The loss of Cl as HC1 from sea salt particles by air pollutants (NO
3- and SO
42-) in the marine atmosphere was discussed, based on both laboratory experiments and field measurements.
In the laboratory experiments, the release of gaseous HCl from sea salt particles was simulated by passing NO
2 or SO
2 through a filter impregnated with sea water. The release of HCl from the filter occurred by the aeration with NO
2 or SO
2, and the concentration of HClreleased depended on both the concentration of NO
2 or SO
2 and relative humidity. The generation rates of HC1 calcurated from the added amounts of NO
2 and SO
2 were 9% for NO
2and 18% for SO
2 (Table 1 and 2).
The marine aerosol was collecte d by Andersen samplers during January 13-20 and December 14-20, 1981 in the two remote islands, Hachijo-jima and Chichi-jima in order to in vestigate the Cl loss from sea salt in the marine atmosphere. The calcurated Cl losses from sea salt particles ( <2 μm) based on the Cl/Na ratio in sea water (1.8) were 0.21 to 0.36 pg/m
3, and 2 to 7% of total particulate marine Cl at the two islands. The Cl loss from sea salt particles smaller than 1 gm was more than 20%, while that from particles larger than 2iam was negligible (Fig.4). A linear correlation was observed between measured SO
42- concentrations (<2 μm) and Cl losses, indicating a 1.1 iimol/m
3 Cl loss per 1 iumol/m
3 SO
42- (Fig.5). The HCl concentrations estimated from the Cl losses (5.9×10
-3 to 10× 10
-3, μmol/m
3 ) agreed with the measured HCl concentrations in the marine atomosphere (4.8 × 10
-3 to 15 × 10
3, μmolf m
3) (Table 5), suggesting that the release salt particles is the main source of gaseous HCl in the marine atomosphere.
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