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Nitrogen and phosphorus concentrations in discharge from drained peatland forests are increasing

机译:排干的泥炭地森林排放的氮和磷浓度正在增加

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摘要

The current understanding, based on previous studies, is that increased discharge nutrient concentrations from boreal peatlands drained for forestry return to similar levels as those of pristine peatlands within about 20 years after their drainage. As an implicit consequence of this finding, it has been assumed that there are no long-term increasing trends in nutrient exports from these peatlands after the establishment of forestry. We analysed discharge total nitrogen (TN) and phosphorus (TP) concentration data from 54 catchments with un-drained pristine peatlands and 34 catchments with drained peatlands using data with considerably longer drainage history than in previous studies. Our results agree with previous studies in that discharge TN and TP concentrations in areas drained 20-30 years ago did not differ much from those in pristine sites. However, we also observed that the TN and TP concentrations were increasing with years since drainage of these catchments. Discharge TN and TP concentrations were over two times higher in areas drained 60 years ago when compared with more recently drained areas. Our results challenge the current perceptions by showing that forestry-drained peatlands may contribute to water eutrophication considerably more than previously estimated.
机译:根据先前的研究,目前的理解是,在被排放后的大约20年内,为林业排放的北方泥炭地的排放养分浓度增加了与原始泥炭地相似的水平。作为这一发现的隐含结果,已经假定在建立林业之后,这些泥炭地的养分出口没有长期增长的趋势。我们使用比以前的研究具有更长的排水历史的数据分析了54个未排水的原始泥炭地集水区和34个排水的泥炭地集水区的排放总氮(TN)和磷(TP)浓度数据。我们的结果与以前的研究一致,即在20到30年前排水的地区,其总氮和总磷的浓度与原始地点的差异不大。但是,我们还观察到,自这些集水区排水以来,TN和TP的浓度随年增加。与最近排放的地区相比,60年前排放的地区的排放总氮和总磷浓度高出两倍以上。我们的结果通过证明森林排水的泥炭地对水体富营养化的贡献可能比以前的估计大得多,从而挑战了当前的看法。

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