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背景土壤汞排放建模。

Modelling of mercury emissions from background soils.

作者信息

Scholtz M T, Van Heyst B J, Schroeder W H

机构信息

Canadian ORTECH Environmental Inc., 2395 Speakman Drive, Mississauga, Ont., Canada L5K 1B3.

出版信息

Sci Total Environ. 2003 Mar 20;304(1-3):185-207. doi: 10.1016/S0048-9697(02)00568-5.

Abstract

Emissions of volatile mercury species from natural soils are believed to be a significant contributor to the atmospheric burden of mercury, but only order-of-magnitude estimates of emissions from these sources are available. The scaling-up of mercury flux measurements to regional or global scales is confounded by a limited understanding of the physical, chemical and biochemical processes that occur in the soil, a complex environmental matrix. This study is a first step toward the development of an air-surface exchange model for mercury (known as the mercury emission model (MEM)). The objective of the study is to model the partitioning and movement of inorganic Hg(II) and Hg(0) in open field soils, and to use MEM to interpret published data on mercury emissions to the atmosphere. MEM is a multi-layered, dynamic finite-element soil and atmospheric surface-layer model that simulates the exchange of heat, moisture and mercury between soils and the atmosphere. The model includes a simple formulation of the reduction of inorganic Hg(II) to Hg(0). Good agreement was found between the meteorological dependence of observed mercury emission fluxes, and hourly modelled fluxes, and it is concluded that MEM is able to simulate well the soil and atmospheric processes influencing the emission of Hg(0) to the atmosphere. The heretofore unexplained close correlation between soil temperature and mercury emission flux is fully modelled by MEM and is attributed to the temperature dependence of the Hg(0) Henry's Law coefficient and the control of the volumetric soil-air fraction on the diffusion of Hg(0) near the surface. The observed correlation between solar radiation intensity and mercury flux, appears in part to be due to the surface-energy balance between radiation, and sensible and latent heat fluxes which determines the soil temperature. The modelled results imply that empirical correlations that are based only on flux chamber data, may not extend to the open atmosphere for all weather scenarios.

摘要

自然土壤中挥发性汞物种的排放被认为是大气汞负担的一个重要来源,但目前仅能获得这些来源排放的量级估算。由于对土壤(一种复杂的环境基质)中发生的物理、化学和生物化学过程了解有限,将汞通量测量结果扩大到区域或全球尺度时会受到干扰。本研究是朝着开发汞的气 - 面交换模型(称为汞排放模型(MEM))迈出的第一步。该研究的目的是模拟无机汞(II)和汞(0)在露天土壤中的分配和移动,并使用MEM来解释已发表的向大气排放汞的数据。MEM是一个多层动态有限元土壤和大气表层模型,用于模拟土壤与大气之间的热量、水分和汞的交换。该模型包含一个将无机汞(II)还原为汞(0)的简单公式。观测到的汞排放通量与每小时模拟通量的气象依赖性之间发现了良好的一致性,得出的结论是MEM能够很好地模拟影响汞(0)向大气排放的土壤和大气过程。土壤温度与汞排放通量之间迄今无法解释的紧密相关性已被MEM完全模拟出来,这归因于汞(0)亨利定律系数对温度的依赖性以及土壤 - 空气体积分数对近地表汞(0)扩散的控制。观测到的太阳辐射强度与汞通量之间的相关性,部分似乎是由于辐射、感热通量和潜热通量之间的表面能量平衡决定了土壤温度。模拟结果表明,仅基于通量室数据的经验相关性可能不适用于所有天气情况下的开阔大气。

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