|
|
Seasonal characteristics of CH4 flux in a restored salt marsh wetland at Liao River estuary |
XING Qing-hui1, CHENG Hao1, LIU Si-qi1,2, XU Xue-mei1, CHEN Hong1, HAN Jian-bo1, DU Jin-qiu1 |
1. State Environmental Protection Key Laboratory of Marine Ecosystem Restoration, National Marine Environmental Monitoring Center, Dalian 116023, China; 2. College of Marine Ecology and Environment, Shanghai Ocean University, Shanghai 201306, China |
|
|
Abstract Using the Eddy Covariance (EC) technique, the seasonal characteristics of CH4 flux between a restored salt marsh and atmosphere were analyzed and its main influencing factors during the period between 2016~2021 in the Liao River estuary were determined. The results showed that the average diurnal fluctuation trend and range of CH4 flux values were different in four seasons in the restored salt marsh. The CH4 flux fluctuates around zero during the daytime in summer, autumn and winter. The peak CH4 emission occurred at 05:30, 01:30, 02:30 and 09:00 respectively in four seasons. On the whole, the salt marsh was usually shown as a CH4 source before 12:00 and a weak CH4 sink or an insignificant CH4 source/sink after 12:00. Both the amplitudes and average values of the diurnal variation of CH4 fluxes were winter, spring, summer and autumn in descending order in the restored salt marsh. The main influencing factors of CH4 release in the restored area were Ta, PAR and WS. In spring, Ta and CH4 flux were negatively correlated, while WS and CH4 flux were positively correlated, Ta and WS accounting for 43.8% of the CH4 flux variation. In summer, PAR and CH4 flux were negatively correlated, while PAR was significantly positively correlated with CH4 flux. In the restored salt marsh of the Liao River estuary, during the year of 2016~2021, the CH4flux values ranged from -60.9 to 155nmol/(m2·s) in different seasons, the average CH4 flux value was 14.05nmol/(m2·s). In general, the restored salt marsh acted as a CH4 source (5.32gC/(m2·a)), with a global warming potential (GWP) of 198.46g CO2-eq/m2.
|
Received: 11 April 2023
|
|
|
|
|
[1] |
IPCC. Climate change 2007:The physical science vasis [M]. Contribution of working group 1to the fourth assessment report of the intergovernmental panel on climate change. Cambridge University Press:Cambridge, 2007.
|
[2] |
丁维新,蔡祖聪.温度对甲烷产生和氧化的影响[J]. 应用生态学报, 2003,(4):604-608. Ding W X, Cai Z C. Effect of temperature on methane production and oxidation in soils [J]. Chinese Journal of Applied Ecology, 2003,14(4):604-608.
|
[3] |
许鑫王豪,赵一飞,邹欣庆,等.中国滨海湿CH4通量研究进展[J]. 自然资源学报, 2015,30(9):1594−1605. Xu X W H, Zhao Y F, Zhou X Q, et al. Advances in the research on methane emissions of coastal saline wetlands in China [J]. Journal of Natural Resources, 2015,30(9):1594-1605.
|
[4] |
Chen Q F, Guo B B, Zhao C S, et al. Characteristics of CH4 and CO2 emissions and influence of water and salinity in the Yellow River delta wetland, China [J]. Environmental Pollution, 2018,239:289-299.
|
[5] |
Gatland J R, Santos I R, Maher D T, et al. Carbon dioxide and methane emissions from an artificially drained coastal wetland during a flood:Implications for wetland global warming potential [J]. Journal of Geophysical Research:Biogeosciences, 2014,119(8):1698−1716.
|
[6] |
Sanders-DeMott R, Eagle M J, Kroeger K D, et al. Impoundment increases methane emissions in Phragmites-invaded coastal wetlands [J]. Global Change Biology, 2022,28(15):4539−4557.
|
[7] |
Gnanamoorthy P, Chakraborty S, Nagarajan R, et al. Seasonal variation of methane fluxes in a mangrove ecosystem in south India:An eddy covariance-based approach [J]. Estuaries and Coasts, 2022:1−16.
|
[8] |
马雪莹.辽河三角洲滨海湿地CO2和CH4释放通量及其影响因素研究[D]. 青岛:青岛大学, 2015. Ma X Y. Study on CO2 and CH4 emission fluxes and their influencing factors in Liao River delta wetland [D]. Qingdao:Qingdao University, 2015.
|
[9] |
袁晓敏,杨继松,刘凯,等.辽河口滨海湿地CH4排放特征及其影响因素[J]. 生态学报, 2019,39(5):1829−1837. Yuan X M, Yang J S, Liu K, et al. Characteristics and impact factors of methane emission in coastal wetland of the Liaohe estuary [J]. Acta Ecologica Sinica, 2019,39(5):1829−1837.
|
[10] |
贺文君.潮汐作用对黄河三角洲盐沼湿地生态系统CO2和CH4交换的影响[D]. 烟台:中国科学院大学(中国科学院烟台海岸带研究所), 2018. He W J. Effects of tides on ecosystem exchange of CO2 and CH4 over a salt marsh in the Yellow River Delta, China [D]. Yantai:University of Chinese Academy of Sciences (Yantai Institute of Coastal Zone Research), 2018.
|
[11] |
杨红霞,王东启,陈振楼,等.长江口崇明东滩潮间带甲烷(CH4)排放及其季节变化[J]. 地理科学, 2007,27(3):408−413. Yang H X, Wang D Q, Chen Z L, et al. Seasonal variation of CH4emission from Chongming east intertidal flat of Yangtze River estuary [J]. Geographical Science, 2007,27(3):408−413.
|
[12] |
胡泓,王东启,李扬杰,等.崇明东滩芦苇湿地温室气体排放通量及影响因素[J]. 环境科学研究, 2014,27(1):43−50. Hu H, Wang D Q, Li Y J, et al. Greenhouse gases fluxes at Chongming Dongtan Phragmites australis wetland and the influencing factors [J]. Research of Environmental Sciences, 2014,27(1):43-50.
|
[13] |
王蒙.杭州湾滨海湿地CH4,N2O,CO2排放通量及其影响因素研究[D]. 北京:中国林业科学研究院, 2014. Wang M. Study on CH4, N2O and CO2 fluxes and their influencing factors in Hangzhou Bay coastal wetland [D]. Beijing:Chinese Academy of Forestry, 2014.
|
[14] |
仝川,黄佳芳,王维奇,等.闽江口半咸水芦苇潮汐沼泽湿地甲烷动态[J]. 地理学报, 2012,67(9):1165−1180. Tong C, Huang J F, Wang W Q. Methane dynamics of a brackish-water tidal Phragmites australis marsh in the Minjiang River estuary [J]. Acta Geographica Sinica, 2012,67(9):1165−1180.
|
[15] |
曾从盛,王维奇,张林海,等.闽江河口短叶茳芏潮汐湿地甲烷排放通量[J]. 应用生态学报, 2010,(2):500−504. Zeng C S, Wang W Q, Zhang L H. Methane fluxes of Cyperus malaccensis tidal wetland in Minjiang River estuary. [J]. Chinese Journal of Applied Ecology, 2010,(2):500−504.
|
[16] |
Zhao X, Wang C, Li T, et al. Net CO2 and CH4 emissions from restored mangrove wetland:New insights based on a case study in estuary of the Pearl River, China [J]. Science of The Total Environment, 2022,811:151619.
|
[17] |
李森,蔡厚才,陈万东,等.海岸带生态恢复区不同林龄红树林对CH4和CO2排放通量的影响[J]. 生态环境学报, 2020,29(12):2414. Li S, Cai H C, Chen W D, et al. Analysis on CH4 and CO2 fluxes of mangroves with different ages in the coastal ecological restoration zone [J]. Ecology and Environmental Sciences, 2020,29(12):2414.
|
[18] |
Baldocchi D D. Assessing the eddy covariance technique for evaluating carbon dioxide exchange rates of ecosystems:past, present and future [J]. Global Change Biology, 2003,9(4):479−492.
|
[19] |
王宪礼,胡远满,布仁仓.辽河三角洲湿地的景观变化分析[J]. 地理科学, 1996,16(3):260−265. Wang X L, Hu Y M, Bu R C. Analysis of wetland landscape changes in Liao River delta [J]. Geographical Science, 1996,16(3):260−265.
|
[20] |
刘红玉,吕宪国,刘振乾,等.辽河三角洲湿地资源与区域持续发展[J]. 地理科学, 2000,(6):545-551. Liu H Y, Lv X G, Liu Z Q, et al. Study on wetland resources and regional sustainable development in Liaohe Delta [J]. Geographical Science,2000,(6):545-551.
|
[21] |
Rosentreter J A, Borges A V, Deemer B R, et al. Half of global methane emissions come from highly variable aquatic ecosystem sources [J]. Nature Geoscience, 2021,14(4):225−230.
|
[22] |
Al-Haj A N, Fulweiler R W. A synthesis of methane emissions from shallow vegetated coastal ecosystems [J]. Global Change Biology, 2020,26(5):2988-3005.
|
[23] |
Tong C, Wang W Q, Zeng C S, et al. Methane (CH4) emission from a tidal marsh in the Min River estuary, southeast China [J]. Journal of Environmental Science and Health, 2010,45(4):506-516.
|
[24] |
贾磊,张弥,蒲旖旎,等.养殖塘CH4通量时空变化特征及其影响因素[J]. 中国环境科学, 2021,41(6):2910-2922. Jia L, Zhang M, Pu Y N, et al. Temporal and spatial characteristics of methane flux and its influencing factors in a typical aquaculture pond [J]. China Environmental Science, 2021,41(6):2910-2922.
|
[25] |
Lin C W, Kao Y C, Chou M C, et al. Methane emissions from subtropical and tropical mangrove ecosystems in Taiwan [J]. Forests, 2020,11(4):470.
|
[26] |
Hu M, Sardans J, Yang X, et al. Patterns and environmental drivers of greenhouse gas fluxes in the coastal wetlands of China:A systematic review and synthesis [J]. Environmental research, 2020,186:109576.
|
[27] |
何露露.模拟恒定和波动盐度对河口湿地CH4通量,产甲烷菌及硫酸盐还原菌的影响[D]. 福州:福建师范大学, 2018. He L L. Effects of simulated constant and fluctuating salinity on CH4 fluxes, methanogens and sulfate-reducing bacteria estuarine wetland [D]. Fuzhou:Fujian Normal University, 2018.
|
[28] |
王晓丽,于建国.一个甲烷氧化菌株的分离,鉴定及其特性研究[J]. 微生物学通报, 2008,35(6):934-938. Wang X L, Yu J G. Isolation, identification and characterization of a methanotrophic strain [J]. Bulletin of microbiology, 2008,35(6):934-938.
|
[29] |
盛宣才,吴明,邵学新,等.模拟水位变化对杭州湾芦苇湿地夏季温室气体日通量的影响[J]. 生态学报, 2016,36(15):4792-4800. Sheng X C, Wu M, Shao X X,et al. Effects of simulated water levels on diurnal variation in the emission of three greenhouse gases in reed wetlands in summer. Acta Ecologica Sinica, 2016,36(15):4792-4800.
|
[30] |
Wang Y H, Yuan F M, Arndt K A, et al. Upscaling methane flux from plot level to eddy covariance tower domains in five Alaskan tundra ecosystems [J]. Frontiers in Environmental Science, 2022,10:939238.
|
[31] |
傅雪海,秦勇,杨永国,等.甲烷在煤层水中溶解度的实验研究[J]. 天然气地球科学, 2004,15(4):345−348. Fu X H, Qin Y, Yang Y G, et al. Experimental study of the solubility of methane in coalbed water [J]. Natural gas geoscience, 2004,15(4):345-348.
|
|
|
|