CHARACTERISTICS OF BROWN FOREST SOILS DEVELOPED ON THE PALEOZOIC SHALE IN NORTHERN KYOTO WITH SPECIAL REFERENCE TO THEIR PEDOGENETIC PROCESS
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概要
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Morphological and chemical properties of brown forest soils and podzolic soils developed on paleozoic shale under beech and/or cryptomeria have been studied with special reference to the eluviation-illuviation characteristics of Fe and Al. Mobilization of Al was observed even in brown forest soils and its pattern was similar to that in podzolic soils. Its intensity was higher in the brown forest soils developed on the ridge under cryptomeria than in those on the slope under beech. Hence, podzolization is considered to be one of the genetic processes involved in the brown forest soils in question. Furthermore, the value of (Fep+Alp)/clay that is employed to define a podzolic B or spodic horizon indicated the presence of a podzolic B horizon even in the brown forest soils studied, while no spodic horizon was found even in the podzolic soils with a clearly recognizable albic horizon. Moreover, the examination of the degree of podzolization showed that the brown forest soils almost corresponded to Ochreous brown earths.
- 社団法人日本土壌肥料学会の論文
著者
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ARAKI Shigeru
Faculty of Agriculture and The Center for African Area Studies, Kyoto University
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Kyuma K
Faculty Of Environmental Science The University Of Shiga Prefecture
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Araki S
Center For African Area Studies Kyoto University
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Hirai Hideaki
Faculty Of Agriculture Kyoto University
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Kyuma Kazutake
Faculty Of Agriculture Kyoto University
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Araki Shigeru
Faculty Of Agriculture And The Center For African Area Studies Kyoto University
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Kyuma Kazutake
Faculty Of Agriculture Kinki University
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