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作 者:王宗林[1] 吴沿友[1,2] 邢德科[1] 刘荣成[1] 周贵尧[1] 赵宽[1]
机构地区:[1]现代农业装备与技术省部共建教育部重点实验室/江苏省重点实验室/江苏大学农业工程研究院,江苏镇江212013 [2]中国科学院地球化学研究所环境地球化学国家重点实验室,贵阳550002
出 处:《应用生态学报》2014年第9期2563-2568,共6页Chinese Journal of Applied Ecology
基 金:"十二五"国家科技支撑计划项目(2009BADB2B04-03)资助
摘 要:福建泉州湾红树林湿地生态系统所处地属正规半日潮,为新近栽植的人工修复林带.采用Li-840便携式土壤二氧化碳分析仪测定主要红树群落土壤CO2排放通量,研究土壤CO2通量周期性变化特征.结果表明: 泉州湾红树林处于幼林期,其土壤CO2通量较小;早、晚潮潮间期,秋茄和桐花树群落土壤CO2浓度和通量随退潮时间变化趋势基本一致;泉州湾红树林湿地土壤CO2浓度和通量分别为557.08-2211.50 μmol·mol-1和-0.21-0.40μmol·m-2·s-1,早、晚潮潮间期和晚、早潮潮间期CO2通量平均值分别为0.26和-0.01μmol·m-2·s-1;对于同一退潮时刻,早、晚潮潮间期CO2通量大于晚、早潮潮间期.早、晚潮潮间期CO2通量与对应的即时CO2浓度呈“钟”型变化,CO2通量随CO2浓度的增加呈先增加后降低的趋势,近似高斯分布,据此可建立该系统土壤CO2通量与CO2即时浓度的数学模型.Mangrove wetland ecosystem in Quanzhou Bay in Fujian Province is newly restored with a regular semidiurnal tide. Soil CO2 concentration in the mangrove soil was determined by Li-840 portable gas analyzer, and periodic characteristics of soil CO2 emission was investigated. The soil CO2 flux in the wetland soil was relatively small because the mangrove was young. The change trends of soil CO2 concentration and flux with time were consistentin Kandelia obovate and Aegiceras corniculatum communities in the intertidal periods. The CO2 concentration and flux in the wetland soil were 557.08-2211.50 μmol·mol-1 and -0.21-0.40 μmol·m-2·s-1, respectively. The average CO2 flux in the wetland soil was 0.26 μmol·mol-1·s-1 in the intertidal of morning and evening tides (early intertidal) and -0.01 μmol·m-2·s-1 in the intertidal of evening and morning tides (late intertidal), respectively. At the same time after the tide, the concentration and flux of CO2in the mangrove soil in early intertidal was higher than that in late intertidal. In early intertidal, the relationship between the flux and instantaneous concentration of CO2 in the wetland soil was expressed as a bellshaped curve, and CO2flux increased first and then decreased with the increa sing CO2 concentration, which was in conformity with Gaussian distribution.
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