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首页> 外文期刊>The Science of the Total Environment >Moss and lichen biomonitoring of atmospheric mercury: A review
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Moss and lichen biomonitoring of atmospheric mercury: A review

机译:大气汞的苔藓和地衣生物监测:综述

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Long-range transport and residence time of elemental Hg (Hg°) in air promote global dispersion and deposition in remote ecosystems. Many biotic and abiotic factors contribute to the photoreduction and phytovolatilization of Hg from terrestrial ecosystems, and the assessment of deposition and volatilization fluxes is very challenging. Mosses and lichens are widespread in nature and constitute the dominant vegetation in alpine and polar ecosystems. This review surveys the results of Hg biomonitoring with cryptogams in areas with different Hg sources and deposition processes. Lichen and moss ecophysiology, and factors affecting Hg uptake and bioaccumulation are discussed. Although some laboratory experiments indicate a linear accumulation of Hg in cryptogams exposed to Hg°, without any significant release, in nature the Hg accumulated in cryptogams is in a dynamic equilibrium with Hg in air and decreases when organisms are transplanted to clean environments. Mercury concentrations in mosses and lichens have often been used to estimate concentrations and deposition fluxes of atmospheric Hg; however, Hg° exchanges between cryptogams and air, and the time necessary for mosses and lichens to equilibrate elemental composition with changing atmospheric chemistry, preclude reliable estimates. Biological processes of Hg uptake and exchange with air cannot be reproduced by mechanical collectors, and comparisons between Hg concentrations in biomonitors and those in atmospheric deposition are scarcely reliable. However, the Hg biomonitoring with mosses and lichens is easy and cheap and allows to locate "hot spots" of natural or anthropogenic emissions and to assess spatio-temporal changes in Hg deposition patterns. Climate change is affecting the global Hg cycle through the melting of sea-ice in coastal Polar Regions, and modifying Hg sequestration in mountain ecosystems. Despite limitations, large-scale monitoring of Hg with mosses and lichens may be used as a tool to evaluate the impact of global processes in remote ecosystems.
机译:空气中Hg(Hg°)的长距离传输和停留时间促进了偏远生态系统的全球扩散和沉积。许多生物和非生物因素都有助于陆地生态系统中汞的光还原和植物挥发,因此对沉积和挥发通量的评估非常具有挑战性。苔藓和地衣在自然界很普遍,是高山和极地生态系统中的主要植被。这篇综述调查了在汞源和沉积工艺不同的地区用隐球菌对汞进行生物监测的结果。讨论了地衣和苔藓的生态生理学以及影响汞吸收和生物积累的因素。尽管一些实验室实验表明,暴露于Hg°的隐秘汞中的Hg呈线性累积,而没有任何显着释放,但实际上,隐秘汞中的Hg与空气中的Hg处于动态平衡,当将生物移植到干净的环境中时会降低。苔藓和地衣中的汞浓度经常被用来估算大气中汞的浓度和沉积通量。然而,隐藻与空气之间的汞交换以及苔藓和地衣通过不断变化的大气化学平衡元素组成所需的时间,排除了可靠的估计。机械收集器无法重现汞吸收和与空气交换的生物过程,而且生物监测器中的汞浓度与大气沉积中的汞浓度之间的比较几乎是不可靠的。但是,用苔藓和地衣对汞进行生物监测既简单又便宜,并且可以定位自然或人为排放物的“热点”,并评估汞沉积模式的时空变化。气候变化通过沿海极地地区的海冰融化,并改变了山区生态系统中的汞固存,影响了全球汞循环。尽管存在局限性,但使用苔藓和地衣对汞进行大规模监测仍可以用作评估全球过程对边远生态系统影响的工具。

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