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长江口湿沉降汞的时间分布及潜在生态危害 被引量:3
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作者 张国玉 周立旻 +1 位作者 郑祥民 黄文丹 《城市环境与城市生态》 CAS CSCD 2010年第2期1-4,共4页
于2008年2月-2009年1月逐月采集长江口右岸陈行采样点的大气湿沉降样品,测试样品的总汞、溶解态汞浓度。分析结果显示,不同月份湿沉降中各形态汞的浓度变化较大,其中总汞浓度变化范围在0.09-0.45μg/L,体积加权平均值为0.22μg/L,总汞... 于2008年2月-2009年1月逐月采集长江口右岸陈行采样点的大气湿沉降样品,测试样品的总汞、溶解态汞浓度。分析结果显示,不同月份湿沉降中各形态汞的浓度变化较大,其中总汞浓度变化范围在0.09-0.45μg/L,体积加权平均值为0.22μg/L,总汞沉降通量高达199.79μg/(m2.a),远高于其它地区,该区域的大气已经受到一定程度的汞污染。总汞、颗粒态汞月沉降量与降水量呈明显的正相关关系(除6月份),总汞浓度与降水量在汛期(6-9月份)具有良好的负相关性,大气湿沉降汞的形态受到人为活动产生的颗粒物的影响,颗粒态汞占总汞比例变化范围在14%-89%之间,平均为62%。以地表水Ⅲ类标准0.1μg/L为评价标准,长江口湿沉降汞的潜在生态危害系数高,全年湿沉降汞平均值属于强生态危害范围。 展开更多
关键词 湿沉降汞 浓度 降水量 长江口
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我国燃煤汞沉降的数值模拟 被引量:6
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作者 权建农 张晓山 +1 位作者 张蔷 李宏宇 《高原气象》 CSCD 北大核心 2009年第1期159-164,共6页
利用CMAQ-Hg(Community Multi-scale Air Quality-Mercury)模式模拟了我国燃煤排放的大气汞在我国区域的沉降分布状况,其中气象模式为MM5。模式中包括了三种价态汞(气态元素汞(GEM)、气态活性汞(RGM)和颗粒汞(PHg))的气相、... 利用CMAQ-Hg(Community Multi-scale Air Quality-Mercury)模式模拟了我国燃煤排放的大气汞在我国区域的沉降分布状况,其中气象模式为MM5。模式中包括了三种价态汞(气态元素汞(GEM)、气态活性汞(RGM)和颗粒汞(PHg))的气相、液相、非均相化学反应过程以及输送、干湿沉降等物理过程。中国燃煤排放的大气汞中RGM所占比例较高,约为58.4%-66.8%,这导致我国汞沉降量较大。模拟结果表明,在我国的西南地区、华东地区以及京津塘地区燃煤汞的沉降较高,在这些区域的沉降通量高达2-6μg m^-2 mon^-1。燃煤大气汞排放形态对汞的沉降有重要影响,减少燃煤汞排放中RGM的比例能够显著降低我国区域汞的沉降通量。 展开更多
关键词 区域模式(CMAQ-Hg) 燃煤排放 形态分布 湿沉降
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Effect of Wet Settlement on Mercury in Alpine Soil in Mercury Mining Area
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作者 HEJIN-LIN TANHONG 《Pedosphere》 SCIE CAS CSCD 1995年第4期379-381,共3页
EffectofWetSettlementonMercuryinAlpineSoilinMercuryMiningAreaHEJIN-LINandTANHONG(GuizhouResearchCentreofPhys... EffectofWetSettlementonMercuryinAlpineSoilinMercuryMiningAreaHEJIN-LINandTANHONG(GuizhouResearchCentreofPhysicalTestingandChe... 展开更多
关键词 alpine soil gaseons Hg wet settlement
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Preliminary Assessment of Total Mercury in Bulk Precipitation around Olkaria Area, Kenya
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作者 G.N. Wetang'ula 《Journal of Environmental Science and Engineering》 2011年第12期1585-1595,共11页
Geothermal power plants are receiving increasing attention as regards the mobilization of mercury (Hg) to the environment. Hg is a trace element that may be present in the geothermal fluid, but due to its volatility... Geothermal power plants are receiving increasing attention as regards the mobilization of mercury (Hg) to the environment. Hg is a trace element that may be present in the geothermal fluid, but due to its volatility, it is transferred mainly into the vapor phase. Hence, it may be mostly discharged to the atmosphere with the non-condensable gases. Olkaria geothermal field hosts 3 geothermal power plants. In this area Hg deposition fluxes have not been studied. Concentrations and wet deposition fluxes of total mercury (T-Hg) were determined from April 2009 to May 2010 at 2 sites in this field. Event-based precipitation samples were collected using fabricated bulk precipitation samplers. Samples were treated according to trace metal protocol and analyzed by cold vapor atomic fluorescence spectrometry (CVAFS). This paper thus reports the first ever determination of T-Hg concentrations and fluxes in precipitation. The T-Hg concentration in samples ranged from 0.002-0.0602 μg/L at the two sites, however, the volume-weighted mean concentration and wet deposition flux were 0.01974 and 0.02884μg.L^-1 and 0.0167-1.45 μg.m2 during the study period. The annual volume-weighted mean wet deposition fluxes of T-Hg for 2 sites were 13.74 and 19.83 μg.m-2.yr-1 with an average flux of 16.785μg.m-2.yr-1. Hg concentrations and the Hg fluxes in precipitation showed seasonal trends being lowest in the short-rains and highest in the long rains. The concentrations of T-Hg for the 2 sites is negatively correlated with the precipitation depth (r2 = 0.26 & r2 = 0.0065), suggesting that scavenging of particle-bound mercury from the atmosphere is an important mechanism contributing to mercury in rainwater. Mean Hg concentrations in precipitation at the study sites were comparable to the ranges reported for Canada and the USA by the Mercury Deposition Network (MDN). 展开更多
关键词 Olkaria GEOTHERMAL MERCURY total mercury bulk precipiation.
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