CHANGES IN CLAY MINERALOGY IN A CHRONOSEQUENCE OF POLDER PADDY SOILS FROM KOJIMA BASIN, JAPAN
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概要
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Changes in the clay mineralogy in a chronosequence of polder soils cultivated with paddy rice for 15, 75,150, and 265 years in Kojima Basin were studied. Parent materials of each profile appeared to be homogeneous. Prolonged paddy cultivation (150 and 265 years) brought about some modification in the clay mineralogy of Ap horizons, while the mineralogical changes were not evident in the profiles less than 75 years of age. Characteristic changes consisted of the formation of 18-25 Å minerals, which were composed of interlamellar humus-smectite complexes and interstratified minerals. The interstratification showed intermediate stages from smectite to kaolin minerals along with partial chloritization of smectite. The interstratification and partial chloritization of smectite caused the CEC of the clay fractions of Ap horizons to decrease partly.
- 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 Kazutake
Faculty Of Agriculture Kyoto University
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Kyuma Kazutake
Faculty Of Agriculture Shimane University
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Wakatsuki Toshiyuki
Faculty Of Agriculture Kinki University
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ISHIKAWA Itaru
Faculty of Agriculture, Shimane University
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Araki Shigeru
Faculty Of Agriculture And The Center For African Area Studies Kyoto University
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Araki Shigeru
Faculty Of Agriculture Shimane University
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Ishikawa Itaru
Faculty Of Agriculture Shimane University
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Kyuma Kazutake
Faculty Of Agriculture Kinki University
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