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Current state of peatland soils as an effect of long-term drainage – preliminary results of peatland ecosystems investigation in the Grójecka Valley (central Poland)

机译:长期排水对泥炭地土壤现状的影响–Grójecka谷地(波兰中部)泥炭地生态系统调查的初步结果

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Understanding the effect of long-term drainage of peatland areas is helpful in future peatland management and regulations of water conditions. The aim of this work was to assess the current state of fen peatland soils in the Grójecka Valley (eastern part of the Wielkopolskie voivodeship, central Poland), affected by long-term agricultural use (pastures, meadows) since the 1960s and potentially by lignite open pit mining industry (KWB Konin) since 1980s. Field studies were carried out in 2015 in selected fen peatland areas. Soil material for laboratory analysis was collected from genetic horizons from four soil profiles. The surface horizons of studied organic and organo-mineral soils were built with well-developed moorsh material. They were classified as medium moorshiefied – MtII (profile 1, 3 and 4) and strongly moorshiefied – MtIII (profile 2). Obtained results of physical and physico-chemical analysis indicate that long-term peatland utilization connected with potential impact of the lignite mining, transformed mainly the upper horizons of studied organic and organo-mineral soils. However, despite obvious strong human impact on peatlands ecosystems, we cannot exclude the climate variables, what should be confirmed by long-term monitoring program. Furthermore, presented paper indicated that new subtype moorsh-muddy soils (in Polish: gleby murszowo-mu?owe) within the type of gleyic soils should be implemented in the next version of Polish Soil Classification.
机译:了解泥炭地长期排水的效果有助于将来泥炭地的管理和水质法规的制定。这项工作的目的是评估自1960年代以来长期受农业(牧草,草地)使用以及褐煤潜在影响的Grójecka谷(波兰中部Wielkopolskie省的东部)的fen泥炭地土壤的现状。自1980年代以来就是露天采矿业(KWB Konin)。 2015年在部分芬泥炭地地区进行了实地研究。从四个土壤剖面的遗传视野中收集了用于实验室分析的土壤材料。研究的有机土壤和有机矿物土壤的地表层是由发育良好的沼泽材料制成的。它们分为中级Motshiefied – MtII(轮廓1、3和4)和强级Moorshiefied – MtIII(轮廓2)。物理和物理化学分析的结果表明,长期利用泥炭地与褐煤开采的潜在影响有关,主要改变了所研究的有机土壤和有机矿物土壤的上层视野。然而,尽管人类对泥炭地生态系统产生了明显的强烈影响,但我们不能排除气候变量,应通过长期监测计划予以确认。此外,提出的论文指出,在下一个版本的波兰土壤分类中,应使用新的亚种的泥质土壤类型(波兰语:gleby murszowo-muowowe)。

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