Abstract
Calcium (Ca) species in aerosol (dust) particles trapped during spring in an ice core at Southeast Greenland (SE-Dome) were examined using X-ray absorption near-edge structure spectroscopy (XANES). The ice core has a record of aerosols from 1957 to 2014, and the samples corresponding to 1971, 1978, 1987, 1995, and 2004 were selected for analysis. Results showed that gypsum fraction to total Ca in the ice core was larger in the recent layers (1995 and 2004) than in the old layers (1971, 1978, and 1987), whereas calcite fraction exhibited the opposite trend. The increased gypsum content was consistent with the increase of SO2 annual emission in China. Given that Ca-bearing dust particles were originally supplied as calcite derived from East Asia, this study suggests that the Ca species in the dust trapped in the ice core can be a good indicator of the secular variation of SO2 emission in this region.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.