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Global Cycle of Boron Isotopes in Modern and Fossil Marine Carbonates and Carbon Minerals

Research Project

Project/Area Number 09640580
Research Category

Grant-in-Aid for Scientific Research (C)

Allocation TypeSingle-year Grants
Section一般
Research Field 地球化学
Research InstitutionTokyo Institute of Technology

Principal Investigator

NOMURA Masao  Research Laboratory for Nuclear Reactors, Tokyo Institute of Technology, Research Associate, 原子炉工学研究所, 助手 (60100997)

Co-Investigator(Kenkyū-buntansha) 野村 雅夫  東京工業大学, 原子炉工学研究所, 助手 (60100997)
Project Period (FY) 1997 – 1999
Project Status Completed (Fiscal Year 1999)
Budget Amount *help
¥1,700,000 (Direct Cost: ¥1,700,000)
Fiscal Year 1999: ¥400,000 (Direct Cost: ¥400,000)
Fiscal Year 1998: ¥500,000 (Direct Cost: ¥500,000)
Fiscal Year 1997: ¥800,000 (Direct Cost: ¥800,000)
KeywordsBoric Acid / Boron isotope / Isotopic Ratio / Carbonate / Coral / Fossil / ホウ素 / 珊瑚
Research Abstract

The boron isotopic composition were measured about coral 28 samples collected on offing the Okinoerabu iland, the Tonaki island, and the Miyako island of the Okinawa southwest islands. The kind of coral used two species of helioporas, 20 species of acroporas, two species of montiporas, and four species of poriteses, respectively. Boron was separated from the about 6g sample by the methyl borate distillation, and the boron isotopic ratios were measure. Moreover, the determination of the element which exists in a sample was carried out by emission spectrochemical analysis. Consequently, Na, K, Li, Mg, Sr, Ba, and B were contained as main coexistence elements. Many Sr, Ns, and Mg were contained in it. As for some coral, the crystal form changed with coexistence of magnesium from the aragonite to the calcite in part. This is guessed from positive correlation being between magnesium concentration, and C / A ratio. There was no correlation between boron concentration or an isotopic ratio, and other chemistry components. Boron concentration was 20-50 ppm, the average was 40.95 ppm, and the standard deviation was ±7.23 ppm. Boron isotopic ratios are 4.107-4.158 (15.8-28.3% as deltaィイD111ィエD1B), the boron isotopic ratios in 26 samples of the others except heliopora are 4.133-4.158, and the average was set to 4.141. The standard deviation at this time was ±0.008, and was the variation in a very narrow sphere. This value showed theoretical calculation and very good coincidence. However, a difference is looked at by a coexistence element, the isotopic ratio, etc. between the coral of heliopora and others, and the boron isotopic ratio in the coral of heliopora showed the in addition to this more low boron isotopic ratio. This is considered to suggest that it may be a certain biologically different isotope effect.

Report

(4 results)
  • 1999 Annual Research Report   Final Research Report Summary
  • 1998 Annual Research Report
  • 1997 Annual Research Report
  • Research Products

    (3 results)

All Other

All Publications (3 results)

  • [Publications] 野村雅夫,大井隆夫,他: "沖縄県宮古島サンゴのホウ素同位体組成"日本海水学会誌. 第53巻・第6号. 471-475 (1999)

    • Description
      「研究成果報告書概要(和文)」より
    • Related Report
      1999 Final Research Report Summary
  • [Publications] Masao NOMURA, Takao OI, Ryo TANGE, Hironobu KAN, Morikazu HOSOE, and Nobuyuki HORI: "Boron Isotopic Composition of Coral off Miyako Island, Okinawa"Bulletin of the Society of Sea Water Science, Japan. Vol. 53. 471-475 (1999)

    • Description
      「研究成果報告書概要(欧文)」より
    • Related Report
      1999 Final Research Report Summary
  • [Publications] 野村雅夫,大井隆夫,他: "沖縄県宮古島サンゴのホウ素同位体組成"日本海水学会誌. 第53巻・第6号. 471-475 (1999)

    • Related Report
      1999 Annual Research Report

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Published: 1997-04-01   Modified: 2016-04-21  

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