Chemical Characteristics and Source Apportionment of Summer Precipitation at the Mount Wutai, Shanxi Province

In order to reveal chemical characteristics of precipitation at the Mount Wutai, based on continuous precipitation observation data from 20 events at the Mount Wutai in Shanxi Province from June to August in 2022. pH value, conductivity, composition and sources of major water-soluble ions in precipi...

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Main Authors: Jin Zehui, Zhou Qing, Wang Gaofang, Zhang Lei, Wang Zizhong, Zhang Long, Meng Jie, Huang Lei, Tian Conghai
Format: Article
Language:English
Published: Editorial Office of Journal of Applied Meteorological Science 2025-05-01
Series:应用气象学报
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Online Access:http://qikan.camscma.cn/en/article/doi/10.11898/1001-7313.20250309
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author Jin Zehui
Zhou Qing
Wang Gaofang
Zhang Lei
Wang Zizhong
Zhang Long
Meng Jie
Huang Lei
Tian Conghai
author_facet Jin Zehui
Zhou Qing
Wang Gaofang
Zhang Lei
Wang Zizhong
Zhang Long
Meng Jie
Huang Lei
Tian Conghai
author_sort Jin Zehui
collection DOAJ
description In order to reveal chemical characteristics of precipitation at the Mount Wutai, based on continuous precipitation observation data from 20 events at the Mount Wutai in Shanxi Province from June to August in 2022. pH value, conductivity, composition and sources of major water-soluble ions in precipitation are analyzed using methods such as the enrichment factor method, positive matrix factorization model (PMF) and Hybrid Single Particle Lagrangian Integrated Trajectory Model (HYSPLIT). Results indicate that the weighted average pH and conductivity values of rainfall during the summer at Mount Wutai are 6.16 and 15.51 μS·cm-1, respectively. It suggests that the acid rain pollution is not severe, and the precipitation composition is relatively clean. The ranking of the mass concentrations of major ions in precipitation, from highest to lowest, is as follows: SO42-, NO3-, NH4+, Ca2+, K+, Na+, Cl-, Mg2+ and F-. Percentages of NH4+ and Ca2+ in the total ion mass concentration are 20% and 7%, while percentages of SO42- and NO3- in the total ion mass concentration are 33% and 27%. Different ions exhibit different characteristics with rainfall under the influence of upstream air masses. Overall, compared with other high-altitude stations, it presents typical precipitation chemical characteristics of inland high-altitude stations. In the case of 0.01 significant level, the highest correlation coefficient is observed between SO42- and NO3- due to their similar chemical properties and related precursor emission characteristics, the correlation coefficient between K+ and Na+ is 0.899, the correlation coefficient between Mg2+and Ca2+ is 0.827, and the correlation coefficient between Mg2+ and Na+ is 0.778. K+ and Mg2+ are enriched relative to the ocean, and Cl- is diluted relative to the ocean and crust. Traffic activities and dust contribute significantly to levels of Cl- and Ca2+. Agricultural practices, such as fertilization, result in elevated concentrations of F- and NH4+. Additionally, biomass combustion is associated with higher levels of K+. SO42- and nitrate (NO3-) primarily originate from fossil fuel combustion and automobile exhaust emissions. Additionally, summer precipitation at the Mount Wutai is significantly influenced by the southerly air mass. The precipitation from the southern air mass (excluding NH4+) is greater than that from the northern air mass. The total ion concentration in the southern air mass is 1.3 times greater than that in the northern air mass.
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spelling doaj-art-d9ef0c2e9ed4414a8b696de3bd89d10f2025-08-20T02:38:19ZengEditorial Office of Journal of Applied Meteorological Science应用气象学报1001-73132025-05-0136335136310.11898/1001-7313.20250309yyqxxb-36-3-351Chemical Characteristics and Source Apportionment of Summer Precipitation at the Mount Wutai, Shanxi ProvinceJin Zehui0Zhou Qing1Wang Gaofang2Zhang Lei3Wang Zizhong4Zhang Long5Meng Jie6Huang Lei7Tian Conghai8Shanxi Meteorological Service Center, Taiyuan 030006Meteorological Observation Center of CMA, Beijing 100081Shanxi Meteorological Service Center, Taiyuan 030006Shanxi Meteorological Service Center, Taiyuan 030006Shanxi Meteorological Observatory, Taiyuan 030006Shanxi Meteorological Service Center, Taiyuan 030006Shanxi Meteorological Service Center, Taiyuan 030006Shanxi Meteorological Service Center, Taiyuan 030006Shanxi Meteorological Service Center, Taiyuan 030006In order to reveal chemical characteristics of precipitation at the Mount Wutai, based on continuous precipitation observation data from 20 events at the Mount Wutai in Shanxi Province from June to August in 2022. pH value, conductivity, composition and sources of major water-soluble ions in precipitation are analyzed using methods such as the enrichment factor method, positive matrix factorization model (PMF) and Hybrid Single Particle Lagrangian Integrated Trajectory Model (HYSPLIT). Results indicate that the weighted average pH and conductivity values of rainfall during the summer at Mount Wutai are 6.16 and 15.51 μS·cm-1, respectively. It suggests that the acid rain pollution is not severe, and the precipitation composition is relatively clean. The ranking of the mass concentrations of major ions in precipitation, from highest to lowest, is as follows: SO42-, NO3-, NH4+, Ca2+, K+, Na+, Cl-, Mg2+ and F-. Percentages of NH4+ and Ca2+ in the total ion mass concentration are 20% and 7%, while percentages of SO42- and NO3- in the total ion mass concentration are 33% and 27%. Different ions exhibit different characteristics with rainfall under the influence of upstream air masses. Overall, compared with other high-altitude stations, it presents typical precipitation chemical characteristics of inland high-altitude stations. In the case of 0.01 significant level, the highest correlation coefficient is observed between SO42- and NO3- due to their similar chemical properties and related precursor emission characteristics, the correlation coefficient between K+ and Na+ is 0.899, the correlation coefficient between Mg2+and Ca2+ is 0.827, and the correlation coefficient between Mg2+ and Na+ is 0.778. K+ and Mg2+ are enriched relative to the ocean, and Cl- is diluted relative to the ocean and crust. Traffic activities and dust contribute significantly to levels of Cl- and Ca2+. Agricultural practices, such as fertilization, result in elevated concentrations of F- and NH4+. Additionally, biomass combustion is associated with higher levels of K+. SO42- and nitrate (NO3-) primarily originate from fossil fuel combustion and automobile exhaust emissions. Additionally, summer precipitation at the Mount Wutai is significantly influenced by the southerly air mass. The precipitation from the southern air mass (excluding NH4+) is greater than that from the northern air mass. The total ion concentration in the southern air mass is 1.3 times greater than that in the northern air mass.http://qikan.camscma.cn/en/article/doi/10.11898/1001-7313.20250309precipitation chemistryionic compositionsource apportionment
spellingShingle Jin Zehui
Zhou Qing
Wang Gaofang
Zhang Lei
Wang Zizhong
Zhang Long
Meng Jie
Huang Lei
Tian Conghai
Chemical Characteristics and Source Apportionment of Summer Precipitation at the Mount Wutai, Shanxi Province
应用气象学报
precipitation chemistry
ionic composition
source apportionment
title Chemical Characteristics and Source Apportionment of Summer Precipitation at the Mount Wutai, Shanxi Province
title_full Chemical Characteristics and Source Apportionment of Summer Precipitation at the Mount Wutai, Shanxi Province
title_fullStr Chemical Characteristics and Source Apportionment of Summer Precipitation at the Mount Wutai, Shanxi Province
title_full_unstemmed Chemical Characteristics and Source Apportionment of Summer Precipitation at the Mount Wutai, Shanxi Province
title_short Chemical Characteristics and Source Apportionment of Summer Precipitation at the Mount Wutai, Shanxi Province
title_sort chemical characteristics and source apportionment of summer precipitation at the mount wutai shanxi province
topic precipitation chemistry
ionic composition
source apportionment
url http://qikan.camscma.cn/en/article/doi/10.11898/1001-7313.20250309
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