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更埴地方の改良農地に生成した酸性硫酸塩土壌とその成因的考察
http://hdl.handle.net/10091/12490
http://hdl.handle.net/10091/12490db74fd33-5ce8-4de8-9c4f-be16e084651d
名前 / ファイル | ライセンス | アクション |
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Item type | 研究報告書 / Research Paper(1) | |||||
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公開日 | 2011-04-19 | |||||
タイトル | ||||||
言語 | ja | |||||
タイトル | 更埴地方の改良農地に生成した酸性硫酸塩土壌とその成因的考察 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | On the Acid Sulfate Soil at Reclaimed farm in Kohsyoku Region and its Genetic Considerations | |||||
言語 | ||||||
言語 | jpn | |||||
資源タイプ | ||||||
資源 | http://purl.org/coar/resource_type/c_18ws | |||||
タイプ | research report | |||||
著者 |
矢彦沢, 清允
× 矢彦沢, 清允× 山本, 満寿夫× 上野, 満夫× 藤松, 仁 |
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信州大学研究者総覧へのリンク | ||||||
氏名 | 藤松, 仁 | |||||
URL | http://soar-rd.shinshu-u.ac.jp/profile/ja.gCSNjekV.html | |||||
出版者 | ||||||
出版者 | 信州大学環境科学研究会 | |||||
引用 | ||||||
内容記述タイプ | Other | |||||
内容記述 | 環境科学年報15:105-110(1993) | |||||
書誌情報 |
環境科学年報 巻 15, p. 105-110, 発行日 1993-03-31 |
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抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | In Kohsyoku region,it has been found that the cropf .ai!ed reclaimed farms. Toc larify the cause,the soil induded in weathered and unweathered zones has beenivestigated by chemical analysis,s canning electron microscopic and X- ray diffraction method. 1n the soil of unweathered zones,v arious forms of framboidal mineralshave been found undei scanning electron microscope observations. The framboiqal minerals have been identified as pyrite by X -raydiffraction method. The pyrite content of subsoil was the range of 0.47 to 3.53 %ーThecontent of 3.53% in sedimentary muds is very high value. The yellow minerals found in the ridge between rice-fields has been identified as jarosite by X -ray diffraction method. The very acid soiJ was found to be drived from sulfuric acid which was produced by the oxidation of pyrite. It was then suggested that the acid soil is aa cid sulfate soi .l 1n the soil horizones con~aining pyrite,peat and so called Takasikozo have been coexisted. 1n addition,th e soil was ah eavy clay of drain ill. The region is af an irrigated by the Sanoh river that has the high acidity of sulfuric acid type. Accordingly,1t is then suggested that the framboidaJ pyrite in the deep subsoil in this farms has been formed by. sulfuric acid in Sanoh river. | |||||
資源タイプ(コンテンツの種類) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Article | |||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 0915-7492 | |||||
書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN1054947X | |||||
出版タイプ | ||||||
出版タイプ | VoR | |||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 |