Use of the RothC model to estimate the carbon sequestration potential of organic matter application in Japanese arable soils
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- Yokozawa Masayuki YOKOZAWA Masayuki
- National Institute for Agro-Environmental Sciences
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- Shirato Yasuhito SHIRATO Yasuhito
- National Institute for Agro-Environmental Sciences
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- Sakamoto Toshihiro [他] SAKAMOTO Toshihiro
- National Institute for Agro-Environmental Sciences
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- YONEMURA Seiichirou
- National Institute for Agro-Environmental Sciences
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- NAKAI Makoto
- National Institute for Agro-Environmental Sciences
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- OHKURA Toshiaki
- National Institute for Agro-Environmental Sciences
この論文をさがす
著者
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- Yokozawa Masayuki YOKOZAWA Masayuki
- National Institute for Agro-Environmental Sciences
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- Shirato Yasuhito SHIRATO Yasuhito
- National Institute for Agro-Environmental Sciences
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- Sakamoto Toshihiro [他] SAKAMOTO Toshihiro
- National Institute for Agro-Environmental Sciences
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- YONEMURA Seiichirou
- National Institute for Agro-Environmental Sciences
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- NAKAI Makoto
- National Institute for Agro-Environmental Sciences
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- OHKURA Toshiaki
- National Institute for Agro-Environmental Sciences
抄録
We estimated the carbon (C) sequestration potential of organic matter application in Japanese arable soils at a country scale by applying the Rothamsted carbon (RothC) model at a 1-km resolution. After establishing the baseline soil organic carbon (SOC) content for 1990, a 25-year simulation was run for four management scenarios: A (minimum organic matter application), B (farmyard manure application), C (double cropping for paddy fields) and D (both B and C). The total SOC decreased during the simulation in all four scenarios because the C input in all four scenarios was lower than that required to maintain the baseline 1990 SOC level. Scenario A resulted in the greatest depletion, reflecting the effects of increased organic matter application in the other scenarios. The 25-year difference in SOC accumulation between scenario A and scenarios B, C and D was 32.3, 11.1 and 43.4Mt C, respectively. The annual SOC accumulation per unit area was similar to a previous estimate, and the 25-year averages were 0.30, 0.10 and 0.41t C ha^<-1> year^<-1> for scenarios B, C and D, respectively. The system we developed in the present study, that is, linking the RothC model and soil spatial data, can be useful for estimating the potential C sequestration resulting from an increase in organic matter input to Japanese arable soils, although more feasible scenarios need to be developed to enable more realistic estimation.
収録刊行物
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- Soil science and plant nutrition
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Soil science and plant nutrition 56(1), 168-176, 2010-02-01
一般社団法人日本土壌肥料学会
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