首页> 外文期刊>The Science of the Total Environment >A geochemical perspective on the natural abundance and predominant sources of trace elements in cranberries (Vaccinium oxycoccus) from remote bogs in the Boreal region of northern Alberta, Canada
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A geochemical perspective on the natural abundance and predominant sources of trace elements in cranberries (Vaccinium oxycoccus) from remote bogs in the Boreal region of northern Alberta, Canada

机译:地球化学观点,来自加拿大艾伯塔省北部的北方沼泽地的蔓越莓(越橘越桔)中微量元素的天然丰富度和主要来源

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Trace elements in native cranberry (Vaccinium oxycoccus) were compared with the underlying Sphagnum moss on which it grows, from two remote ombrotrophic (rain-fed) peat bogs in northern Alberta, Canada. The purpose of the comparison was to distinguish between dust inputs to the berries versus plant uptake from the substrate, and to determine the natural abundance of trace elements in native berries. Using Al as an indicator of the abundance of soil-derivedmineral particles, the abundance of dust on the surface of the berries is 20 to 29x lower than that of the substrate (moss). Other lithophile elements (V, Cr, Co, Ga, Li and Y) show similar differences between moss and berry. The concentrations of Rb and Ba in berries were similar tomoss and Sr within a factor of 3 to 4x, probably reflecting passive uptake of these lithophile elements by the plants, even though they have no known physiological function. Of themicronutrients examined (Mn, Fe, Ni, Cu, Zn andMo), Cu and Mnwere more abundant in berries than moss, Ni and Zn yielded similar concentrations in both whereas Fe followed by Mo showed the greatest concentration difference. For these micronutrients, uptake by the plants through their roots via the substrate (moss and peat) outweighs contributions from atmospheric dusts.In respect to potentially toxic "heavymetals", Pb concentrations in the moss (BMW, 89 +/- 7.3 mu g/kg; CMW, 93 +/- 27 mu g/kg) are below the natural, "background" values reported for ancient layers of Swiss peat from the mid-Holocene (6000 years old). The Pb concentrations in the berries, however, are 19 to 47x lower than in the underlying moss indicating that Pb in the berries, like Al, is exclusively supplied by dust. Cadmiumin the berries is at or above the level found in moss due to active uptake by the plants from the substrate, most likely because of the chemical similarity of this element to Zn. Silver, Sb and Tl in the berries were bLOD, but assuming that they are supplied exclusively by dust inputs, their concentrations in the berries can be estimated from the Al concentrations. Taken together, these data provide an estimate of the natural abundance of these elements in berries, based on measured (Cd, Pb) and calculated (Ag, Sb, Tl) values. (C) 2018 Published by Elsevier B.V.
机译:从加拿大阿尔伯塔省北部的两个偏僻的营养营养(雨养)泥炭沼泽中,比较了天然蔓越莓(葡萄球菌)中的痕量元素与潜在的蔓生的泥炭藓。比较的目的是区分输入到浆果的粉尘与从底物吸收的植物,并确定天然浆果中微量元素的自然丰度。用铝作为土壤来源的矿物颗粒含量的指标,浆果表面的粉尘含量比基质(苔藓)的含量低20至29倍。其他嗜石元素(V,Cr,Co,Ga,Li和Y)在苔藓和浆果之间显示出相似的差异。浆果中Rb和Ba的浓度在3到4倍之间类似于托莫斯和Sr,即使它们没有已知的生理功能,也可能反映了植物对这些亲石元素的被动吸收。在所检测的微量营养元素(锰,铁,镍,铜,锌和钼)中,浆果中的铜和锰比苔藓中的丰富,镍和锌的含量均相似,而铁,钼和钼的浓度差异最大。对于这些微量营养素,植物通过根部通过基质(苔藓和泥炭)对植物的吸收超过了大气尘埃的贡献。就潜在有毒的“重金属”而言,苔藓中的Pb浓度(BMW,89 +/- 7.3亩)克/千克; CMW,93 +/- 27微克/千克)低于全新世中期(> 6000年以前)瑞士泥炭古层的自然“背景”值。但是,浆果中的Pb浓度比下面的苔藓低19至47倍,这表明浆果中的Pb(如Al)仅由灰尘提供。浆果中的镉水平等于或高于苔藓中的水平,这是由于植物从底物中主动摄取,最有可能是由于该元素与锌的化学相似性。浆果中的银,Sb和Tl为bLOD,但假设它们仅由粉尘输入提供,则可以根据Al的浓度估算它们在浆果中的浓度。综上所述,这些数据基于测量的(Cd,Pb)和计算的(Ag,Sb,Tl)值,提供了浆果中这些元素自然丰度的估计值。 (C)2018由Elsevier B.V.发布

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