The input-output balance of nitrogen was studied in a catchment area (4.28 km
2) at Mt. Awaga (elevation at the summit: 962 m a.s.l.) in the town of Aogaki, Hyogo Prefecture, Japan. Precipitation (collected using a wet-only sampler) and cloud water, as well as gas and aerosol (HNO
3(g), NH
3(g), NO
3-(p), and NH
4+(p) in ambient air), were considered as agents providing input to the catchment area, while stream water was considered as an agent carrying output from the catchment area. The input amounts of nitrogen by precipitation, cloud water, HNO
3(g), NH
3(g), NO
3-(p), and NH
4+(p) in ambient air were approximately 1400, 6700, 230, 160, 27, and 290 kgN, respectively, during the 7-month survey period (May - November, 1999), equivalent to 4.5, 30.2, 1.3, 0.90, 0.15, and 1.6 kgN/ha/year, respectively. However, the output amount of nitrogen by the stream water was approximately 2600 kgN for the period from April 21, 1999, to April 22, 2000, equivalent to 6.1 kgN/ha/year. The input (38.7 kgN/ha/year) was approximately 6.3 times greater than the output (6.1 kgN/ha/year). The input amount of nitrogen through nitrate was approximately 3400 kgN / 7 months, equivalent to 15.0 kgN/ha/year, while that through ammoniacal nitrogen (NHx = NH
3(g) + NH
4+(p)) was approximately 5300 kgN / 7 months, equivalent to 23.7 kgN/ha/year. The input through ammoniacal nitrogen was 1.6 times greater than that through nitrate. The dry deposition through HNO
3(g) was 8.7 times larger than that through NO
3-(p), while the dry deposition through NH
3(g) was approximately two-thirds that through NH
4+(p).
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