Abstract
The Kamabuchi experimental watershed, which is located alongside the sea of Japan in the Tohoku district, northern
Japan, receives considerable amount of snowfall in winter. We reported the mean annual solute concentrations of the rainwater and streamwater obtained between 2000 and 2014 in a small, forested watershed of this experimental watershed. The area of this watershed was 3.06 ha, and the vegetation was a mixed forest of deciduous and evergreen species. The mean annual NO3− and SO42− concentrations in rainwater showed no trend. The mean annual dissolved inorganic nitrogen input through rainwater was 12.4 kg ha−1 yr−1, about 60% of which was in the form of NO3−-N. SO42− input was 63.0 kg ha−1 yr−1, and about two third of that was the non-sea salt SO42− input. Annual NO3−-N and SO42− input had a positive correlation with the annual precipitation, suggesting that the loads of these inputs were mostly dependent on the amount of precipitation rather than the concentrations. There was a fluctuation in the mean annual NO3− concentration in streamwater, but an obvious annual change was not recognized. A change was not observed in the mean annual SO42− concentrations in streamwater.