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泥炭層出現深度と上位層の母材判定に基づく酪農学園元野幌農場の土壌区分図
http://hdl.handle.net/10659/0002000032
http://hdl.handle.net/10659/0002000032a5edc7c7-4432-4d2c-827f-6d59c3d8f644
名前 / ファイル | ライセンス | アクション |
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S-48-1-1-11.pdf
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||||||||||||||
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公開日 | 2023-10-17 | |||||||||||||||||
タイトル | ||||||||||||||||||
言語 | ja | |||||||||||||||||
タイトル | 泥炭層出現深度と上位層の母材判定に基づく酪農学園元野幌農場の土壌区分図 | |||||||||||||||||
タイトル | ||||||||||||||||||
言語 | ja-Kana | |||||||||||||||||
タイトル | デイタンソウ シュツゲン シンド ト ジョウイソウ ノ ボザイ ハンテイ ニ モトヅク ラクノウ ガクエン モトノッポロ ノウジョウ ノ ドジョウ クブンズ | |||||||||||||||||
タイトル | ||||||||||||||||||
言語 | en | |||||||||||||||||
タイトル | Soil map derived from survey on depth of upper boundary of peat layer and parent material of upper layer in Moto-Nopporo Farm | |||||||||||||||||
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 | |||||||||||||||||
アクセス権 | ||||||||||||||||||
アクセス権 | open access | |||||||||||||||||
アクセス権URI | http://purl.org/coar/access_right/c_abf2 | |||||||||||||||||
著者 |
三枝,俊哉
× 三枝,俊哉
WEKO
1667
× 西元,佑輔
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抄録 | ||||||||||||||||||
内容記述タイプ | Abstract | |||||||||||||||||
内容記述 | A soil map was drawn in Moto-Nopporo Farm of Rakuno Gakuen Field Education and Research Center. Moto-Nopporo Farm has 4 Filed groups as follows, 16.9 ha of Group I consists of 3 swards (I1-I3), 21.7 ha of Group II consists of 10 swards (II1-II10), 20.0 ha of Group III consists of 4 swards (III2-III5), and 17.3 ha of Group IV consists of 4 swards (IV1, IV2, IV4, IV5). 4 soil types were distributed in this farm as results of soil profile survey, Transitional-moor Peat soils, Sapric Peat soils, Haplic Gray Lowland soils, and Lowland Reformed soils. The depth of the upper boundary of the Transitional-moor Peat layer and GPS location data was surveyed as densely as possible on a rough grid for all swards. An isobath at 25 cm depth was extracted by spatial statistical processing using the IDW interpolation method. This was considered as the boundary of the surface Transitional-moor Peat soils. The parent material of soil material covering the upper layer was detected at a depth of the upper boundary of the Transitional-moor Peat layer greater than 25 cm. Spatial statistics using spline interpolation were used to classify Haplic Gray Lowland soils and Sapric Peat soils. Haplic Gray Lowland soils were distributed in the whole area of I1, I2, II7, and parts area of II1, II8, II9, II10, III5. Sapric Peat soils were distributed in whole area of II2, II3, II4, and parts area of II1, II5, II6, II8, II9, II10, III3, III4. Transitional-moor Peat soils were distributed in the whole area of Group IV, III2, and parts area of II5, II6, III3, III4. In general, these soil maps matched up well with the soil maps issued by the National Agriculture and Food Research Organization in the Japanese Soil Inventory. | |||||||||||||||||
言語 | en | |||||||||||||||||
書誌情報 |
ja : 酪農学園大学紀要. 自然科学編 巻 48, 号 1, p. 1-11, 発行日 2023-10 |
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ISSN | ||||||||||||||||||
収録物識別子タイプ | EISSN | |||||||||||||||||
収録物識別子 | 2187-0500 | |||||||||||||||||
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識別子タイプ | NCID | |||||||||||||||||
関連識別子 | AN00247860 | |||||||||||||||||
著者版フラグ | ||||||||||||||||||
出版タイプ | VoR | |||||||||||||||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||||||||||||||
出版者 | ||||||||||||||||||
言語 | ja | |||||||||||||||||
出版者 | 酪農学園大学 | |||||||||||||||||
資源タイプ | ||||||||||||||||||
内容記述タイプ | Other | |||||||||||||||||
内容記述 | Bulletin | |||||||||||||||||
言語 | ja |