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京都府丹後地方および愛知県三河地方の森林土壌の鉱物学的研究(農芸化学部門)
https://kpu.repo.nii.ac.jp/records/4750
https://kpu.repo.nii.ac.jp/records/47502ace3246-1edc-4987-b27a-e61dee3647d2
名前 / ファイル | ライセンス | アクション |
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Item type | [ELS]紀要論文 / Departmental Bulletin Paper(1) | |||||||||||||
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公開日 | 2017-02-20 | |||||||||||||
タイトル | ||||||||||||||
タイトル | 京都府丹後地方および愛知県三河地方の森林土壌の鉱物学的研究(農芸化学部門) | |||||||||||||
言語 | ja | |||||||||||||
その他(別言語等) | ||||||||||||||
その他のタイトル | Mineralogical studies of forest soils in Kyoto and Aichi prefecture (Agricultural Chemistry) | |||||||||||||
言語 | en | |||||||||||||
言語 | ||||||||||||||
言語 | jpn | |||||||||||||
資源タイプ | ||||||||||||||
資源タイプ | departmental bulletin paper | |||||||||||||
著者 |
服部, 共生
× 服部, 共生
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抄録(日) | ||||||||||||||
内容記述タイプ | Other | |||||||||||||
内容記述 | 京都府丹後地方の酸性褐色森林土地帯と愛知県三河地方の赤黄色土地帯に分布する種々母材を異にする土壌の鉱物学的研究を行ない。次の結果を得た。これらの2つの土壌生成作用に伴つて起こる粘土の風化生成過程には著しい相違は両者の間に認められず, 現気候条件下で安定と思われる風化最終産物はハロイサイト, ギブサイトであつた。しかし現在土壌中にみられる粘土鉱物は母材および土壌生成作用を受けた時間により差異があることを明らかにした。 | |||||||||||||
言語 | ja | |||||||||||||
抄録(英) | ||||||||||||||
内容記述タイプ | Other | |||||||||||||
内容記述 | The mineralogical studies of the forest soils in Tango of Kyoto Prefecture and in Mikawa of Aichi Prefecture, which are developed on the various rocks under the climatic conditions of the formation of brown forest soil and red yellow soil, were performed. The petrographic methods were applied for the studies of sand fractions and the X-ray diffraction procedure, the differential thermal analysis and the other methods for sand and clay fractions. The results were summerized as follows. The sand fractions were containing the considerable amount of clay minerals in Tango soils, but the small amount in Mikawa soils except in the serpentine soil. The species of clay minerals in sand fractions were resemble to the ones in clay fractions. The various clay mineral species were detected in the clay fractions due to the variations of par ent material and the differences of soil age. But it was considered that there were no marked differences on the processes of clay formation occured during the forming processes of brown forest soil in Tango and red yellow soil in Mikawa, and the most stable weathering products were halloysite and gibbsite under present climatic conditions. | |||||||||||||
言語 | en | |||||||||||||
書誌情報 |
ja : 京都府立大學學術報告. 農學 en : The scientific reports of Kyoto Prefectural University. Agriculture 巻 15, p. 83-88, 発行日 1963-09-01 |
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雑誌書誌ID | ||||||||||||||
収録物識別子タイプ | NCID | |||||||||||||
収録物識別子 | AN00062275 | |||||||||||||
ISSN | ||||||||||||||
収録物識別子タイプ | PISSN | |||||||||||||
収録物識別子 | 00757373 |