When precipitation passes through forest canopies, some ion concentration may increase while others may decrease in the throughfall. The enrichment phenomena result from the ion leaching from plant tissue and the removal of dry deposition, while decrease in ion concentration is due to ion absorption in-to plant tissue. This study was carried out to make clear how chemistry of the simulated rain water solution was changed when epiphytic lichens and tree leaves were submerged at varing acidity and time. The obtained result was as follows; (1) Lichens leached K
+(27.2±3.4μeq/g), Mg
2+(7.1±1.01μeq/g) and Ca
2+(18.4±5.0μeq/g) to the solution, absorbed NH
4+(6.3±2.6μeq/g) and NO
3(3.0±0.3μeq/g) from the solution. (2) Leaching of Ca
2+ and Mg
2+ from the thallus increaed significantly with increasing H
+concentration of solution, while K+ was not so. (3) Absorption of NO3
- to the thallus increased with increasing H
+ concentration of simulated rain water, while that of NH4
+ decreased in reverse. (4) The linear relationship between leaching and absorption through plant tissue and time was observed with respect to K
+, Mg
2+, Ca
2+, NH4
+ and NO3
-, respectively. Though leaves of Cryptomeria japonica and Quercus serrata responded in manners similar to those of the lichens, the leaching amounts were about 1/2-1/9 those of the lichens, except for Quercus serrata which indicated the possibility of the leakage of K
+ due to damage of cuticle tissue.
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