Influence of Eolian Dust Brought from the Precambrian Area in Northern Asia on the Parent Materials in a Fine-Textured Soil Developed on the Tertiary Rock in Mt. Horyu, Noto Peninsula, Central Japan

  • OKUDA Toshio
    Graduate School of Bio Sciences, Fukui Prefectural University
  • FUJITA Tetsushi
    Graduate School of Bio Sciences, Fukui Prefectural University
  • FUJIE Kohtaro
    Graduate School of Bio Sciences, Fukui Prefectural University
  • KITAGAWA Yasuo
    Graduate School of Bio Sciences, Fukui Prefectural University
  • SAITO Mannosuke
    Depertment of Biotechnology Kyoto Sangyo University
  • NARUSE Tosihiro
    Social Science and Social Studies, and Language Education, Hyogo University of Teacher Education
  • TOYODA Shin
    Department of Applied Physics, Okayama University of Science

Bibliographic Information

Other Title
  • 能登半島宝立山山頂付近に分布する細粒質土壌母材へのアジア大陸北部の先カンブリア界由来の風成塵の影響
  • 能登半島宝立山山頂付近に分布する細粒質土壌母材へのアジア大陸北部先カンブリア界由来の風成塵の影響
  • ノト ハントウ ホウ ホウリュウサンチョウ フキン ニ ブンプスル サイリュウシツ ドジョウ ボザイ エノ アジア タイリク ホクブ センカンブリアカイ ユライ ノ フウセイジン ノ エイキョウ

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Abstract

The ESR-signal intensity associated with the oxygen vacancy in the fine quartz and the clay mineral composition were examined, in order to investigate the influence of eolian dust on the parent materials in a fine-textured Brown Forest soil developed on the bedrock, Tertiary dacitic Pyroclastic rock, near the top of Mt. Horyu in Noto peninsula. The results were summarized as follows: The high values, more than 10 unit, in the ESR-signal intensity of fine quartz in this soil suggested that, large amount of the eolian dust brought from the Precambrian sediment area influenced severely on the parent materials in this soil, and this eloian dust had been brought from Precambrian sediments area by NW-monsoon during the Last Glacial Maxmum, MIS2 (24-11 thousand years ago). On the other hand, the autochtonous Terciary bedrock was also influenced slightly on the parent materials in this soil. Moreover, the influence of a small amount of the Tephra such as A-Th was also observed in this soil.

Journal

  • Pedologist

    Pedologist 51 (2), 104-110, 2007-12-31

    Japanese Society of Pedology

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