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Major implication of the littoral zone for methane release from boreal lakes

机译:滨海带对北方湖泊甲烷排放的主要影响

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摘要

[1] Transitions between aquatic and terrestrial environments can be recognized as biogeochemically active ecotones that support high CH4 release. We studied the links between littoral CH4 fluxes and aquatic vegetation, hydrologic conditions, and sediment quality, and integrated the CH4 fluxes into a whole-lake assessment. Methane fluxes were measured using a closed chamber method in the littoral and pelagic zones of three Finnish mid-boreal lakes from May to October. The cumulative CH_4 fluxes were spatially integrated over the lake relative to the vegetation coverage in the littoral, and to depth zones in the pelagic regions. During the ice-free period, 66–77% of the CH_4 was released from the littoral zone, and the mean CH_4 effluxes from these lakes were 0.08–0.42 mol m~(-2) ice-free season~(-1). Littoral and pelagic productivity was reflected in CH_4 release from the lakes. Our results show that estimates of lake CH_4 release should include an assessment of the vegetated littoral zone.
机译:[1]水生和陆地环境之间的过渡可以被认为是支持高CH4释放的生物地球化学活性过渡带。我们研究了沿海CH4通量与水生植被,水文条件和沉积物质量之间的联系,并将CH4通量纳入了整个湖泊评估。从5月至10月,在三个芬兰中北部湖泊的沿海和中上层带,采用密闭室法测量了甲烷通量。相对于沿岸的植被覆盖度以及中上层地区的深层区域,湖泊中累积的CH_4通量在空间上被积分。在无冰期,CH_4的66–77%从沿海地带释放,这些湖泊的平均CH_4流出量为0.08–0.42 mol m〜(-2)无冰季节〜(-1)。沿湖和中上层生产力反映在湖泊中的CH_4释放中。我们的结果表明,对CH_4湖泊释放的估算应包括对沿岸植被带的评估。

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