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首页> 外文期刊>Roczniki Gleboznawcze >Nitrogen mineralization in forestry-drained peatland soils in the Sto?owe Mountains National Park (Central Sudetes Mts)
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Nitrogen mineralization in forestry-drained peatland soils in the Sto?owe Mountains National Park (Central Sudetes Mts)

机译:斯托沃夫山国家公园(Central Sudetes Mts)森林排水的泥炭地土壤中的氮矿化作用

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摘要

The aim of this work was to determine the intensity of nitrogen mineralization in forestry drained ombrotrophic peatland soils in the Sto?owe Mountains National Park, SW Poland. Additionally discussion about the shallow organic soils classification according to Polish Soil Classification (2011) is presented. For the study three research transects were established on forestry drained ombrotrophic peatlands in the Sto?owe Mountains. Each of the transect consisted of four (site A and B) or five (site C) sampling plots. Sampling was conducted in the year 2012. The soil samples for the basic soil properties analysis were sampled in April, whereas undisturbed soil samples were collected in stainless steel rings (100 cm3) every 10 cm in April (spring), July (summer) and October (autumn) to show the seasonal dynamics of nitrogen mineralization. Statistical analysis showed that the content of N-NH4 was mainly determined by actual soil moisture and precipitation rate, whereas the content of N-NO3 was positively correlated with air temperature. Among investigated peatlands the highest concentrations of mineral nitrogen forms was observed in the D?ugie Mokrad?o bog, situated on the Skalniak Plateau-summit. Additionally, the results obtained showed that implementation of new subtype: shallow fibric peat soils (in Polish: gleby torfowe fibrowe p?ytkie) within the type of peat soils (in polish: gleby torfowe) should be considered during developing of the next update of Polish Soil Classification.
机译:这项工作的目的是确定波兰西南部斯托沃夫山国家公园森林排水的非营养营养泥炭地土壤中氮的矿化强度。此外,还根据波兰土壤分类(2011年)对浅层有机土壤分类进行了讨论。为了进行这项研究,在斯托弗山的森林排水的非营养营养泥炭地上建立了三个研究样带。每个样带由四个(站点A和B)或五个(站点C)采样图组成。采样于2012年进行。用于基本土壤性质分析的土壤样品于4月进行了采样,而未扰动的土壤样品则于4月每10 cm被收集在不锈钢环(100 cm 3 )中(春季),七月(夏季)和十月(秋季)以显示氮矿化的季节动态。统计分析表明,N-NH 4 的含量主要取决于土壤的实际水分和降水量,而N-NO 3 的含量与气温呈正相关。 。在被调查的泥炭地中,在Skalniak高原峰顶的Dugugie Mokrad?o沼泽中观察到最高浓度的矿物质氮。此外,获得的结果表明在开发下一个更新版本的泥炭土壤类型(波兰语:gleby torfowe fibrowe p?ytkie)内应考虑实施新的亚型:浅纤维泥炭土(波兰语:gleby torfowe fibrowe p?ytkie)。波兰土壤分类。

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