首页> 外文会议>Annual Meetings of the American Society of Mining and Reclamation >MACRONUTRIENT ACCUMULATION AND RELATIONSHIPS IN A SCOTS PINE (PINUS SYLVESTRIS L.) ECOSYSTEM ON RECLAIMED OPENCAST LIGNITE MINE SPOIL HEAPS IN CENTRAL POLAND
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MACRONUTRIENT ACCUMULATION AND RELATIONSHIPS IN A SCOTS PINE (PINUS SYLVESTRIS L.) ECOSYSTEM ON RECLAIMED OPENCAST LIGNITE MINE SPOIL HEAPS IN CENTRAL POLAND

机译:在波兰中部再生Opencast Lignite矿的苏格兰州松(Pinus Sylvestris L.)生态系统中的Macronutrient累积和关系

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The aim of this study was to determine the sources, accumulation rate and relationships between macronutrients in reclaimed mine soils (RMS) and aboveground plant biomass on external slopes of lignite mines in central Poland. The study was conducted on two different types of sites with 10-year-old Scots (Pinus sylvestris L.) pine stands located on Quaternary loamy sands (QLS) and on Tertiary acidic carboniferous sands following neutralisation (TCS). The control plot was located in the same vicinity on an external slope in a natural pine ecosystem on a Haplic Podzol in a young mixed coniferous forest habitat (NPE). The nutrient resources, apart from N, were higher in RMS than in comparable Haplic Podzols, however, N primarily accumulated in the mineral horizons. In forest soils, the main macronutrient resources were accumulated in organic horizons, which in natural soils of coniferous forest habitats constitute the main source of nutrients. The proportion of individual macronutrients accumulated in the biomass vs. pools in soil was much lower on the external slope RMS than in the natural site, which in view of the potential richness of RMS, indicated poorer sorption and utilization of macronutrients in aboveground plant biomass than in natural habitats. Other important linear correlations (p=.05) were found between the sources of nutrients in RMS and elements accumulated in biomass (most clearly in case of K, Ca and Mg), which indicates important relationships between soil and vegetation in the first stages of ecosystem development as stimulated by reclamation.
机译:本研究的目的是确定波兰中部地区褐煤矿外部斜坡外部矿山土壤(RMS)和地下植物生物量的克斯营养素之间的来源,积累率和关系。该研究是在两种不同类型的网站上进行,其中10岁的苏格兰人(Pinus Sylvestris L.)松树架,位于季硝基砂砂(QLS)和中和(TCS)后的叔酸性石炭料砂上。对照图位于幼苗林栖植物(NPE)的天然杉木生态系统中的外侧坡度在相同的附近。营养资源除了N的营养资源高于RMS,而不是相当的单级豆荚,然而,N主要积累在矿物视野中。在森林土壤中,主要的Macronurient资源积累在有机视野中,其在针叶林栖息地的天然土壤中构成了营养素的主要来源。在土壤中累积的单个常态营养素的比例在土壤中的池中比在天然遗址中较低得多,这鉴于RMS的潜在丰富性,表明在地上植物生物质中的巨额营养素的吸附和利用率较差在自然栖息地。在生物质中累积的rms和元素的营养素源和元素之间发现了其他重要的线性相关(p = .05)(在K,Ca和mg的情况下最明确),这表明了在第一阶段中的土壤和植被之间的重要关系生态系统开发被垦殖刺激。

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