新万金填海造地地区大气氨浓度的年分布

Sung-Chang Hong, Min-Wook Kim, Jin-Ho Kim
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引用次数: 1

摘要

背景:最近,研究表明,大气氨(NH3)通过与酸性物质(如SO2、NOx)反应,在大气中形成PM2.5气溶胶,在二次颗粒物的形成中起主要作用。全北地区是颗粒物浓度较高的地区。由于219平方公里的新万金填海造地的环境变化,有必要对全北地区的颗粒物和大气氨的影响进行评估。方法与结果:使用被动采样器和CRDS分析仪测量2020年6月至2021年5月的大气氨浓度。被动采样器测得的季节和年大气氨浓度(本底浓度)在11.4 ~ 18.2 μg/m3之间,显著降低。扶安、金堤、群山、完州地区的大气氨浓度虽然有轻微的季节差异,但没有明显的差异。安装在新万金填海造地附近的综合综合设施的CRDS分析仪测得的最大大气氨浓度分别为:秋季51.5 μg/m3、夏季48.0 μg/m3、冬季37.6 μg/m3、春季32.7 μg/m3。春季最低浓度为4.9 μg/m3,夏季最低浓度为4.2 μg/m3,秋冬季最低浓度为3.5 μg/m3。年平均浓度为14.6 μg/m3。结论:需要对农区大气氨进行长期监测,以评价细颗粒物的形成及其对环境的影响。此外,减少农田氨排放的技术需要不断发展。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Annual Distribution of Atmospheric Ammonia Concentration in Saemangum Reclaimed Land Area
BACKGROUND: More recently, it has been shown that atmospheric ammonia (NH3) plays a primary role in the formation of secondary particulate matter by reacting with the acidic species, e.g. SO2, NOx, to form PM2.5 aerosols in the atmosphere. The Jeonbuk region is an area with high concentration of particulate matter. Due to environmental changes in the Saemangeum reclaimed land with an area of 219 km2, it is necessary to evaluate the impact of the particulate matter and atmospheric ammonia in the Jeonbuk region. METHODS AND RESULTS: Atmospheric ammonia concentrations were measured from June 2020 to May 2021 using a passive sampler and CRDS analyzer. Seasonal and annual atmospheric ammonia concentration measured using passive sampler was significantly lower in Jangjado (background concentration), and the concentration ranged from 11.4 μg/m3 to 18.2 μg/m3. Atmospheric ammonia concentrations in Buan, Gimje, Gunsan, and Wanju regions did not show a significant difference, although there was a slight seasonal difference. The maximum atmospheric ammonia concentration measured using the CRDS analyzer installed in the IAMS near the Saemangeum reclaimed land was 51.5 μg/m3 in autumn, 48.0 μg/m3 in summer, 37.6 μg /m3 in winter, and 32.7 μg/m3 in spring. The minimum concentration was 4.9 μg/m3 in spring, 4.2 μg/m3 in summer, and 3.5 μg/m3 in autumn and winter. The annual average concentration was 14.6 μg/m3. CONCLUSION(S): Long term monitoring of atmospheric ammonia in agricultural areas is required to evaluate the formation of fine particulate matter and its impact on the environment. In addition, continuous technology development is needed to reduce ammonia emitted from farmland.
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