Song Changchun, Zhang Jinbo, Wang Yiyong, Wang Yaosi, Zhao Zhichun
Chinese Academy Sciences, Northeast Institute of Geography and Agricultural Ecology, CAS, Changchun, Jilin 130012, China.
J Environ Manage. 2008 Aug;88(3):428-36. doi: 10.1016/j.jenvman.2007.03.030. Epub 2007 May 22.
The wetlands play an important role in carbon storage, especially at high latitudes, at which they store nearly one-third of global soil carbons. However, few studies have investigated the emissions of CO(2), CH(4) and N(2)O in the long-term, especially effects of freeze-thaw cycles on these gases emissions in freshwater marsh ecosystems. In this paper, we collected greenhouse gas emission data from a freshwater marsh area in China for 4 years, evaluated their release variables and speculated on their potential atmospheric impact. For this paper, we report on the CO(2), CH(4) and N(2)O emission rates recorded from June 2002 to November 2005 in the Sanjiang Plain of northeast China. We measured their interannual variations and fluctuations, as well as factors affecting their emissions, and estimated their regulation and freeze-thaw cycle impacts. Our results revealed obvious CO(2) and CH(4) emission fluctuations during the winter months, and during the freeze-thaw cycle, and a strong interannual variation during the growing season. Overall, we documented a close relationship between the CO(2) and CH(4) emissions, implicating some regulatory commonality. We determined that the marsh was a N(2)O sink during the winter, but a significant source of N(2)O during the freeze-thaw cycle as the temperature increased, especially in early summer. During the thaw-freeze period, the N(2)O levels were positively correlated with the water depth. Additionally, water depth greatly governed the interannual variation of the N(2)O emissions from the marshes during the thaw-freeze period.
湿地在碳储存中发挥着重要作用,尤其是在高纬度地区,它们储存了全球近三分之一的土壤碳。然而,很少有研究长期调查二氧化碳、甲烷和氧化亚氮的排放情况,特别是冻融循环对淡水沼泽生态系统中这些气体排放的影响。在本文中,我们收集了中国一个淡水沼泽地区4年的温室气体排放数据,评估了它们的释放变量,并推测了它们对大气的潜在影响。在本文中,我们报告了2002年6月至2005年11月在中国东北三江平原记录的二氧化碳、甲烷和氧化亚氮排放率。我们测量了它们的年际变化和波动情况,以及影响它们排放的因素,并估计了它们的调节作用和冻融循环的影响。我们的结果显示,冬季和冻融循环期间二氧化碳和甲烷排放有明显波动,生长季节有强烈的年际变化。总体而言,我们记录了二氧化碳和甲烷排放之间的密切关系,这意味着存在一些共同的调节机制。我们确定,该沼泽在冬季是氧化亚氮的汇,但在冻融循环期间,随着温度升高,尤其是在初夏,是氧化亚氮的重要排放源。在融冻期,氧化亚氮水平与水深呈正相关。此外,水深在很大程度上控制了融冻期沼泽氧化亚氮排放的年际变化。