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首页> 外文期刊>ournal of the Meteorological Society of Japan >Seasonal Changes in the Concentrations of Major Cations and Anions in Precipitations in Urban Nagoya, Japan
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Seasonal Changes in the Concentrations of Major Cations and Anions in Precipitations in Urban Nagoya, Japan

机译:日本名古屋市区降水中主要阳离子和阴离子浓度的季节性变化

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A continuous sampling at every 0.5mm of precipitation during rain (average sampling time of 19 minutes) and analyses of ions involved in the rainwater were carried out from April 1, 1993 to March 31, 1994 in Nagakute, 16km east of Nagoya, Japan, to understand temporal changes in ion concentrations in precipitation in detail. The average pH, nitrate (NO3-), and non-seasalt sulfate (nss-SO42-) in the collected rainwaters were 4.76, 14.5μeq l-1 and 18.0μeq l-1, respectively. The average concentrations of ions obtained in this study were about half of those obtained during 1984 and 1986 by the Japan Environmental Agency, which was thought to be caused by either the longer rainy season in 1993 or the reduction of sulfur dioxide emission in recent years.The seasonal changes in ion concentrations show that they were significantly influenced by Asian dust storms and typhoons. Asian dust storms and typhoons were found to play important role in characterizing the precipitation chemistry in Japan.A rapid change in ion concentrations during several minutes was frequently found in individual precipitation accompanied by weather change. Concentrations of NO3-, NH4+, and SO42- decreased with an increase in wind speed, while those of Na+ and Cl- increased, showing the differences in the production and the deposition processes of ions. Higher concentrations of NO3- and nss-SO42- in rain samples with southern wind direction were frequently observed, showing a clear relation to the industrial facilities of ion sources located in the southern direction. A greater amount of ammonium ion (NH4+) was observed to be transported from the suburbs of Nagoya rather than from the downtown area. This measurement (short period sampling and continuous observation) showed characteristics typical of a precipitation chemistry, especially for the seasonal concentration change in major cations and anions and ion transport processes, observed in suburbs in the eastern Asia region.
机译:1993年4月1日至1994年3月31日,在日本名古屋以东16公里的长久手市,对雨中每0.5mm降水量进行连续采样(平均采样时间为19分钟),并对雨水中的离子进行分析。详细了解降水中离子浓度的时间变化。收集的雨水的平均pH值分别为4.76、14.5μeq l-1和18.0μeql-1,硝酸盐(NO3-)和非海水硫酸盐(nss-SO42-)。这项研究中获得的离子平均浓度约为日本环境署在1984年和1986年获得的离子的一半,这被认为是由于1993年雨季延长或近年来二氧化硫排放减少所致。离子浓度的季节性变化表明它们受到亚洲沙尘暴和台风的重大影响。人们发现亚洲沙尘暴和台风在日本降水化学特征中起着重要作用。个别降水中伴随着天气变化的离子浓度在几分钟内迅速变化。随着风速的增加,NO3-,NH4 +和SO42-的浓度降低,而Na +和Cl-的浓度增加,这表明离子的产生和沉积过程存在差异。经常观察到南风向的雨水样品中NO3-和nss-SO42-的浓度较高,这与南风向的离子源的工业设施有着明显的关系。观察到从名古屋市郊而不是从市区迁移出了更多的铵离子(NH4 +)。这种测量(短期采样和连续观察)显示了沉淀化学的典型特征,尤其是在东亚地区郊区观察到的主要阳离子和阴离子的季节性浓度变化以及离子迁移过程。

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