To elucidate the differences in the dry deposition process between sulfate and nitrate in PM
2.5, vertical profiles of the inorganic components were measured in a forest in suburban Tokyo (FM Tama site) for one year from December, 2012 to November, 2013. We carried out weekly samplings of PM
2.5 at 4 heights (2 heights above canopy, 2 heights below canopy) on a tower built in the forest. The major inorganic aerosols consisted of NH
4NO
3 and (NH
4)
2SO
4 at the 4 heights through out the year. Significant differences between the SO
42- and NO
3- profiles were observed. NO
3- relatively decreased compared to SO
42- toward the forest floor through out the year. In the winter and spring, the air temperature of the forest floor was higher than that of the other heights. On the other hand, in the summer and autumn, the air temperature of the forest floor was lower than that of the other heights. The profiles of the concentrations and the air temperatures indicated that volatilization of NH
4NO
3 by the higher temperature on the floor caused the rapid decrease of NO
3- in the winter and spring, and the volatilization of NH
4NO
3 by the low concentration of HNO
3 due to its significant removal by the leaves caused the rapid decrease of NO
3- in the summer and autumn. These volatilization processes indicated that the dry deposition of ammonium nitrate to forests was more efficient than that of ammonium sulfate.
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