Long-term changes in the water quality of soil water and streamwater were monitored before and after cutting at the lower slope position in a small forested watershed composed of artificial stands of old aged Japanese cedar and cypress in the northern Kanto region in Japan. The NO
3− concentration in soil water directly reflected the N dynamics, i.e., the reduced nutrient uptake and accelerated nitrogen mineralization in the surface soil layer immediately after the cutting, and the increased nutrient uptake induced by regenerated trees several years after the practice. In contrast, the NO
3− concentration in streamwater maintained higher level than before cutting in the sixth year after the practice. The NO
3− concentrations in high and low discharge, which is dominated by direct flow and base flow, respectively, were calculated from the relationships between discharge rates and the NO
3− concentration in streamwater. The results suggested that the NO
3− distribution in soil affects the NO
3− concentration in streamwater. Changes in the NO
3− concentration in the subsoil were calculated using the HYDRUS-1D model, and these changes were consistent with previously measured seasonal and long-term changes in the NO
3− concentration in streamwater. This finding implies that NO
3− adsorption characteristics of the volcanic ash subsoil affects NO
3− leaching into streamwater. In order to clarify the effects of the aging of artificial forests, the method of cutting, and environmental changes on N dynamics in soil and streamwater, it is necessary to consider the NO
3− adsorption characteristics of volcanic ash soil.
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