Abstract
The seasonal and inter-annual variations of pH and EC (electrical conductivity) at Yulong (chinese source) Snow Mountain, Lijiang (chinese source) City, are sensitive to precipitation variations and are important indicators of the atmospheric environment. The pH of summer rainfall at Lijiang City ranges from 6.7 to 7.4, and alkaline mineral salts dominate the variations of rainfall acidity. pH values in the shallow firn profile at Baishui (chinese source) Glacier No. 1 range from 5.6 to 6.3, and EC values from 2.4 to 7.3 μs/cm. The ranges are lower than those in other firn cores from China because of stronger elution and the influence of marine aerosols. This indicates that environmental records from a monsoonal temperate glacier differ from those at continental glaciers. © 2010 China University of Geosciences and Springer-Verlag Berlin Heidelberg.
Original language | English |
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Pages (from-to) | 157-165 |
Number of pages | 8 |
Journal | Journal of Earth Science |
Volume | 21 |
Issue number | 2 |
DOIs | |
Publication status | Published - 2010 |
Keywords
- Baishui Glacier No. 1
- EC
- Lijiang City
- pH
- Yulong Snow Mountain