Mineral Composition of Clay Fractions and Oxygen Vacancies in Silt-Sized Quartz in Soils on the Ka-Etsu Plateau, Fukui, Central Japan-Possibility of Eolian Dust Brought from Northern Asia as Parent Material of Soils(Soil Genesis, Classification and Survey

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概要

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• Fine- to medium-textured soils are distributed on the Early Pliocene rocks and Pleistocene sandy sediments in the Ka-Etsu plateau. The Jingaoka (JIN) soil was classified into Aluandic Andosols by WRB, and Low-humic Non-allophanic Kuroboku soils by the Fourth Committee for Soil Classification and Nomenclature of the Japanese Society of Pedology, although it was similar morphologically to Yellow-Brown Forest soils. On the other hand, the Tomitsu (TMI) and Yamamuro (YAM) soils were classified into Hyperdystri-Chromic Cambisols by WRB, and Typic Yellow-Brown Forest soils by the Fourth Committee for Soil Classification and Nomenclature based on the morphological, physical and chemical properties. These soils were influenced considerably by the Akahoya tephra, especially the JIN soil. Based on the results of clay-mineralogical analysis and the measurement of the ESR-signal intensity associated with the oxygen vacancies in fine quartz, a large part of parent materials in the soils distributed on the Ka-Etsu plateau was derived from the eolian dust which was brought with the NW winter monsoon from the Precambrian sediments in the northern part of the Asian continent during MIS 2 (24-11 thousand years ago) at the Last Glacial Maximum. The parent materials of the fine-textured JIN soil located on the highest terrace near the rocky coastline were mostly composed of eolian dust, although the influenced of the Akahoya tephra was recognized. The parent materials of the TMI soil were admixed with a small amount of autochthonous materials from the sandy coast located windward. In the YAM soil which was located on the side of a hilly area distant from the coastline, the ESR-signal intensity in fine quartz was considerably low, and the admixture of autochthonous materials was also considered since the texture of this soil was coarser than that of the JIN and TMI soils.

• 社団法人日本土壌肥料学会の論文

著者

• TOYODA Shin

  Department of Applied Physics Faculty of Science Okayama University of Science

• 栗原 宏彰

  福井県立大

• Kitagawa Y

  Fukui Prefectural University

• Kitagawa Yasuo

  Graduate School Of Bioscience Fukui Prefectural University

• Kitagawa Yasuo

  Graduate Program For Biochemical Regulation Graduate School Of Agricultural Sciences

• 栗原 宏彰

  愛知県立田口高等学校林業科

• Kurihara Hiroaki

  Taguchi High School

• Imoto H

  Takeda Chemical Ind. Ltd. Osaka Jpn

• Imoto Hiroshi

  Graduate School of Bioscience and Biotechnology, Fukui Prefectural University

• Saito Mannosuke

  Faculty of Engineering, Kyoto Sangyo University

• Fujie Kohtaro

  Graduate School of Bioscience and Biotechnology, Fukui Prefectural University

• Naruse Toshiro

  Department of Geography, Hyogo University of Teacher Education

• Imoto H

  Graduate School Of Bioscience And Biotechnology Fukui Prefectural University

• Fujie Kohtaro

  Graduate School Of Bioscience Fukui Prefectural University

• SAITO MANNOSUKE

  Fuculty of Technology, Kyotosangyo University

• Naruse Toshiro

  Department Of Geography Hyogo University Of Education

• Saito Mannosuke

  Fuculty Of Technology Kyotosangyo University

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