CLAY MINERALOGY OF SOME VOLCANIC ASH SOILS IN WHICH CRISTOBALITE PREDOMINATES
スポンサーリンク
概要
- 論文の詳細を見る
The clay mineralogical composition of soils on volcanic ashes from Mashu^^- and Kamuinupuri-dake volcanoes, Hokkaido, which are rich in cristobalite, was determined using petrological, X-ray diffraction, differential thermal, and selective dissolution and differential infrared spectroscopic methods. The cristobalite occurred in abundance in every size of fraction from coarse sand to clay and every soil from approximately 1,700to 8,400 years old, and was concluded to be of igneous origin. The major clay minerals were allophanelike constituents and allophane with some layer silicates as the minor clay mineral, being similar to those of andesitic ash soils and different from those of volcanic ash soils containing abundant quartz. The quartz of volcanic ashes was presumed to bederived from the groundmass-equivalent portion of the ashes which had been formed from magma at a low temperature.
- 社団法人日本土壌肥料学会の論文
著者
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MIZOTA Chitoshi
Faculty of Agriculture, Iwate University
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Mizota Chitoshi
Faculty Of Agriculture Iwate University
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AOMINE SHIGENORI
Faculty of Agriculture, Kyushu University
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Aomine Shigenori
Faculty Of Agriculture Kyushu University
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Mizota Chitoshi
Faculty Of Agricultuer Iwate University
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