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土壌鉱質粒子分散系におけるシルト部分のストークス径による粒度測定法
https://kindai.repo.nii.ac.jp/records/4843
https://kindai.repo.nii.ac.jp/records/4843b6befb63-7355-4660-8429-552eb564cf45
名前 / ファイル | ライセンス | アクション |
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AN00064044-20010331-0181.pdf (1.5 MB)
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Item type | ☆紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2008-01-28 | |||||
タイトル | ||||||
タイトル | 土壌鉱質粒子分散系におけるシルト部分のストークス径による粒度測定法 | |||||
その他(別言語等)のタイトル | ||||||
その他のタイトル | Method of measurement of soil silt size distribution by the stokes diameter in a soil mineral particle suspension | |||||
著者 |
川村, 三郎
× 川村, 三郎 |
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言語 | ||||||
言語 | jpn | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
資源タイプ | departmental bulletin paper | |||||
著者(英) | ||||||
en | ||||||
Kawamura, Saburo | ||||||
著者 所属 | ||||||
近畿大学農学部農芸化学科 | ||||||
著者所属(翻訳) | ||||||
Department of Agricultural Chemistry, Faculty of Agriculture, Kinki University | ||||||
版 | ||||||
出版タイプ | NA | |||||
出版タイプResource | http://purl.org/coar/version/c_be7fb7dd8ff6fe43 | |||||
出版者 名前 | ||||||
出版者 | 近畿大学農学部 | |||||
書誌情報 |
近畿大学農学部紀要 en : Memoirs of the Faculty of Agriculture of Kinki University 号 34, p. 181-187, 発行日 2001-01-01 |
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ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 04538889 | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | It is very important for the detailed distribution of soil silt particle to realize the state as narrow a range as detectable. The automatic electrical balance can be measured continuously the contents of settling silt particles in soil suspension at a given time. According to the Stokes law, the contents of silt particles corresponding to available size range taken as subdivided range of the silts portion, can be understood as the soil properties themselves. A narrow size range provided reliable data as regards the content of different silt particles. Results were obtained from the charges in increment observed by weighing particles at a given time. Soil silt particle-size distribution characterizes soil according to a range of sizes. There is a need for reliable distribution diagrams with subdivided size ranges. Such detailed diagrams are necessary because of the expression of principal large-size classes such as international division of silt particle. Moreover, such diagrams would benefit studies attempting to describe details about soil texture. Application of this study necessitate understanding physico-chemical, soil genetic and ceramic properties of soil particle ; such an understanding may be enhanced by realistic silt particle-size distribution diagarams. | |||||
内容記述 | ||||||
内容記述タイプ | Other | |||||
内容記述 | 記事区分:原著 | |||||
サムネイル |
AN00064044-20010331-0181.jpeg |
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フォーマット | ||||||
内容記述タイプ | Other | |||||
内容記述 | application/pdf |