Effect of chemical fertilizer and manure application on N_2O emission from reed canary grassland in Hokkaido, Japan
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- Jin Tao JIN Tao
- Soil Science Laboratory, Graduate School of Agriculture, Hokkaido University
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- Shimizu Mariko SHIMIZU Mariko
- Soil Science Laboratory, Graduate School of Agriculture, Hokkaido University
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- Marutani Satoru [他] MARUTANI Satoru
- Soil Science Laboratory, Graduate School of Agriculture, Hokkaido University
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- DESYATKIN Alexey R.
- Soil Science Laboratory, Graduate School of Agriculture, Hokkaido University
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- IIZUKA Natsumi
- Soil Science Laboratory, Graduate School of Agriculture, Hokkaido University
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- HATA Hiroshi
- Field Science Center for Northern Biosphere, Agro-ecosystem Research Station, Shizunai Livestock Farm, Hokkaido University
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- HATANO Ryusuke
- Soil Science Laboratory, Graduate School of Agriculture, Hokkaido University
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著者
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- Jin Tao JIN Tao
- Soil Science Laboratory, Graduate School of Agriculture, Hokkaido University
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- Shimizu Mariko SHIMIZU Mariko
- Soil Science Laboratory, Graduate School of Agriculture, Hokkaido University
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- Marutani Satoru [他] MARUTANI Satoru
- Soil Science Laboratory, Graduate School of Agriculture, Hokkaido University
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- DESYATKIN Alexey R.
- Soil Science Laboratory, Graduate School of Agriculture, Hokkaido University
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- IIZUKA Natsumi
- Soil Science Laboratory, Graduate School of Agriculture, Hokkaido University
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- HATA Hiroshi
- Field Science Center for Northern Biosphere, Agro-ecosystem Research Station, Shizunai Livestock Farm, Hokkaido University
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- HATANO Ryusuke
- Soil Science Laboratory, Graduate School of Agriculture, Hokkaido University
抄録
We evaluated the effect of chemical fertilizer and manure applications on N2O emission from a managed grassland by establishing three treatment plots of chemical N fertilizer (chemical fertilizer), manure combined chemical N fertilizer (manure) and no N fertilizer (control) at the Shizunai Experimental Livestock Farm in southern Hokkaido, Japan. N2O fluxes from soils were measured by a closed-chamber method from May 2005 to April 2008. Soil denitrifying enzyme activity (DEA) in root-mat layer (0-2.5cm) and mineral soil layer (2.5-5cm) of each treatment plot was measured by an acetylene inhibition method after treatment with NO^[-]_[3]-N and glucose addition and neither NO^[-]_[3]-N nor glucose addition, respectively. Annual N2O emission ranged from 0.6 4.9 kg N2O-N ha^[-1]yr^[-1], with the highest observed in manure plot and lowest in control plot. Chemical fertilizer-induced emission factor (EF) (range: 0.85-1.32%) was significantly higher than manure-induced EF (range 0.35-0.85%). Denitrification potential of soil horizons was measured with addition of both NO^[-]_[3]-N and glucose, which was significantly higher in root-mat soil than that in mineral soil. Soil DEA in root-mat in NO^[-]_[3]-N addition with and without addition of glucose had a significantly positive correlation with soil pH (P < 0.05). Soil pH was significantly influenced by N source, which was significantly lower in chemical fertilizer plot than that in control and manure plot. For a fixed quantity of available N, the application of manure could result in higher N2O emission compared with chemical fertilizer owing to high soil pH values under manure application than under chemical fertilizer application.
We evaluated the effect of chemical fertilizer and manure applications on N_2O emission from a managed grassland by establishing three treatment plots of chemical N fertilizer (chemical fertilizer), manure combined with chemical N fertilizer (manure) and no N fertilizer (control) at the Shizunai Experimental Livestock Farm in southern Hokkaido, Japan. The N_2O fluxes from the soils were measured using a closed-chamber method from May 2005 to April 2008. Soil denitrifying enzyme activity (DEA) in the root-mat layer (0-2.5cm) and in the mineral soil layer (2.5-5cm) of each treatment plot was measured using an acetylene inhibition method after treatment with NO_3^--N addition, glucose addition, both NO_3^--N and glucose addition or neither NO_3^--N nor glucose addition. Annual N_2O emission ranged from 0.6 to 4.9kg N_2O-N ha^<-1> year^<-1>, with the highest emission observed in the manure plot and the lowest in the control plot. The chemical fertilizer induced emission factor (EF) (range: 0.85-1.32%) was significantly higher than the manure-induced EF (range: 0.35-0.85%). The denitrification potential of the soil horizons was measured with the addition of both NO_3^--N and glucose, and was significantly higher in root-mat soil than in mineral soil. Soil DEA in the root mat with the addition of NO_3^--N with and without the addition of glucose had a significantly positive correlation with soil pH (P<0.05). Soil pH was significantly influenced by N source, which was significantly lower in the chemical fertilizer plot than in the control and manure plots. For a fixed quantity of available N, the application of manure could result in higher N_2O emission compared with chemical fertilizer, owing to higher soil pH values under manure application than under chemical fertilizer application.
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), 53-65, 2010-02-01
一般社団法人日本土壌肥料学会
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