A four-stage filter pack method (F
0: PTFE, F
1: polyamide, F
2: 6%K
2CO
3+2% glycerol impregnated and F
3: 5 % phosphoric acid +2 % glycerol impregnated filters) was used to sample the atmosphere for determination of gas (SO
2, HNO
3, HCl, NH
3) and particulate matter (SO
42-, NO
3-, Cl
-, Na
+, NH
4+, K
+, Ca
2+, Mg
2+) concentrations. The average concentrations of SO
2, H NO
3, HCl, NH
3 gases and SO
42-, NO
3-, Cl
-, Na
+, NH
4+, K
+, Ca
2+ and Mg
2+ particles were 76.2 (1.83), 27.3 (0.66), 31.8 (0.76), 115 (2.76), 52.3, 47.7, 45.1, 34.4, 121, 9.4, 20.5 and 6.2 nmol/m
3 (ppb: 20 °C), respectively.
The gases and particulate matter concentrations were multiplied by dry deposit ion velocities for various surfaces (bare soil, farmland, deciduous forest, coniferous forest) from the literature to estimate dry deposition. The coniferous forest received the greatest dry deposition of SO
42- and NO
3-. The average amounts of dry deposition of SO
42- and NO
3- estimated with data from a Wet/Dry collector were 0.692 and 0.601 molm
-2/month, respectively, smaller than the average amounts obtained with the inferential method. The contribution of dry deposition to total deposition was greater for gaseous species than for particulate matter. In the coniferious forest, the SO
42- and NO
3- contributions to total dry deposition were 59 and 77%, respectively. Forest damage cannot be fully evaluated by wet deposition measurements alone; estimate of dry deposition of HNO
3 to coniferous forests will advance our understanding of forest damage by acidic deposition.
View full abstract