Song Chang-chun, Zhang Li-hua, Wang Yi-yong, Zhao Zhi-chun
Northeast Institute of Geography and Agricultural Ecology, Chinese Academy of Sciences, Changchun 130012, China.
Huan Jing Ke Xue. 2006 Dec;27(12):2369-75.
Annual dynamics of CO2, CH4, N2O emissions from freshwater marshes and affected by nitrogen fertilization were studied in situ in Sanjiang Plain of Northeast China from June 2002 to December 2004, using the static opaque chamber-GC techniques. The results showed that there was significant seasonal and annual variation in the CO2, CH4 and N2O emissions. The ecosystem emission of CO2 reached a maximum of 779.33- 965.40 mg x (mxh)(-1) in July and August, CH4 reached a maximum of 19.19-30.52 mg x (mxh)(-1) in August, N2O reached a maximum of 0.072-0.15 mgx (mxh)(-1) in May and September, respectively. While the minimum of the CO2, CH4, N2O emission was 2.36-18.73 mg x (mxh)(-1), - 0.35 - 0.59 mg x (mxh)(-1), - 0.032- 0.009 mg (mxh)(-1), respectively, which occurs in winter. The freshwater marsh was the sink of N2O in winter. Temperature was a primary factor, controlling greenhouse gas seasonal emissions in freshwater marshes; while the precipitation and floodwater depth were the dominating influencing factors, affecting the greenhouse gas annual variations. Especially, the influence of precipitation on CH4 emissions was more obvious, comparing with the CO2 and N20 emissions. And the summer higher CH4 emission was mainly induced by the ice and snow thawing water in winter. Respiration of the ecosystem and CH4 emission were exponentially dependent on soil temperature of 5cm depth, while the N2O emission was not related to the soil temperature and water depth. The greenhouse gas (CO2, CH4, N2O) emissions were significantly influenced by nitrogen fertilization in Sanjiang Plain. The CO2, CH4, N2O flux of fertilization increased 34% , 145% , 110% , respectively, comparing to the control treatment.
2002年6月至2004年12月,在中国东北三江平原,采用静态不透明箱-气相色谱技术,对淡水沼泽二氧化碳、甲烷、氧化亚氮排放的年动态变化以及氮肥对其的影响进行了原位研究。结果表明,二氧化碳、甲烷和氧化亚氮排放存在显著的季节和年际变化。生态系统二氧化碳排放在7月和8月达到最大值,为779.33 - 965.40毫克×(平方米·小时)⁻¹,甲烷在8月达到最大值,为19.19 - 30.52毫克×(平方米·小时)⁻¹,氧化亚氮分别在5月和9月达到最大值,为0.072 - 0.15毫克×(平方米·小时)⁻¹。而二氧化碳、甲烷、氧化亚氮排放的最小值分别为2.36 - 18.73毫克×(平方米·小时)⁻¹、 - 0.35 - 0.59毫克×(平方米·小时)⁻¹、 - 0.032 - 0.009毫克×(平方米·小时)⁻¹,出现在冬季。淡水沼泽在冬季是氧化亚氮的汇。温度是控制淡水沼泽温室气体季节排放的主要因素;而降水和洪水深度是影响温室气体年际变化的主导因素。特别是,与二氧化碳和氧化亚氮排放相比,降水对甲烷排放的影响更为明显。夏季较高的甲烷排放主要是由冬季冰雪融化水引起的。生态系统呼吸和甲烷排放与5厘米深度土壤温度呈指数关系,而氧化亚氮排放与土壤温度和水深无关。三江平原的氮肥对温室气体(二氧化碳、甲烷、氧化亚氮)排放有显著影响。与对照处理相比,施肥处理的二氧化碳、甲烷、氧化亚氮通量分别增加了34%、145%、110%。