水田
氮气
生长季节
温带气候
甲烷
有机质
农学
野外试验
土壤碳
化学
总有机碳
动物科学
环境化学
环境科学
土壤水分
植物
土壤科学
生物
有机化学
作者
Xunhua Zheng,Zaixing Zhou,Yuesi Wang,Jianguo Zhu,Yulong Wang,Jin Yue,Yi Shi,Kazuhiko Kobayashi,Kazuyuki Inubushi,Yao Huang,Shenghui Han,Zhongjun Xu,Baohua Xie,Klaus Butterbach‐Bahl,Lianxin Yang
标识
DOI:10.1111/j.1365-2486.2006.01199.x
摘要
Abstract Using the free‐air CO 2 enrichment (FACE) techniques, we carried out a 3‐year mono‐factorial experiment in temperate paddy rice fields of Japan (1998–2000) and a 3‐year multifactorial experiment in subtropical paddy rice fields in the Yangtze River delta in China (2001–2003), to investigate the methane (CH 4 ) emissions in response to an elevated atmospheric CO 2 concentration (200±40 mmol mol −1 higher than that in the ambient atmosphere). No significant effect of the elevated CO 2 upon seasonal accumulative CH 4 emissions was observed in the first rice season, but significant stimulatory effects (CH 4 increase ranging from 38% to 188%, with a mean of 88%) were observed in the second and third rice seasons in the fields with or without organic matter addition. The stimulatory effects of the elevated CO 2 upon seasonal accumulative CH 4 emissions were negatively correlated with the addition rates of decomposable organic carbon ( P <0.05), but positively with the rates of nitrogen fertilizers applied in either the current rice season ( P <0.05) or the whole year ( P <0.01). Six mechanisms were proposed to explain collectively the observations. Soil nitrogen availability was identified as an important regulator. The effect of soil nitrogen availability on the observed relation between elevated CO 2 and CH 4 emission can be explained by (a) modifying the C/N ratio of the plant residues formed in the previous growing season(s); (b) changing the inhibitory effect of high C/N ratio on plant residue decomposition in the current growing season; and (c) altering the stimulatory effects of CO 2 enrichment upon plant growth, as well as nitrogen uptake in the current growing season. This study implies that the concurrent enrichment of reactive nitrogen in the global ecosystems may accelerate the increase of atmospheric methane by initiating a stimulatory effect of the ongoing dramatic atmospheric CO 2 enrichment upon methane emissions from nitrogen‐poor paddy rice ecosystems and further amplifying the existing stimulatory effect in nitrogen‐rich paddy rice ecosystems.
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