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大阪中河内地区の堆積層序とその土壌
https://kindai.repo.nii.ac.jp/records/4957
https://kindai.repo.nii.ac.jp/records/4957a69506b7-a168-49c2-b8c9-357d87bdb8de
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
AN00064044-19920315-0033.pdf (1.1 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 | 大阪中河内地区の堆積層序とその土壌 | |||||||||
| タイトル | ||||||||||
| タイトル | Horizon Sequences and the Soil of the Osaka Naka-Kawachi Alluvium | |||||||||
| 言語 | en | |||||||||
| 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) | ||||||||||
| 言語 | en | |||||||||
| 値 | Kawamura, Saburo | |||||||||
| 著者 所属 | ||||||||||
| 値 | 近畿大学農学部農芸化学科植物栄養・土壌学研究室 | |||||||||
| 著者所属(翻訳) | ||||||||||
| 値 | Laboratory of Plant Nutrition and Soil Science, 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 25, p. 33-42, 発行日 1992-01-01 |
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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 | The character of soil horizon sequences was studied in relation to the past and present surface of the soil. The soil horizon sequences at sampled locations showed the processes of soil accumulation, but each soil layer accompanies the action of soil formation at the surface of the ground. Plain formation by an alluvium shows a shallow underground water level, and is piled up in reductive soil according to each period and the microconfiguration on the ground. In the soil horizon sequences, the content of organic matter in layers of oxidative soil was low, and iron was seen as a reddish mottling. In reductive layers, organic matter decomposed slowly, so the content of organic matter was high. The iron content was the same as in the oxidative layer. The mean phosphate content of the soil samples reseached were 34% of the mean value for farm lands in Japan, and the phosphate and iron concentrations were correlated. The fertility of buried field soils that had been used from the Yayoi to the Edo period for rice culture was comparable to that of present paddy field soil. From these results, it seems likely that manure in early rice culture of Tanan had been practised. | |||||||||
| 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 |
AN00064044-19920315-0033.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 | |||||||||
