The isotopic signatures of nitrate in mountain streams indicate the dominant processes associated with nitrogen (N) export from a forested watershed. The nitrate concentrations sampled at 40 mountain streams around Mt. Tsukuba, and the oxygen (δ
18O) and nitrogen isotope ratios (δ
15N) of that nitrate, showed that the geophysical and geological characteristics of the basin significantly affected the N export processes in the forest watershed. From this study we discovered the following: 1) At seven sites, the isotopic signal (i. e., high δ
18O) indicated that bulk precipitation was one of the primary nitrate sources in winter. Using two source mixing models, high δ
18O levels in winter were only found in streams with low nitrate concentrations although precipitation substantially inflow. 2) Significant correlations were found between the geophysical/geological parameters of the basin and the nitrate concentration/isotope ratio parameters. These could mostly be explained by the increased nitrate production and consumption activity during the summer and the increase in the relative contribution of nitrate derived from bulk precipitation in winter.
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