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DRY DEPOSITION OF SULFUR CONTAINING SPECIES TO THE WATER SURFACE SAMPLER AT TWO SITES

机译:在两个站点上将含硫物种干沉积到水表面采样器中

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Sulfate dry deposition increases the deteriorating effects on environment. Sulfate can be deposited from atmosphere to water via both particulate (SO_4~(2-): sulfate) and a gas (SO_2: sulfur dioxide) form. In this research, the fluxes of gaseous (SO_2) and particulate (SO_4~(2-)) species were measured employing a water surface sampler (WSS) and glass fiber filters (GFFs) on the knife-edge surrogate surface (KSSs) in the campus of Uludag University and the city of Bursa, Turkey. Sampling program was conducted intermittently between September 2004 and March 2005. Average total sulfate fluxes measured with the WSS at the Uludag University campus and in the city of Bursa were 58 ± 41 and 235 ± 43 mg m~(-2) d~(-1), respectively. The total sulfate fluxes measured at Bursa were higher and this was probably due to greater sulfur containing species in its atmosphere. The dry deposition of gaseous SO_2 flux was calculated by subtracting the particulate flux collected with the KSSs from the total flux (particulate sulfate plus SO_2 flux) obtained by the WSS. An automatic SO_2 analyzer was used concurrently to measure the ambient concentration of gaseous SO_2. The average SO_2 gas fluxes and ambient SO_2 concentrations were 18 ± 28 and 54 ± 48 mg m~(-2) day~(-1) and 11 ± 7 and 49 ± 14 μg m~(-3) for the campus and the city, respectively. The measured gaseous SO_2 fluxes and ambient concentrations were used to calculate the mass transfer coefficient. The calculated MTC values for the campus and the city were 0.8 ± 1.0 and 1.2 ± 1.1 cm s~(-1), respectively. These values were in agreement with previously reported dry deposition velocities for SO_2.
机译:硫酸盐干沉降增加了对环境的恶化作用。硫酸盐可以通过颗粒(SO_4〜(2-):硫酸盐)和气体(SO_2:二氧化硫)形式从大气中沉积到水中。在这项研究中,气态(SO_2)和颗粒(SO_4〜(2-))的通量是使用水表面采样器(WSS)和玻璃纤维过滤器(GFFs)在刀口替代表面(KSSs)上测量的。乌鲁达大学校园和土耳其布尔萨市。在2004年9月至2005年3月间断地进行了采样程序。在乌鲁达大学校园和布尔萨市使用WSS测量的平均总硫酸盐通量为58±41和235±43 mg m〜(-2)d〜(- 1)。在布尔萨(Bursa)测得的总硫酸盐通量较高,这可能是由于其大气中含有更多的含硫物质。通过从由WSS获得的总通量(硫酸盐加SO_2通量)中减去用KSS收集的颗粒通量,计算出气态SO_2通量的干沉降。同时使用自动SO_2分析仪测量气态SO_2的环境浓度。校园和校园的平均SO_2气体通量和周围SO_2浓度分别为18±28和54±48 mg m〜(-2)day〜(-1)和11±7和49±14μgm〜(-3)。城市。使用测得的气态SO_2通量和环境浓度来计算传质系数。计算得出的校园和城市的MTC值分别为0.8±1.0和1.2±1.1 cm s〜(-1)。这些值与先前报道的SO_2的干沉积速度一致。

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