闽江河口芦苇潮汐湿地甲烷通量及主要影响因子

2007年利用静态箱-气相色谱仪法对闽江河口区最大的鳝鱼滩芦苇湿地和入侵种互花米草斑块涨潮前、涨落潮过程及落潮后甲烷通量季节动态进行了原位测定,并利用室内培养-气相色谱仪法测定了芦苇湿地不同土层土壤甲烷产生潜力.结果表明,鳝鱼滩芦苇湿地全年均属于大气甲烷的排放源,排放通量具有明显的季节变化;涨潮前、涨落潮过程和落潮后甲烷通量大小并无一致的规律,平均排放通量分别为5.13、5.06和4.74 mg·m-2·h-1,差异不显著,其中涨落潮过程排放到潮水和大气环境的甲烷通量分别为2.98和2.08 mg·m-2·h-1.互花米草入侵斑块年均甲烷排放通量(11.02mg·m-2·h-1)明显高于芦苇湿地年均甲烷排放通量(4.98mg·m-2·h-1),互花米草入侵明显增加了闽江河口区湿地的甲烷排放通量.芦苇湿地0～40 cm土壤中甲烷产生潜力范围为0.029～0.123μg·g-1·d-1,0～5 cm土层的甲烷产生潜力最大,且与其它土层差异显著(P<0.05).气温、土壤温度和地上生物量对芦苇湿地甲烷排放影响显著(P<0.05),落潮后芦苇湿地甲烷排放通量与盐度有负相关关系.

Main factors influencing CH4 flux from a Phragmites australis wetland in the Min River estuary

Seasonal and diel variation of methane flux from a Phragmites australis wetland and a Spartina alterniflora invasive patch were measured using the enclosed chamber technique.Samples were taken in 2007 before flood,in flooding and ebbing,and after ebb.Potential rates of methane production from the soil layers were also measured using an incubation method.The results indicated that the Shanyutan Phragmites australis wetland,which is the biggest Phragmites australis wetland in the Min River estuary area,was a ...