Institute Atmospheric and Environmental Science, Crew Building, University of Edinburgh, King's Buildings, Edinburgh EH9 3JN, UK.
Sci Total Environ. 2010 Jan 15;408(4):985-95. doi: 10.1016/j.scitotenv.2009.10.048. Epub 2009 Nov 10.
An atmospheric transport-chemistry model is applied to investigate the effects of source configuration in simulating regional sulphur deposition footprints from elevated point sources. Dry and wet depositions of sulphur are calculated for each of the 69 largest point sources in the UK. Deposition contributions for each point source are calculated for 2003, as well as for a 2010 emissions scenario. The 2010 emissions scenario has been chosen to simulate the Gothenburg protocol emission scenario. Point source location is found to be a major driver of the dry/wet deposition ratio for each deposition footprint, with increased precipitation scavenging of SO(x) in hill areas resulting in a larger fraction of the emitted sulphur being deposited within the UK for sources located near these areas. This reduces exported transboundary pollution, but, associated with the occurrence of sensitive soils in hill areas, increases the domestic threat of soil acidification. The simulation of plume rise using individual stack parameters for each point source demonstrates a high sensitivity of SO(2) surface concentration to effective source height. This emphasises the importance of using site-specific information for each major stack, which is rarely included in regional atmospheric pollution models, due to the difficulty in obtaining the required input data. The simulations quantify how the fraction of emitted SO(x) exported from the UK increases with source magnitude, effective source height and easterly location. The modelled reduction in SO(x) emissions, between 2003 and 2010 resulted in a smaller fraction being exported, with the result that the reductions in SO(x) deposition to the UK are less than proportionate to the emission reduction. This non-linearity is associated with a relatively larger fraction of the SO(2) being converted to sulphate aerosol for the 2010 scenario, in the presence of ammonia. The effect results in less-than-proportional UK benefits of reducing in SO(2) emissions, together with greater-than-proportional benefits in reducing export of UK SO(2) emissions.
大气输送-化学模型被应用于研究模拟来自高空点源的区域硫沉积足迹时源配置的影响。计算了英国 69 个最大的点源中的每个源的干湿沉降。计算了每个点源在 2003 年以及 2010 年排放情景下的沉积贡献。选择 2010 年排放情景来模拟哥德堡议定书的排放情景。点源位置是每个沉积足迹干/湿沉降比的主要驱动因素,在丘陵地区降水对 SO(x)的清除作用增加,导致在靠近这些地区的源处沉积的排放硫的比例更大。这减少了跨境污染的输出,但与丘陵地区敏感土壤的存在相关,增加了国内土壤酸化的威胁。使用每个点源的单个烟囱参数模拟羽流上升,表明 SO2 地表浓度对有效源高的高度敏感。这强调了使用每个主要烟囱的特定于地点的信息的重要性,由于难以获得所需的输入数据,因此很少在区域大气污染模型中包含这些信息。这些模拟量化了从英国出口的排放 SO(x)的比例如何随源强度、有效源高和偏东位置的增加而增加。2003 年至 2010 年期间模拟的 SO(x)排放量减少导致出口量减少,因此英国的 SO(x)沉积减少量小于排放量减少量的比例。这种非线性与氨存在时 2010 年情景中 SO2 转化为硫酸盐气溶胶的比例相对较大有关。结果导致英国减少 SO2 排放的好处不成比例,减少英国 SO2 排放的出口好处不成比例。