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Concentrations of Atmospheric Sulfur Compounds in an Extremely Snowy Region the Hokuriku District Japan

机译:日本北陆地区雪域中的大气硫化合物浓度

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摘要

The diurnal and seasonal characteristics in gaseous sulfur dioxide and sulfate in aerosol particles, as well as the concentrations of sulfate in rain and snow, were measured in the Hokuriku District, Japan in order to investigate the spatial spread pattern of sulfur compounds and identify the origin of sulfur. The concentration of sulfur dioxide showed a distinct diurnal pattern, while the concentrations of nss-SO4 in precipitation and aerosol particles did not. These results implied that the sulfur dioxide might originate in local emissions and did not affect the concentration of nss-SO4 in precipitation, while nss-SO4 in aerosol particles seemed to be widespread and might result from long-range transportation. The deposition of nss-SO4 in precipitation increased in winter, while the concentration of nss-SO4 in aerosol particles decreased. This could be attributed to the lower cloud base often observed in this district in winter associated with a higher washout ratio.
机译:在日本北陆地区,测量了气溶胶颗粒中气态二氧化硫和硫酸盐的日,季节特征以及雨雪中的硫酸盐浓度,以调查硫化合物的空间扩散模式并确定其来源。硫。二氧化硫的浓度表现出明显的昼夜模式,而沉淀和气溶胶颗粒中的nss-SO4浓度却没有。这些结果表明,二氧化硫可能起源于局部排放,并且不影响降水中nss-SO4的浓度,而气溶胶颗粒中的nss-SO4似乎很普遍,可能是由于远距离运输所致。冬季降水中nss-SO4的沉积增加,而气溶胶颗粒中nss-SO4的浓度降低。这可能归因于冬季在该地区经常观察到的较低的云层基数和较高的冲刷比。

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