『Abstract
　Nitrogen compounds generated by anthropogenic combustion deposits in forest watersheds and induce nitrogen saturation of the area. Because excess nitrogen is derived from atmospheric deposition, this action is expected to uniformly affect a wide area of forest soils. Geographically, heterogeneous nitrate concentration of stream water within a small area has been attributed to the tree type, geological setting and tree cut. In this article, we hypothesized that the effect of the atmospheric nitrogen deposition in the forest watershed may vary within a small area, and that such variation is induced by the degree of air mass containing a high concentration of nitrogen deposition of combustion origin. We measured major ion concentrations, including nitrate, nitrite oxygen and nitrogen stable isotope of nitrate sampled at 24 water streams in the Chichibu region, which is 50-100 km from the Tokyo metropolitan area. The nitrate concentration showed a wide range (35.6-237 μmol L^-1) within 300 km², which was explained sufficiently by the air mass advection path and its contact with the mountain's surface. The nitrate concentration showed a significant positive correlation with chloride (r = 0.73; p＜0.001). As chloride originates outside of the Chichibu region, the positive correlation between two ions showed that the nitrate concentration of the stream water was affected by the nitrogen compound from the Tokyo Metropolitan area as a form of atmospheric deposition. Between the nitrate concentration and the stable isotope ratio of oxygen of nitrate, there was a positive correlation until nitrate concentration of 100 μmol L^-1. When the nitrate is over 100 μmol L^-1, δ¹⁸O shows a stable value of ca. 5.7‰. This indicates that the nitrification proceeds when the nitrate concentration was low to middle, but the reaction showed when the nitrate concentration became high. Oxygen stable isotope of nitrate along with a set of nitrate concentrations can be used as a good indicator of nitrogen saturation.

Keywords: Nitrogen saturation; Nitrate; Oxygen stable isotope of nitrate; Stream water; Atmospheric deposition』

1. Introduction
2. Methods
　2.1. Study area and sampling points
　2.2. Ion concentration and stable isotope ratio of the stream water
3. Results
4. Discussion
　4.1. The heterogeneous effect of atmospheric nitrogen deposition on the stream water
　4.2. Relationship between stages of nitrate saturation and δ¹⁸O and δ¹⁵N of nitrate in the stream water
5. Conclusions
Acknowledgments
References