Key Laboratory of Tibetan Environment Changs and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China; Laboratory of Green Chemistry, Lappeenranta University of Technology, Sammonkatu 12, 50130 Mikkeli, Finland; Graduate University of Chinese Academy of Sciences, Beijing 100039, China.
State Key Laboratory of Cryospheric Sciences, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China; Center for Excellence in Tibetan Plateau Earth Sciences, Chinese Academy of Sciences, Beijing 100085, China.
Sci Total Environ. 2017 Feb 1;579:1240-1248. doi: 10.1016/j.scitotenv.2016.11.110. Epub 2016 Nov 30.
The Kathmandu Valley, located in the Himalayan foothills in Nepal, is heavily polluted. In order to investigate ambient particulate-bound mercury (Hg) in the Kathmandu Valley, a total 64 total suspended particulates (TSP) samples were collected from a sub-urban site in the Kathmandu Valley, the capital region of Nepal during a sampling period of an entire year (April 2013-April 2014). They were analyzed for ambient particulate-bound Hg (PBM) using thermal desorption combined with cold vapor atomic spectroscopy. In our knowledge, it is the first study of ambient PMB in the Kathmandu Valley and the surrounding broader Himalayan foothill region. The average concentration of PBM over the entire sampling period of a year was found to be 850.5 (±962.8) pg m in the Kathmandu Valley. This is comparable to those values reported in the polluted cities of China and significantly higher than those observed in most of urban areas in Asia and other regions of world. The daily average Hg contents in TSP (PBM/TSP) ranges from 269.7 to 7613.0ngg with an average of 2586.0 (±2072.1) ng g, indicating the high enrichment of Hg in TSP. The average concentrations of PBM were higher in the winter and pre-monsoon season than in the monsoon and post-monsoon season. The temporal variations in the strength of anthropogenic emission sources combined with other influencing factors, such as ambient temperature and the removal of atmospheric aerosols by wet scavenging are attributable to the seasonal variations of PBM. The considerably high dry deposition flux of PBM estimated by using a theoretical model was 135μgmyr at the Kathmandu Valley. This calls for an immediate attention to addressing ambient particulate Hg in the Kathmandu Valley, including considering it as a key component of future air quality monitoring activities and mitigation measures.
加德满都谷地位于尼泊尔喜马拉雅山麓,污染严重。为了研究加德满都谷地的环境颗粒态汞(PBM),我们于 2013 年 4 月至 2014 年 4 月在尼泊尔首都加德满都谷地的一个郊区点采集了总共 64 个总悬浮颗粒物(TSP)样本。使用热解吸结合冷蒸气原子光谱法分析了这些样本中环境颗粒态汞(PBM)的含量。据我们所知,这是首次对加德满都谷地及周边更广阔的喜马拉雅山麓地区的环境 PBM 进行的研究。在整个一年的采样期间,PBM 的平均浓度为 850.5(±962.8)pg m 在加德满都谷地。这与中国污染城市报告的值相当,明显高于亚洲大部分城市地区和世界其他地区观察到的值。TSP 中汞的日平均含量(PBM/TSP)范围为 269.7 至 7613.0ng g,平均值为 2586.0(±2072.1)ng g,表明 Hg 在 TSP 中高度富集。PBM 在冬季和前季风季的浓度高于季风季和后季风季。人为排放源强度的时间变化以及环境温度等其他影响因素的变化,加上通过湿清除去除大气气溶胶,是导致 PBM 季节性变化的原因。使用理论模型估算的 PBM 干沉降通量相当高,在加德满都谷地为 135μgmyr。这呼吁立即关注加德满都谷地的环境颗粒态汞问题,包括考虑将其作为未来空气质量监测活动和缓解措施的关键组成部分。