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Precometary organic matter: A hidden reservoir of water inside the snow line.
Nakano, Hideyuki; Hirakawa, Naoki; Matsubara, Yasuhiro; Yamashita, Shigeru; Okuchi, Takuo; Asahina, Kenta; Tanaka, Ryo; Suzuki, Noriyuki; Naraoka, Hiroshi; Takano, Yoshinori; Tachibana, Shogo; Hama, Tetsuya; Oba, Yasuhiro; Kimura, Yuki; Watanabe, Naoki; Kouchi, Akira.
Afiliação
  • Nakano H; Department of Science, Kyoto University of Education, 1 Fukakusafujinomori-cho, Fushimi-ku, Kyoto, 612-8522, Japan.
  • Hirakawa N; Department of Sport Education, Toin University of Yokohama, 1614 Kurogane-cho, Aoba-ku, Yokohama, 225-8503, Japan.
  • Matsubara Y; Department of Science, Kyoto University of Education, 1 Fukakusafujinomori-cho, Fushimi-ku, Kyoto, 612-8522, Japan.
  • Yamashita S; Graduate School of Engineering Science, Yokohama National University, 79-5 Tokiwadai, Hodogaya-ku, Yokohama, 240-8501, Japan.
  • Okuchi T; Department of Science, Kyoto University of Education, 1 Fukakusafujinomori-cho, Fushimi-ku, Kyoto, 612-8522, Japan.
  • Asahina K; Institute for Planetary Materials, Okayama University, 827 Yamada, Misasa, Tottori, 682-0193, Japan.
  • Tanaka R; Institute for Planetary Materials, Okayama University, 827 Yamada, Misasa, Tottori, 682-0193, Japan.
  • Suzuki N; Research Institute for Geo-resources and Environment, Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology, Tsukuba, Ibaraki, 305-8567, Japan.
  • Naraoka H; Department of Earth and Planetary Sciences, Hokkaido University, Sapporo, Hokkaido, 060-0810, Japan.
  • Takano Y; Ube Industries, Ltd., 1978-96 Kogushi, Ube, Yamaguchi, 755-8633, Japan.
  • Tachibana S; Department of Earth and Planetary Sciences, Hokkaido University, Sapporo, Hokkaido, 060-0810, Japan.
  • Hama T; Department of Earth and Planetary Sciences/Research Center for Planetary Trace Organic Compounds, Kyushu University, 744 Motooka, Nishi-ku, Fukuoka, 819-0395, Japan.
  • Oba Y; Biogeochemistry Program, Japan Agency for Marine-Earth Science and Technology, 2-15 Natsushima, Yokosuka, Kanagawa, 237-0061, Japan.
  • Kimura Y; UTokyo Organization for Planetary and Space Science, University of Tokyo, 7-3-1 Hongo, Tokyo, 113-0033, Japan.
  • Watanabe N; Japan Aerospace Exploration Agency, Sagamihara, Kanagawa, 252-5210, Japan.
  • Kouchi A; Institute of Low Temperature Science, Hokkaido University, Sapporo, Hokkaido, 060-0819, Japan.
Sci Rep ; 10(1): 7755, 2020 May 08.
Article em En | MEDLINE | ID: mdl-32385395
ABSTRACT
The origin and evolution of solar system bodies, including water on the Earth, have been discussed based on the assumption that the relevant ingredients were simply silicates and ices. However, large amounts of organic matter have been found in cometary and interplanetary dust, which are recognized as remnants of interstellar/precometary grains. Precometary organic matter may therefore be a potential source of water; however, to date, there have been no experimental investigations into this possibility. Here, we experimentally demonstrate that abundant water and oil are formed via the heating of a precometary-organic-matter analog under conditions appropriate for the parent bodies of meteorites inside the snow line. This implies that H2O ice is not required as the sole source of water on planetary bodies inside the snow line. Further, we can explain the change in the oxidation state of the Earth from an initially reduced state to a final oxidized state. Our study also suggests that petroleum was present in the asteroids and is present in icy satellites and dwarf planets.

Texto completo: 1 Coleções: 01-internacional Base de dados: MEDLINE Idioma: En Revista: Sci Rep Ano de publicação: 2020 Tipo de documento: Article País de afiliação: Japão

Texto completo: 1 Coleções: 01-internacional Base de dados: MEDLINE Idioma: En Revista: Sci Rep Ano de publicação: 2020 Tipo de documento: Article País de afiliação: Japão