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Temporal variations in methane emissions from emergent aquatic macrophytes in two boreonemoral lakes

机译:两个硼砂湖中新兴水生植物甲烷排放的时间变化

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摘要

Methane (CH4) emissions via emergent aquatic macrophytes can contribute substantially to the global CH4 balance. We addressed temporal variability in CH4 flux by using the static chamber approach to quantify fluxes from plots dominated by two species considered to differ in flux transport mechanisms (Phragmites australis, Carex rostrata). Temporal variability in daily mean emissions from early June to early October was substantial. The variable that best explained this variation was air temperature. Regular and consistent diel changes were absent and therefore less relevant to include when estimating or modelling CH4 emissions. Methane emissions per m2 from nearby plots were similar for Phragmites australis and Carex rostrata indicating that CH4 production in the system influenced emissions more than the species identity. This study indicates that previously observed diel patterns and species-effects on emissions require further evaluation to support improved local and regional CH4 flux assessments.
机译:新兴水生植物排放的甲烷(CH4)可能对全球CH4平衡产生重大影响。我们通过使用静态腔室方法来量化CH2通量的时间变异性,该方法采用静态腔室方法来量化由两种物质(主要分布于芦苇,Carex rostrata)不同的两种物种主导的地块的通量。 6月初至10月初的日平均排放量随时间变化很大。最好的解释这种变化的变量是气温。由于没有规律和一致的迪尔变化,因此在估算或模拟CH4排放时不宜包括在内。芦苇和非洲苔藓的每m 2 附近地块的甲烷排放量相似,表明系统中CH4的产生对排放的影响大于物种识别。这项研究表明,以前观察到的diel模式和对排放的物种影响需要进一步评估,以支持改进的本地和区域CH4通量评估。

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