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Post-fire ecohydrological conditions at peatland margins in different hydrogeological settings of the Boreal Plain

机译:泥土边缘在北方平原不同水文地质环境中的消防后生态水文条件

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In the Boreal Plain of Canada, the margins of peatland ecosystems that regulate solute and nutrient fluxes between peatlands and adjacent mineral uplands are prone to deep peat burning. Whether post-fire carbon accumulation is able to offset large carbon losses associated with the deep burning at peatland margins is unknown. For this reason, we examined how post-fire hydrological conditions (i.e. water table depth and periodicity, soil tension, and surface moisture content) and depth of burn were associated with moss recolonization at the peatland margins of three sites. We then interpreted these findings using a hydrogeological systems approach, given the importance of groundwater in determining conditions in the soil-plant-atmosphere continuum in peatlands. Peatland margins dominated by local groundwater flow from adjacent peatland middles were characterized by dynamic hydrological conditions that, when coupled with lowered peatland margin surface elevations due to deep burning, produced two common hydrological states: 1) flooding during wet periods and 2) rapid water table declines during dry periods. These dynamic hydrological states were unfavorable to peatland moss recolonization and bryophytes typical of post-fire recovery in mineral uplands became established. In contrast, at a peatland margin where post-fire hydrological conditions were moderated by larger-scale groundwater flow, flooding and rapid water table declines were infrequent and, subsequently, greater peatland-dwelling moss recolonization was observed. We argue that peatland margins poorly connected to larger-scale groundwater flow are not only prone to deep burning but also lags in post-fire moss recovery. Consequently, an associated reduction in post-fire peat accumulation may occur and negatively affect the net carbon sink status and ecohydrological and biogeochemical function of these peatlands. (C) 2017 Elsevier B.V. All rights reserved.
机译:在加拿大的北方平原中,泥炭地生态系统的边缘调节泥炭地和邻近矿物高地之间的溶质和营养助核易患深处泥炭燃烧。火灾后碳积累是否能够抵消与泥炭地边距的深度燃烧相关的大碳损失是未知的。因此,我们研究了消防后的水文条件(即水表深度和周期性,土壤张力和表面水分含量)和烧伤深度与三个地点的泥炭地边缘的苔藓重组有关。然后,鉴于地下水在泥炭地在泥炭地的土壤 - 植物气氛中的条件下,使用水文地理系统方法将这些发现解释了这些发现。泥炭地利润以邻近的泥炭地覆盖泥土流域主导的泥炭地利润是动态水文条件的特点是,当由于深燃烧而导致的泥炭地边缘表面升高时,产生两种常见水文状态:1)潮湿时期的洪水和2)快速水桌干燥时期下降。这些动态水文州不利于泥炭覆代苔藓重组,典型的矿产后矿物质后的苔藓植物成立。相比之下,在泥炭缘边缘,通过较大尺寸的地下水流动调节消失后水文条件,洪水和快速的水位表现出不常见,随后观察到更大的泥炭地 - 住宅的苔藓重新调整。我们认为,与大规模地下水流量相连的泥炭地利润率不仅容易发生深深的燃烧,而且在火灾后青苔恢复中也滞后。因此,可能发生爆炸后泥炭堆积的相关减少,并对这些泥炭块的净碳汇状态和生态文化和生物地球化学功能产生负面影响。 (c)2017年Elsevier B.V.保留所有权利。

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