Nitrous oxide emission derived from soil organic matter decomposition from tropical agricultural peat soil in central Kalimantan, Indonesia(Environment)
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概要
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Our previous research showed large amounts of nitrous oxide (N_2O) emission (>200 kg N ha^<-1> year^<-1>) from agricultural peat soil. In this study, we investigated the factors influencing relatively large N_2O fluxes and the source of nitrogen (N) substrate for N_2O in a tropical peatland in central Kalimantan, Indonesia. Using a static chamber method, N_2O and carbon dioxide (CO_2) fluxes were measured in three conventionally cultivated croplands (conventional), an unplanted and unfertilized bare treatment (bare) in each cropland, and unfertilized grassland over a three-year period. Based on the difference in N_2O emission from two treatments, contribution of the N source for N_2O was calculated. Nitrous oxide concentrations at five depths (5-80 cm) were also measured for calculating net N_2O production in soil. Annual N fertilizer application rates in the croplands ranged from 472 to 1607 kg N ha^<-1> year^<-1>. There were no significant differences in between N_2O fluxes in the two treatments at each site. Annual N_2O emission in conventional and bare treatments varied from 10.9 to 698 and 6.55 to 858 kg N ha^<-1> year^<-1>, respectively. However, there was also no significant difference between annual N_2O emissions in the two treatments at each site. This suggests most of the emitted N_2O was derived from the decomposition of peat. There were significant positive correlations between N_2O and CO_2 fluxes in bare treatment in two croplands where N_2O flux was higher than at another cropland. Nitrous oxide concentration distribution in soil measured in the conventional treatment showed that N_2O was mainly produced in the surface soil down to 15 cm in the soil. The logarithmic value of the ratio of N_2O flux and nitrate concentration was positively correlated with water filled pore space (WEPS). These results suggest that large N_2O emission in agricultural tropical peatland was caused by denitrification with high decomposition of peat. In addition, N_2O was mainly produced by denitrification at high range of WFPS in surface soil.
- 一般社団法人日本土壌肥料学会の論文
著者
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DOHONG Salampak
パランカラヤ大農
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Darung Untung
UNPAR
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Dohong Salampak
Faculty Of Agriculture University Of Palangka Raya
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Takakai Fumiaki
北大院農
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Hatano Ryusuke
北大院農
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Limin Suwido
Fac. Of Agriculture Palangkaraya Univ.
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Hatano Ryusuke
Soil Science Laboratory Graduate School Of Agriculture Hokkaido University
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Hatano Ryusuke
Research Faculty Of Agriculture Hokkaido University
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Takakai Fumiaki
Faculty Of Bioresource Sciences Akita Prefectural University
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Toma Yo
Graduate School Of Agriculture Hokkaido Univ. Sapporo 060-8589 Jpn
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Takakai Fumiaki
Akita Prefectural Univ. Akita
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Limin Suwido
Faculty Of Agriculture Palangka Raya University
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Darung Untung
Faculty Of Agriculture Palangka Raya University
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Toma Yo
Field Science Center For Northern Biosphere Hokkaido University
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Kuramochi Kanta
北大 大学院
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Hatano Ryusuke
北大 大学院
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Kuramochi Kanta
Research Faculty Of Agriculture Hokkaido University
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