Impact of nitrogen cycling on stream water quality in a basin associated with forest, grassland, and animal husbandry, Hokkaido, Japan

The direct discharge of wastes from agricultural fields and livestock feedlots increases the concentration of nitrogen (N) in streams. This study was conducted to determine the impact of farm N budgets on stream water quality. In 1999–2000, we investigated an experimental livestock farm of 457 ha in the Kepau River watershed in Shizunai, Southern Hokkaido, Japan, where grasslands and maize fields account for 33% of the farm's total area. Annual N flow was calculated on the basis of the farm's land management records. Livestock was supplied with 15.2 t N yr⁻¹ from agricultural lands, which made the farm 81% self-sufficient. Livestock excreta produced 17.2 t N yr⁻¹, of which 4 t N yr⁻¹ was lost, probably by ammonia volatilization during decomposition. Apart from manure, the major N inputs were 9.1 t N yr⁻¹ of chemical fertilizers, 6.4 t N yr⁻¹ of atmospheric deposition, and 12.6 t N yr⁻¹ biological N fixation. The major outputs were uptake by forest vegetation of 11.0 t N yr⁻¹, denitrification of 1.5 t N yr⁻¹, and livestock feed production. Consequently, the annual surplus N on the whole farm was estimated to be 12.7 t N yr⁻¹, which corresponds to 28 kg N ha⁻¹ of agricultural land.The annual N load from the farm to the Kepau River was measured at 14.4 t N yr⁻¹. Ninety percent of this load, however, occurred during rainfall and spring snowmelt. Within one 2-week snowmelt period, 5.0 t N was discharged, which corresponds to 35% of the annual load. Although the average N concentration of stream water below the farm was 2.8 mg N L⁻¹, the maximum concentration recorded during the snowmelt season was 13.5 mg N L⁻¹. The N concentration of the stream water increased and the silica (Si) concentration decreased as the stream flow rate increased. Consequently, the molar ratio of Si/N frequently dropped below 2.7, the critical level for the occurrence of eutrophication. The large N load during rainfall and snowmelt could be ascribed to open ditches, which collect tile drainage and surface runoff from the fields, discharging it directly to the river, bypassing the forested riparian zone.