globalchange  > 气候变化与战略
CSCD记录号: CSCD:5142931
论文题名:
夏季九龙江口红树林土壤-大气界面温室气体通量的研究
其他题名: Summer fluxes of atmospheric greenhouse gases from mangrove soils in Jiulongjiang Estuary
作者: 余丹1; 陈光程2; 陈顺洋2; 陈雅萍1; 陈彬2; 叶勇1; 侯建平2
刊名: 应用海洋学学报
ISSN: 2095-4972
出版年: 2014
卷: 33, 期:2, 页码:1181-1192
语种: 中文
中文关键词: 海洋化学 ; 九龙江口 ; 温室气体 ; 通量 ; 土壤 ; 红树林 ; 夏季
英文关键词: marine chemistry ; Jiulongjiang Estuary ; greenhouse gases ; flux ; soil ; mangrove ; summer
WOS学科分类: OCEANOGRAPHY
WOS研究方向: Oceanography
中文摘要: 红树林湿地土壤是一个潜在的温室气体排放源.调查了夏季福建九龙江口的秋茄(Kandelia candel)红树林湿地土壤-大气界面3种温室气体的通量并分析土壤环境对其的影响.研究结果显示,九龙江口红树林夏季3种温室气体N_2 O、CH_4和CO_2的通量分别是0.27~2.45、-0.28~341.43mumol /(m~2· h)和-0.49~17.00 mmol/(m~2· h),表明九龙江口夏季红树林土壤总体上是温室气体的排放源.根据3种温室气体的平均通量及其增温潜力计算它们的CO_2当量通量以反映3种温室气体产生的增温效应,计算结果显示九龙江口红树林夏季土壤排放温室气体的CO_2当量通量为82.33~674.92 mg /(m~2· h),而CO_2是最大的贡献因素.双因素方差分析结果表明,CO_2通量和土壤理化性质因林地和滩面而异,CH_4通量受林地的影响,但N_2 O通量则不受林地和滩面的影响.相关性分析结果显示,土壤环境因子是影响红树林温室气体通量空间差异的重要原因,其中土壤有机质、氨态氮和总氮含量是影响N_2 O和CO_2通量的主要因子,而CH_4则只与土壤氧化还原电位显著相关.
英文摘要: Mangrove swamps are considered to be a potential net source of greenhouse gases,but the fluxes of greenhouse gases from mangrove soils are still poorly characterized.The present study,conducted in July 2012 in 3 Kandelia candel mangrove forests in Jiulongjiang Estuary in southern China,aimed to investigate the summer fluxes of N_2 O,CH_4 and CO_2 from the soil and the role of soil characteristics in regulating gas fluxes.Gas fluxes ranged from 0.27 to 2.45 mumol/(m~2· h),-0.28 to 341.43 mumol/(m~2· h)and -0.49 to 17.00 mmol/(m~2· h) for N_2 O,CH_4 and CO_2, respectively,indicating that mangrove soil was an emission source of greenhouse gases in Jiulongjiang Estuary in summer.Total CO_2-equivalent fluxes of the three gases,indicating their global warming po-tential,ranged from 82.33 to 674.92 mg /(m~2 · h),and CO_2 was the most dominant in the total flux in the man-groves.This study recorded higher CO_2 at the landward site than middle zone and seaward site,while there were no differences in both N_2 O and CH_4 fluxes among different tidal positions.Soil characteristics also varied with mangrove transect or sampling position.These characteristics,especially nutrient contents were factors regulating greenhouse gases emissions and their spatial variations in mangrove.N_2 O and CO_2 fluxes were positively related to soil organic matter,ammonium and total nitrogen concentrations,and CH_4 flux showed significant and negative correlation with the redox potential(E_h).
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/148554
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作者单位: 1.厦门大学环境与生态学院, 厦门, 福建 361102, 中国
2.国家海洋局第三海洋研究所, 厦门, 福建 361005, 中国

Recommended Citation:
余丹,陈光程,陈顺洋,等. 夏季九龙江口红树林土壤-大气界面温室气体通量的研究[J]. 应用海洋学学报,2014-01-01,33(2):1181-1192
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