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首页> 外文期刊>Mires and Peat >Undrained peatland areas disturbed by surrounding drainage: a large scale GIS analysis in Finland with a special focus on aapa mires
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Undrained peatland areas disturbed by surrounding drainage: a large scale GIS analysis in Finland with a special focus on aapa mires

机译:未排水的泥炭地地区受到周围排水系统的干扰:芬兰的大规模GIS分析,特别关注aapa泥潭

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摘要

Half of the Finnish peatland area is drained for forestry. The remaining undrained peatlands are not all pristine, because surrounding drainage may disturb their hydrology. This concerns especially aapa mires, which are dependent on hydrological connections to their upper catchments. We investigated the amount and sizes of Finnish undrained peatlands, the drainage state of their margins, and the naturalness of aapa mires in large ( 50 ha) undrained peatland areas, using a GIS analysis based on digital map data, aerial images and an elevation model. The results show that a majority (66.7 % of count, 84.7 % of area) of undrained peatland areas have at least partly drained margins. Drainage activities commonly disturb minerotrophic water discharge to aapa mires. In the middle boreal zone, on average 41.6 % (median 42.8 %) of the catchment area of aapa mires is such that hydrological connection with the mire is disturbed by intervening drainage. In the southern boreal zone, the figure is 25.1 % (median 16.1 %), and in the southern part of the northern boreal zone 24.2 % (median 9.9 %). Possible implications of the disturbances include tree encroachment, hummock formation and fen–bog transition, which is likely to cause a loss of biodiversity but could potentially increase peat growth and carbon sequestration.
机译:芬兰泥炭地面积的一半被排干用于林业。剩下的不排水的泥炭地并不是全部原始的,因为周围的排水系统可能会扰乱其水文状况。这尤其涉及aapa mire,后者取决于与上游流域的水文联系。我们使用了基于数字地图数据,航空影像和高程的GIS分析,调查了芬兰不排水的泥炭地的数量和大小,其边缘的排水状态以及大面积(> 50公顷)泥炭地的aapa泥潭的自然状态模型。结果表明,大部分不排水的泥炭地面积(占总数的66.7%,面积的84.7%)至少有一部分被排水。排水活动通常会干扰矿养水向aapa mire的排放。在中北部寒带地区,平均aapa泥潭集水面积的41.6%(中位数为42.8%)是这样的,以至于泥潭的水文联系受到中间排水的干扰。在南部寒带区,这一数字为25.1%(中位数为16.1%),在北部寒带区的南部为24.2%(中位数为9.9%)。干扰的潜在影响包括树木侵占,山岗形成和沼泽过渡,这可能会导致生物多样性的丧失,但可能会增加泥炭的生长和碳固存。

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