When precipitation passes through forest canopies, some ion concentration may increase while others may decrease in the throughfall. The enrichment phenomena result from the heavy metal ions leaching from plant tissue and the removal of dry deposition, while decrease in heavy metal ions concentration is due to heavy metal ions absorption into plant tissue. This phenomena seems to be emphasized by increasing H
+ concentration in the rain. This study was carried out to make clear how chemistry of the simulated rain water solution was changed when epiphytic lichens were submerged at varing acidity and time. Fe, Mn, Zn and Cd was leached from the thallus to the solution above a peculiar ranges of H
+ concentration of simulated rain water, while absorbed from the solution to the thallus bellow the ranges of concentration. The peculiar pH range was 2.7-3.1 for Fe, 3.4-3.6 for Mn, 3.1-3.3 for Zn and 2.4 for Cd. Cu was absorbed to the thallus at range of pH 2.1-6.5. Leaching velocity (k
1) and half life period(r)of metal ion from the thallus at pH 2.1 were as follows; Fe (k
1=2.0×10-2min
-1, τ=34.3 min.), Mn (k
1=15.6×10
-2 min
-1, τ=4.5 min.) and Zn (k
1=4.2×10
-2min
-1, τ=16.6 min.). The other hand, absorption velocity (k
1) and half life period(τ) of metal ion to the thallus at pH 3 .9 were as follows; Fe (k
1= -5.3×10
-2min
-1, τ=13.0 min.), Mn (k1= -15.7×10-2min-1, τ=4.1 min.), Zn (k
1= - 9.6×10
-2min
-1, τ=7.3 min.) and Cu (k
1= -8 .3× 10
-2min
-1, τ=8.4 min.). Leaching rate of K
+, Mg
+2 and Ca
2+ from the thallus and absorption rate of NH
4+ and N03- to the thallus were increased in the presence of heavy metal ions.
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