-in-Aid for General Scientific Research (B)

Allocation TypeSingle-year Grants
Research Field 鉱物学(含岩石・鉱床学)
Research InstitutionKyusyu University

Principal Investigator

SHINNO Isamu  College of General Education, 教養部・地学科, 教授 (00038465)

Co-Investigator(Kenkyū-buntansha) HAYASHI Masao  Institute of Advanced Material Science, 機能物質科学研究所, 助教授 (40038592)
Project Period (FY) 1985 – 1987
Project Status Completed (Fiscal Year 1987)
Budget Amount *help
¥6,500,000 (Direct Cost: ¥6,500,000)
Fiscal Year 1987: ¥500,000 (Direct Cost: ¥500,000)
Fiscal Year 1986: ¥1,500,000 (Direct Cost: ¥1,500,000)
Fiscal Year 1985: ¥4,500,000 (Direct Cost: ¥4,500,000)
Keywordszircon / photo-luminescence / rare earth element / alpha-decay / uranium / トリウム / 希土類元素 / 顕微分光法 / 螢光 / ESR / 希上類元素
Research Abstract

The photo-luminescences of natural zircons are originated from three main luminescent centers. 1. Type I consists of line spectra originated from REE such as Dy^<3+>, Eu^<3+>, Tm^<3+>. 2. Type II consists of broad bands originating from radiation centers due to the <alpha>-decay effect of radioactive elements of U and Th. This was ascertained successfully in the case of Ca-doped zircons, in which <alpha>-decay was induced by the nuclear reaction of ^<40>Ca(n,<alpha>)^<37>Ar. The experiment was the first success of making artificially the type II. The centers consist of several radicals in the zircon, which were also detected by ESR. The transitions depend on the crystallographic direction. However, this artificial type II disappeared for several months if REE does not coexist. The intensity of the type II of natural zircons is proportional to the geologic age of the zircon, but it is not affected by the nuclear fission of U and <gamma>-ray irradiation. Also, the luminescence is easily diminished by heat treatment at temperatures higher than 700゜C, and can be restored after several days at room temperature. 39 The type III is vary rare in occurence, and consists of relatively simple bands. This is attributed to three types of activators. (1) U and P with electron-hole centers, (2) transition elements Mn, Ni and V with 3d electrons, and (3) Ca, Ba, Zn and Sc with electron-hole centers. These activators are strongly affected by the coexisting P sensitizer. The latter two types of activators in the type III could not be distinguished in natural zircons.

Report

(2 results)
  • 1987 Final Research Report Summary
  • 1986 Annual Research Report
  • Research Products

    (7 results)

All Other

All Publications (7 results)

  • [Publications] 進野勇: 岩石鉱物鉱床学会誌. 81. 433-445 (1986)

    • Description
      「研究成果報告書概要(和文)」より
    • Related Report
      1987 Final Research Report Summary
  • [Publications] 進野勇: Mineralogical journal. 13. 239-253 (1987)

    • Description
      「研究成果報告書概要(和文)」より
    • Related Report
      1987 Final Research Report Summary
  • [Publications] I.Shinno: "Three types of photo-luminescence in natural zircon" Journla of Japanese Assoc. Min. Pet. Econ. Geol.81. 433-445 (1986)

    • Description
      「研究成果報告書概要(欧文)」より
    • Related Report
      1987 Final Research Report Summary
  • [Publications] I.Shinno: "Color and photo-luminescence of rare earth element-doped zircon" Mineralogical Journal. 13. 239-253 (1987)

    • Description
      「研究成果報告書概要(欧文)」より
    • Related Report
      1987 Final Research Report Summary
  • [Publications] I.SHINNO: 岩石.鉱物.鉱床学会誌. 81. 433-445 (1986)

    • Related Report
      1986 Annual Research Report
  • [Publications] I.SHINNO: Mineralogical Journal. 13. (1987)

    • Related Report
      1986 Annual Research Report
  • [Publications] I.SHINNO: Mineralogical Magazine. (1987)

    • Related Report
      1986 Annual Research Report

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Published: 1987-03-31   Modified: 2016-04-21  

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