Seasonal fluctuation of concentration and flux of major inorganic ions in t
hroughfall, stem flow, snowpack and soil solution was investigated at a nat
ural cool temperate mixed forest in Hokkaido, northern Japan, in order to c
larify the effect of snowmelt on the solute dynamics in the forest soil in
snow-dominated region. Na+, Ca2+, Mg2+, Cl- and SO42- concentrations in soi
l solution showed a large fluctuation in the snowmelt period. The percentag
e of output of these elements from soil during the snowmelt period in the a
nnual output was as follows. Mg2+: 51%, Na+ and Cl-: 59 and 60%, SO42-: 65%
, Ca2+: 77%. Our results indicated that the snowmelt event was very importa
nt to quantify the annual elemental budgets in this region. Although the le
aching of base cat ion from the soil was larger than that of inputs and acc
umulation into the vegetation, annual decreasing rate of acid neutralizatio
n capacity (triangle ANC((s))) from the soil was mostly affected by the bas
e cation accumulation into the vegetation, related that the base cations we
athering accompanied with bicarbonate was slow due to the acidic and weathe
red soil in the studied site. It is suggested that the weakly acidic soil w
hich has tow triangle ANC((s)) in snow-dominated region will be relatively
sensitive to the future increase of acidic deposition.