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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Total gaseous mercury emissions from soil in Guiyang, Guizhou, China
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Total gaseous mercury emissions from soil in Guiyang, Guizhou, China

机译:贵州贵阳土壤中气态汞的总排放量

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摘要

Guiyang is located in the Circum-Pacific Global Mercuriferous Belt, and mercury concentrations in soil in this area are enriched. In situ total gaseous mercury (TGM) exchange fluxes between air and soil surface were intensively measured at four sampling sites in Guiyang from 21 May to 16 June 2003. Overall, net emissions were obtained from all sampling sites. Soil mercury concentration and solar radiation are proved to be the two most important parameters to control mercury emissions from soil. Meanwhile, a rain event can enhance mercury emission rate significantly. A simple model based on the linear correlation between mercury flux and solar radiation was applied to scale up mercury emissions from soil zones with different mercury concentration ranges. It is observed that mercury emission fluxes from soil in Guiyang are one order of magnitude higher than the value used in early models to represent emissions from global mercuriferous belts which is 1.1 ng m?2 h?1. The annual mercury emission from soil in Guiyang is calculated to be 408 kg, which highlights that natural emissions from soil contribute significantly to the elevated TGM concentrations in the ambient air in Guiyang.
机译:贵阳位于环太平洋全球汞化带,该地区土壤中的汞含量富集。 2003年5月21日至6月16日,在贵阳的四个采样点对空气和土壤表面之间的原位总气态汞(TGM)交换通量进行了测量。总体而言,所有采样点均获得了净排放量。事实证明,土壤汞浓度和太阳辐射是控制土壤汞排放的两个最重要参数。同时,降雨可以显着提高汞排放率。一个简单的模型基于汞通量和太阳辐射之间的线性相关性,用于按比例放大来自不同汞浓度范围的土壤区域的汞排放量。据观察,贵阳土壤中的汞排放通量比早期模型中用来表示全球汞铁带排放的1.1 ng m?2 h?1的值高一个数量级。据计算,贵阳土壤每年的汞排放量为408千克,这表明贵阳土壤的自然排放量是造成大气中TGM浓度升高的重要原因。

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