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Linking forest fires to lake metabolism and carbon dioxide emissions in the boreal region of Northern Qucbbec

机译:将森林大火与魁北克北部寒带的湖泊新陈代谢和二氧化碳排放联系起来

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摘要

Natural fires annually decimate up to 1% of the forested area in the boreal region of Qucbbec, and represent a major structuring force in the region, creating a mosaic of watersheds characterized by large variations in vegetation structure and composition. Here, we investigate the possible connections between this fire-induced watershed heterogeneity and lake metabolism and CO dynamics. Plankton respiration, and water-air CO fluxes were measured in the epilimnia of 50 lakes, selected to lie within distinct watershed types in terms of postfire terrestrial succession in the boreal region of Northern Qucbbec. Plankton respiration varied widely among lakes (from 21 to 211 og C Lp# dayp#), was negatively related to lake area, and positively related to dissolved organic carbon (DOC). All lakes were supersaturated in CO and the resulting carbon (C) flux to the atmosphere (150 to over 3000 mg C mpo dayp#) was negatively related to lake area and positively to DOC concentration. CO fluxes were positively related to integrated water column respiration, suggesting a biological component in this flux. Both respiration and CO fluxes were strongly negatively related to years after the last fire in the basin, such that lakes in recently burnt basins had significantly higher C emissions, even after the influence of lake size was removed. No significant differences were found in nutrients, chlorophyll, and DOC between lakes in different basin types, suggesting that the fire-induced watershed features influence other, more subtle aspects, such as the quality of the organic C reaching lakes. The fire-induced enhancement of lake organic C mineralization and C emissions represents a long-term impact that increases the overall C loss from the landscape as the result of fire, but which has never been included in current regional C budgets and future projections. The need to account for this additional fire-induced C loss becomes critical in the face of predictions of increasing incidence of fire in the circumboreal landscape.
机译:每年自然火灾最多会破坏Qucbbec北部地区森林面积的1%,并代表了该地区的主要结构力量,形成了以植被结构和组成变化较大为特征的流域马赛克。在这里,我们研究了这种火灾引发的流域异质性与湖泊新陈代谢和CO动态之间的可能联系。在50个湖泊的上溢流中测量了浮游生物的呼吸作用以及水-空气中的CO通量,这些湖泊被选为北部库克贝奇北部地区的火后陆生演替,位于不同的分水岭类型内。湖泊之间的浮游生物呼吸变化很大(从21到211 og C Lp#dayp#),与湖泊面积呈负相关,与溶解有机碳(DOC)呈正相关。所有湖泊的CO含量都过饱和,所产生的通向大气的碳(C)通量(150至3000 mg C mpo dayp#)与湖泊面积呈负相关,与DOC浓度呈正相关。 CO通量与水柱综合呼吸呈正相关,表明该通量中存在生物成分。流域最后一次大火之后的数年,呼吸和CO通量都与负相关,因此,即使消除了湖泊规模的影响,最近被烧过的盆地中的湖泊的碳排放量也明显较高。在不同流域类型的湖泊之间,养分,叶绿素和DOC均未发现显着差异,这表明火源流域特征影响其他更微妙的方面,例如到达湖泊的有机碳的质量。火灾引起的湖泊有机碳矿化和碳排放的增加代表了一种长期影响,由于火灾而增加了景观中的总体碳损失,但从未包括在当前的区域碳预算和未来预测中。在周围环境中发生火灾的可能性不断增加的预测中,解决这种由火灾引起的额外C损失的需求变得至关重要。

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