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タイトル: Soil color analysis for statistically estimating total carbon, total nitrogen and active iron contents in Japanese agricultural soils
著者: Moritsuka, Naoki  KAKEN_id  orcid https://orcid.org/0000-0002-6473-6389 (unconfirmed)
Matsuoka, Kaori
Katsura, Keisuke  kyouindb  KAKEN_id
Sano, Shuji
Yanai, Junta
著者名の別形: 森塚, 直樹
キーワード: Active iron
Japanese agricultural soils
organic matter
paddy field
soil color reader (SPAD-503)
発行日: 17-Jun-2014
出版者: Taylor & Francis Group
誌名: Soil Science and Plant Nutrition
巻: 60
号: 4
開始ページ: 475
終了ページ: 485
抄録: Soil color originates mainly from organic matter, iron mineralogy and moisture content. We aimed to find a suitable method to measure soil color sensitively and to evaluate the extent to which the color parameters can be useful for statistically estimating total carbon (C), total nitrogen (N) and active iron (Fe) contents in Japanese agricultural soils. A soil color reader (SPAD-503) was applied to two sample sets: (1) 100 surface soils collected throughout a 0.5-ha paddy field (field scale) and (2) 147 surface soils collected from agricultural fields in Japan (national scale). For analysis with this instrument, about 2 g of air-dried, finely-ground samples were packed firmly in a plastic cell, and their colors as they appeared on windows in both sides of the cell were measured. A CIE 1976 (L[*], a[*], b[*]) color space was used for color description. For the field-scale samples, the values of the coefficient of variation were around 15% for total C, total N and acid oxalate extractable iron (Feo). The L[*] value (lightness) was negatively correlated with the content of total C and total N (R[2] = 0.18** and 0.26**, respectively), and the b[*] value (yellowness) was positively correlated with the Feo content (R[2] = 0.59[**]). For the national-scale samples, the values of the coefficient of variation were around 60% for total C, total N and Feo. The L[*] value was negatively correlated with the content of total C and total N (R[2] = 0.70** and 0.59[**], respectively), but the b[*] value was not correlated with the content of Feo (R[2] = 0.00). When the analysis was limited to 65 samples frequently used for paddy fields, the b[*] value was positively correlated with the Feo content (R[2] = 0.52[**]). In conclusion, the proposed method enabled us to measure soil color sensitively with a small sample size. The L[*] and b[*] values obtained can be useful for rapid estimation of total C, total N and Feo contents in agricultural surface soils in Japan.
著作権等: This is an Accepted Manuscript of an article published by Taylor & Francis in "Soil Science and Plant Nutrition" on 17 Jun 2014, available online: http://www.tandfonline.com/10.1080/00380768.2014.906295.
この論文は出版社版でありません。引用の際には出版社版をご確認ご利用ください。
This is not the published version. Please cite only the published version.
URI: http://hdl.handle.net/2433/198800
DOI(出版社版): 10.1080/00380768.2014.906295
出現コレクション:学術雑誌掲載論文等

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