| 季节性冻融期沼泽湿地CO2、CH4和N2O排放动态 |
| 摘要点击 1852 全文点击 1775 投稿时间：2004-10-12 修订日期：2004-12-14 |
| 查看HTML全文
查看全文 查看/发表评论 下载PDF阅读器 |
| 中文关键词 冻融作用 沼泽湿地 温室气体 三江平原 |
| 英文关键词 freezing and thawing mire greenhouse gas Sanjiang Plain |
|
| 中文摘要 |
| 三江平原季节性冻-融时间长达7～8个月,对沼泽湿地温室气体排放有重要影响.采用静态箱/气相色谱法研究了三江平原冻、融期沼泽湿地温室气体排放特征,表明三江平原不同类型沼泽湿地冬季都有明显的CH4和CO2排放,且冬季沼泽湿地CH4排放量在全年CH4排放中占有重要份额.融冻期沼泽湿地出现明显的CH4和CO2排放峰值,季节性积水沼泽化草甸CH4和CO2排放量大于常年积水沼泽湿地,而冬季常年积水沼泽湿地CH4排放通量大于季节性积水沼泽化草甸.融冻期CO2排放通量与土壤温度(5cm)呈指数相关关系(R2=0.912,p<0.001),沼泽湿地CO2排放通量与CH4通量间也呈显著正相关关系(R2=0.751,p<0.001).冬季三江平原沼泽湿地是N2O的汇,融冻期随着土壤温度升高逐渐成为N2O的源,且在5月份沼泽湿地表层土壤(0～20cm)融冻期间N2O排放通量明显增大.三江平原土壤冻、融期间沼泽湿地温室气体的排放特征,反映了冬季微生物活性的存在及融冻作用对土壤碳矿化和氮硝化、反硝化作用有重要影响. |
| 英文摘要 |
| In the Sanjiang Plain, the freezing and thawing phase have 7～8 months and play important role in the greenhouse gases emission. The characters of the greenhouse gases emission during freezing and thawing season in the Sanjiang Plain were studied, using the static chamber and gas chromatogram method. The results observed show that there were obvious CH4 and CO2 emissions in winter and the CH4 emission made a relatively large contribution to the total CH4 flux from the different type mires during the winter in the Sanjiang Plain. And there were significantly CH4 and CO2 emission peak values during thawing time. The CH4 and CO2 emissions fluxes from seasonal flooded mire were larger than that from continuously flooded mire during thawing time. On the contrary, the CH4 and CO2 emissions from continuously flooded mire were larger than that from seasonal flooded mire in winter. During thawing, there was exponential relationship between CO2 fluxes and the soil temperature(5cm)(R2=0.912,p<0.001). Meanwhile, CO2 fluxes was obviously correlated with the CH4 emission fluxes(R2=0.751,p<0.001). The mires are N2O sink in winter and gradually become N2O source, with increasing temperature during thawing time. The characters of the greenhouse gases emission, during freezing and thawing in the Sanjiang Plain respond to the microbial activity in winter and the effects of thawing on soil carbon mineralization, nitrification and denitrification. |
|
|
|
