Influence of Eolian Dust Originated in the Precambrian Area in Northern Asia Continent on a Fine-Textured Soil Distributed on the Pleistocene Plateau, the Right Bank of Jinzu River in Sarukura, Toyama City, Central Japan

  • OKUDA Toshio
    Graduate School of Biosciences, Fukui Prefectural University
  • FUJITA Tetsushi
    Graduate School of Biosciences, Fukui Prefectural University
  • FUJIE Kohtaroh
    Graduate School of Biosciences, Fukui Prefectural University
  • KITAGAWA Yasuo
    Graduate School of Biosciences, Fukui Prefectural University
  • SAITO Mannosuke
    Depertment of Engineering Kyoto Sangyo University
  • NARUSE Toshiro
    Social Science and Social Studies, and Language Education, Hyogo University of Teacher Educatior
  • TOYODA Shin
    Department of Applied Physics, Okayama University of Science

Bibliographic Information

Other Title
  • 富山市南部神通川右岸の更新世台地上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風成塵の影響
  • トヤマシ ナンブ ジンズウガワ ウガン ノ コウシンセイ ダイチジョウ 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 フウセイジン ノ エイキョウ

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Abstract

The ESR-signal intensity of fine quartz in the silt fraction and the clay mineral composition were examined, in order to investigate the influence of eolian dust on the parent materials in a fine-textured soil developed on the Pleistocene plateau in the northern foot of Mt. Sarukura (354m), Sarukura Ohsawano, Toyama city. The results are summarized as follows: It was considered that the eolian dust brought with the winter NW-monsoon from the Precambrian area in the northern part of Asia continent during the M1S2 (24-11thousand years ago) in the Last Glacial Maximum was influenced severely on the parent materials in this soil. The autochitonous Pleiocene rocks were also considered to be influenced slightly on the parent materials in this soil. Moreover, a small amount of the tephras such as "AiraTn" was admixed with in this soil.

Journal

  • Pedologist

    Pedologist 52 (1), 35-41, 2008-06-30

    Japanese Society of Pedology

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