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2002 Fiscal Year Final Research Report Summary

EXPERIMENTAL STUDY ON MINERAL CONDENSATION FROM GAS

Research Project

Project/Area Number 12440152
Research Category

Grant-in-Aid for Scientific Research (B)

Allocation TypeSingle-year Grants
Section一般
Research Field 地球化学
Research InstitutionTHE UNIVERSITY OF TOKYO

Principal Investigator

HIROKO Nagahara  GRADUATE SCHOOL OF SCIENCE, Professor, 大学院・理学系研究科, 教授 (80172550)

Co-Investigator(Kenkyū-buntansha) KAZUHITO Ozawa  GRADUATE SCHOOL OF SCIENCES, Professor, 大学院・理学系研究科, 教授 (90160853)
Project Period (FY) 2000 – 2002
KeywordsCondensation / evaporation / stars / the solar system / forsterite / metallic iron
Research Abstract

In order to explore the time scale and controlling factors of phases appear during condensation in various stellar environments, experimental approach to get dusts in laboratory was employed. Condensation includes two elementary processes, nucleation and crystal growth, in which condensation is hard to control on the Earth due to the gravitational force. The most abundant elements that form solid materials in the universe are Si, Mg and Fe. Calculation of chemical equilibrium and astrophysical observation around young and evolved stars and interstellar space reveal that forserite, enstatite and metallic iron are the dominant phases. Therefore, experiments of condensation of forsterite, ensatite, and metallic iron dust on substrates without nucleation are planned at low pressure conditions.
At first, development of an experimental equipment was attempted, and an vacuum chamber made of stainless steel with tungsten mesh heated and W and Mo thermal shields were prepared to obtain large amount of hot gas at the condensation spot. The results, however, were found to be unsuitable for condensation of silicate dusts, because the tungsten prevents condensation of oxygen atoms or molecules into silicates. Then, condensation of metallic iron was intended by using iron oxide (Fe2O3) as an evaporation source, and metallic Mo and forsterite for substrates. The source was heated at 1350℃ for 1 to 120 hours, and the reside and condensates were observed with a scanning electron microscopy (SEM) and analyzed with electron back scattered diffraction (EBSD) technique. Condensates were observed on both Mo and forsterite, of which size and amount increase with time, and are determined to be metallic iron. They show cubic shape and the size is larger on forsterite than Mo. The results show that the temperature of substance at a radiation field from a star plays key role on dust growth due to difference in actual temperature.

  • Research Products

    (18 results)

All Other

All Publications (18 results)

  • [Publications] Nagahara, H., Ozawa, K.: "Isotopic fractionation as a probe of heating processes in the solar nebula"Chemical Geology. 169. 45-68 (2000)

    • Description
      「研究成果報告書概要(和文)」より
  • [Publications] Ozawa, K., Nagahara, H.: "Kinetics of diffusion-controlled evaporation of Fe-Mg olivine : experimental study and implications for the cosmochemical fractionation"Geochim. Cosmochim. Acta. 64. 173-189 (2000)

    • Description
      「研究成果報告書概要(和文)」より
  • [Publications] Kita, N.T., Nagahara, H., Togashi, S., Morishita, Y.: "A short duration of chondrules formation in the solar nebula : Evidence from ^<26>Al in Semarkona ferromagnesian chondrules"Geochim. Cosmochim. Acta. 64. 3913-3922 (2000)

    • Description
      「研究成果報告書概要(和文)」より
  • [Publications] K.Ozawa, H.Nagahara: "Chemical and isotopic fractionations by evaporation and their cosmochemical implications"Geochim. Cosmochim. Acta. 65. 2171-2199 (2001)

    • Description
      「研究成果報告書概要(和文)」より
  • [Publications] Nagahara, H., Ozawa, K: "The timescale of accretion and core formation of the Earth inferred from Hf-W isotope systematics"Proc. Japan National Academy. 77B. 167-171 (2001)

    • Description
      「研究成果報告書概要(和文)」より
  • [Publications] Ozawa, K: "Mass balance equations for open magmatic systems : Trace element behavior and its application to open system melting in the upper mantle"Jour. Geophys. Res.. 106. 13407-13434 (2001)

    • Description
      「研究成果報告書概要(和文)」より
  • [Publications] Tachibana, S., Tsuchiyama, A, Nagahara, H.: "Experimental study of incongruent evaporation kinetics of enstatite in vacuum and in hydrogen gas"Geochim. Cosmochim. Acta. 66. 713-728 (2002)

    • Description
      「研究成果報告書概要(和文)」より
  • [Publications] Young, E.D., Galy, A., Nagahara, H: "Kinetic and equilibrium mass-dependent fractionation laws in nature and their geochemical and cosmochemical significance"Geochim. Cosmochim. Acta. 66. 1095-1104 (2002)

    • Description
      「研究成果報告書概要(和文)」より
  • [Publications] Mostfaoui, S., Kita, N.T., Togashi, S., Tachibana, S., Nagahara, H., Morishita, Y: "The relative formation ages of ferromagnesian chondrules inferred from their initial 26Al/27Al"Meteorit. Planet. Sci. 37. 421-438 (2002)

    • Description
      「研究成果報告書概要(和文)」より
  • [Publications] Nagahara, H. and Ozawa, K.: "Isotopic fractionation as a probe of heating processes in the solar nebula"Chemical Geology. 169. 45-68 (2000)

    • Description
      「研究成果報告書概要(欧文)」より
  • [Publications] Ozawa, K. and Nagahara, H: "Kinetics of diffusion-controlled evaporation of Fe-Mg olivine : experimental study and implications for the cosmochemical fractionation"Geochim. Cosmochim. Acta. 64. 173-189 (2000)

    • Description
      「研究成果報告書概要(欧文)」より
  • [Publications] Kita, N. T., Nagahara, H., Togashi, S., and Morishita, Y: "A short duration of chondrules formation in the solar nebula : Evidence from ^<26>Al in Semarkona ferromagnesian chondrules"Geochim. Cosmochim. Acta. 64. 3913-3922 (2000)

    • Description
      「研究成果報告書概要(欧文)」より
  • [Publications] K. Ozawa and H. Nagahara: "Chemical and isotopic fractionations by evaporation and their cosmochemical implications"Geochim. Cosmochim. Acta. 65. 2171-2199 (2000)

    • Description
      「研究成果報告書概要(欧文)」より
  • [Publications] Nagahara, H. and Ozawa, K: "The timescale of accretion and core formation of the Earth inferred from Hf-W isotope systematics"Proc. Japan National Academy. 77B. 167-171 (2001)

    • Description
      「研究成果報告書概要(欧文)」より
  • [Publications] Ozawa, K: "Mass balance equations for open magmatic systems : Trace element behavior and its application to open system melting in the upper mantle"Jour. Geophys. Res.. 106. 13407-13434 (2001)

    • Description
      「研究成果報告書概要(欧文)」より
  • [Publications] Tachibana, S., Tsuchiyama, A. and Nagahara, H: "Experimental study of incongruent evaporation kinetics of enstatite in vacuum and in hydrogen gas"Geochim. Cosmochim. Acta. 66. 713-728 (2002)

    • Description
      「研究成果報告書概要(欧文)」より
  • [Publications] Young, E. D., Galy, A., and Nagahara, H: "Kinetic and equilibrium mass-dependent fractionation laws in nature and their geochemical and cosmochemical significance"Geochim. Cosmochim. Acta. 66. 1095-1104 (2002)

    • Description
      「研究成果報告書概要(欧文)」より
  • [Publications] Mostfaoui, S., Kita, N. T. Togashi, S., Tachibana, S., Nagahara, H. and Morishita, Y.: "The relative formation ages of ferromagnesian chondrules inferred from their initial 26Al/27Al"Meteorit. Planet. Sci.. 37. 421-438 (2002)

    • Description
      「研究成果報告書概要(欧文)」より

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Published: 2004-04-14  

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