成増付近の関東ローム層の粘土鉱物

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概要

• 論文の詳細を見る

• Clay mineralogical composition of a composite profile of the Kanto Loam Formation near Narimasu determined by the X-ray diffraction resulted as follows; The uppermost humic soil and Tachikawa Loam were dominated by allophane with a little quantities of 14Å minerals. he Musashino Loam was composed by halloysite with allophane, the uppermost buried soil horizon being characterized by the relatively high crystallinity of halloysite, and the intercalated Tokyo pumice bed by allophane. The Shimosueyoshi Loam was dominated by halloysite associated with 14Å minerals, the uppermost buried soil horizon being weathered to the more advanced stage. These results supported as a whole the prevailing information.

• 日本粘土学会の論文
• 1971-09-05

著者

• 松井 健

  群馬県立富岡高校

• 斎藤 賢一

  群馬県立富岡高校

関連論文

• 成増付近の関東ローム層の粘土鉱物
• 粘土およぴ土壌中の粘土鉱物同定における置換性カチオンの意義, Shurygina, E. A., (1960), Pochvovedenie, No.9., 1960, 87〜94.
• カオリン群鉱物の赤外吸収測定, Lyon, R. J. P. & Tuddenham, W. H., 1960, Nature., 185, No.4716, 835〜836.
• 粘土鉱物のX線回折標準物質としてのコレステロール, Kittrick, J. A., (1960), Soil Sci. Soc. Amer. Proc., 24, 17〜20.
• 愛鷹ローム層を母材とする累積性火山灰土の粘土鉱物

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