A copy of this work was available on the public web and has been preserved in the Wayback Machine. The capture dates from 2014; you can also visit the original URL.
The file type is
A quantitative analysis of the total concentrations of Al and Na in the Antarctic ice sheet during the past 340 kyr was performed by applying the acid digestion method to the Dome Fuji ice core. Atmospheric fluxes of mineral and sea-salt aerosol to Dome Fuji were calculated from the total concentration. The average fluxes of mineral aerosol to Dome Fuji in the periods of glacial maximum, 18.6 ± 10.1 mg·m -2 ·yr -1 , were larger than the value in the interglacial periods, 3.77 ± 2.20 mg·m -2 ·yrdoi:10.4236/acs.2013.32020 fatcat:nz466dwafngbxjbixv7qpb3pu4