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Background levels of some major, trace, and rare earth elements in indigenous plant species growing in Norway and the influence of soil acidification, soil parent material, and seasonal variation on these levels

机译:挪威本土植物物种中某些主要,微量和稀土元素的背景水平以及土壤酸化,土壤母体材料和季节变化对这些水平的影响

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摘要

Baseline levels of 43 elements, including major, trace, and rare earth elements (REEs) in several native plant species growing in boreal and alpine areas, are presented. Focus is placed on species metal levels at different soil conditions, temporal variations in plant tissue metal concentrations, and interspecies variation in metal concentrations. Vegetation samples were collected at Sogndal, a pristine site in western Norway, and at Risdalsheia, an acidified site in southernmost Norway. Metal concentrations in the different species sampled in western Norway are compared with relevant literature data from Norway, Finland, and northwest Russia, assumed to represent natural conditions. Except for aluminium (Al) and macronutrients, the levels of metals were generally lower in western Norway than in southern Norway and may be considered close to natural background levels. In southern Norway, the levels of cadmium (Cd) and lead (Pb) in particular appear to be affected by air pollution, either by direct atmospheric supply or through soil acidification. Levels of some elements show considerable variability between as well as within plant species. Calcium (Ca), magnesium (Mg), and potassium (K) are higher in most species at Sogndal compared to Risdalsheia, despite increased extractable concentrations in surface soil in the south, probably attributed to different buffer mechanisms in surface soil. Antagonism on plant uptake is suggested between Ca, Mg, and K on one hand and Al on the other. Tolerance among calcifuges to acid conditions and a particular ability to detoxify or avoid uptake of Al ions are noticeable for Vaccinium vitis-idaea.
机译:介绍了在北高寒地区生长的几种原生植物物种中43种元素的基线水平,包括主要,痕量和稀土元素(REE)。重点放在不同土壤条件下的物种金属水平,植物组织金属浓度的时间变化以及金属浓度的种间变化。在挪威西部的原始地Sogndal和挪威最南端的酸化地Risdalsheia收集了植被样品。将挪威西部采样的不同物种中的金属浓度与挪威,芬兰和俄罗斯西北部的相关文献数据进行了比较,假定这些数据代表自然条件。除铝和大量营养素外,挪威西部的金属含量通常低于挪威南部,并被认为接近自然本底水平。在挪威南部,特别是镉的含量和铅(Pb)的含量似乎受到大气污染的影响,无论是直接大气供应还是通过土壤酸化。一些元素的水平显示出植物之间以及植物内部之间的巨大差异。尽管在南部表层土壤中可提取物的浓度增加,但Sogndal大部分物种中的钙(Ca),镁(Mg)和钾(K)高于Risdalsheia,这可能是由于表层土壤的缓冲机制不同所致。建议一方面在Ca,Mg和K之间,另一方面在Al之间对植物的吸收产生拮抗作用。葡萄球菌对酸条件的耐受性以及特定的解毒或避免摄入铝离子的能力很明显。

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