부산대학교 도서관

To evaluate nitrogen (N) saturation in xeric environments, we measured hydrologic N losses, soil N pools, and microbial processes, and developed an N-budget for a chaparral catchment (Sierra Nevada, California) exposed to atmospheric N inputs of approximately 8.5 kg N ha−1 y−1. Dual-isotopic techniques were used to trace the sources and processes controlling nitrate (NO3−) losses. The majority of N inputs occurred as ammonium. At the onset of the wet season (November to April), we observed elevated streamwater NO3− concentrations (up to 520 µmol l−1), concomitant with the period of highest gaseous N-loss (up to 500 ng N m−2 s−1) and suggesting N-saturation. Stream NO3− δ15N and δ18O and soil N measurements indicate that nitrification controlled NO3− losses and that less than 1% of the loss was of atmospheric origin. During the late wet season, stream NO3− concentrations decreased (to