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Journal of Atmospheric Chemistry

, Volume 71, Issue 2, pp 157–174 | Cite as

Chemical composition of rainwater at Lijiang on the Southeast Tibetan Plateau: influences from various air mass sources

  • Ningning ZhangEmail author
  • Junji Cao
  • Yuanqing He
  • Shun Xiao
Article

Abstract

Daily rainwater samples collected at Lijiang in 2009 were analyzed for pH, electrical conductivity, major ion (SO4 2−, Cl, NO3 , Na+, Ca2+, Mg2+, and NH4 +) concentrations, and δ18O. The rainwater was alkaline with the volume-weighted mean pH of 6.34 (range: 5.71 to 7.11). Ion concentrations and δ18O during the pre-monsoon period were higher than in the monsoon. Air mass trajectories indicated that water vapor from South Asia was polluted with biomass burning emissions during the pre-monsoon. Precipitation during the monsoon was mainly transported by flow from the Bay of Bengal, and it showed high sea salt ion concentrations. Some precipitation brought by southwest monsoon originated from Burma; it was characterized by low δ18O and low sea salt, indicating that the water vapor from the region was mainly recycled monsoon precipitation. Water vapor from South China contained large quantities of SO4 2−, NO3 , and NH4 +. Throughout the study, Ca2+ was the main neutralizing agent. Positive matrix factorization analysis indicated that crustal dust sources contributed the following percentages of the ions Ca2+ 85 %, Mg2+ 75 %, K+ 61 %, NO3 32 % and SO4 2− 21 %. Anthropogenic sources accounted for 79 %, 68 %, and 76 % of the SO4 2−, NO3 and NH4 +, respectively; and approximately 93 %, 99 %, and 37 % of the Cl, Na+, and K+ were from a sea salt source.

Keyword

Alkaline rain Air mass Neutralization PMF analysis 

Notes

Acknowledgments

This work was supported by the Natural Science Foundation of China (NSFC40801028, 40925009), the West Light Foundation of Chinese Academy of Sciences, projects from the Chinese Academy of Sciences (No O929011018, KZCX2-YW-BR-10 and KZCX2-YW-148), the Ministry of Science & Technology (2012BAH31B03, 2009IM030100) and Meteorological Innovative Research Project of Baoji Meteorological Bureau (No.T2012-01). We sincerely thank the staffs at the Yulong Snow Mountain glacial and environment observation station who were instrumental in the field work.

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Copyright information

© Springer Science+Business Media Dordrecht 2014

Authors and Affiliations

  • Ningning Zhang
    • 1
    • 2
    Email author
  • Junji Cao
    • 1
    • 3
  • Yuanqing He
    • 2
  • Shun Xiao
    • 1
    • 4
    • 5
  1. 1.Key Laboratory of Aerosol Chemistry & Physics, SKLLQG, Institute of Earth EnvironmentChinese Academy of SciencesXi’anChina
  2. 2.State key Laboratory of Cryspheric science, Cold and Arid Regions Environmental and Engineering Research InstituteChinese Academy of SciencesLanzhouChina
  3. 3.Institute of Global Environmental ChangeXi’an Jiaotong UniversityXi’anChina
  4. 4.Climate Center of Shaanxi Meteorological BureauXi’anChina
  5. 5.Meteorological Bureau of Baoji MunicipalityBaojiChina

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