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Dynamic Surface Interface Exchanges of Mercury: A Review and Compartmentalized Modeling Framework

机译:汞的动态表面接口交换:一个综述和分隔的建模框架

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This paper presents a review of recent natural surface mercury exchange research in the context of a new modeling framework. The literature indicates that the mercury biogeochemical flux is more dynamic than the current models predict, with interacting multimedia storage and processes. Although several natural mercury emissions models have been created and incorporated into air quality models (AQMs), none are coupled with air quality models on a mass balance basis, and all lack the capacity to explain processes that involve the transport of mercury across atmosphere-surface media concentration gradients. Existing natural mercury emission models treat the surface as both an infinite source and infinite sink for emissions and deposition, respectively,and estimate emissions through the following three pathways: soil, vegetation, and surface waters. The use of these three transport pathways, but with compartmentalized surface storage in a surface-vegetation-atmosphere transport (SVAT) resistance model, is suggested. Surface water fluxes will be modeled using a two-film diffusion model coupled to a surface water photochemical model. This updated framework will allow both the parameterization of the transport of mercury across atmosphere-surface mediaconcentration gradients and the accumulation/depletion of mercury in the surface media. However, several key parameters need further experimental verification before the proposed modeling framework can be implemented in an AQM. These include soil organic mercury interactions, bioavailabil-ity, cuticular transport of mercury, atmospheric surface compensation points for different vegetation species, and enhanced soil diffusion resulting from pressure perturbations.
机译:本文在一个新的建模框架的背景下,对最近的自然表面汞交换研究进行了综述。文献表明,汞的生物地球化学通量比当前模型预测的更具动态性,并且具有相互作用的多媒体存储和过程。尽管已经创建了几种自然汞排放模型并将其纳入空气质量模型(AQM),但是没有一个模型与质量平衡基础上的空气质量模型相结合,并且都缺乏解释涉及汞在整个大气表面传输的过程的能力。介质浓度梯度。现有的自然汞排放模型分别将表面视为排放和沉积的无限来源和无限汇,并通过以下三种途径估算排放:土壤,植被和地表水。建议使用这三种传输路径,但在表面-植被-大气传输(SVAT)阻力模型中使用分区的表面存储。将使用与地表光化学模型耦合的两层扩散模型对地表水通量进行建模。这个更新的框架将既可以实现跨大气表面介质浓度梯度的汞传输参数化,也可以实现表面介质中汞的累积/耗竭。但是,在可以在AQM中实现所提出的建模框架之前,几个关键参数需要进一步的实验验证。这些因素包括土壤有机汞的相互作用,生物利用度,汞的表皮运输,不同植被的大气表面补偿点以及由于压力扰动而导致的土壤扩散增强。

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