CLAY MINERALOGICAL PROPERTIES OF BROWN FOREST SOILS IN NORTHERN KYOTO WITH SPECIAL REFERENCE TO THEIR PEDOGENETIC PROCESS

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概要

• 論文の詳細を見る

• Clay mineralogical properties of brown forest soils and podzolic soils under natural beech and/or cryptomeria forests were studied. B horizons in both profiles had 2 : 1 : 1-2 : 1 intergrade as a dominant clay mineral. This intergrade, which was formed from dioctahedral clay mica in the weathering process, changed to smectite or high charge smectite via vermiculite in the pedogenetic process. The distribution pattern of exchangeable Al in the profiles was closely related to the mineralogical changes, which may enable to distinguish the brown forest soil from the podzolic soil, since the amount of Al increased toward the surface from the subsurface horizon in the brown forest soils whereas it showed a maximum value at A3 or B1 horizon in the podzolic soils.

• 社団法人日本土壌肥料学会の論文

著者

• ARAKI Shigeru

  Faculty of Agriculture and The Center for African Area Studies, Kyoto University

• Kyuma K

  Faculty Of Environmental Science The University Of Shiga Prefecture

• Araki S

  Center For African Area Studies Kyoto University

• Hirai Hideaki

  Faculty Of Agriculture Kyoto University

• Kyuma Kazutake

  Faculty Of Agriculture Kyoto University

• Araki Shigeru

  Faculty Of Agriculture And The Center For African Area Studies Kyoto University

• Kyuma Kazutake

  Faculty Of Agriculture Kinki University

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