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Nitrogen deposition and forest nitrogen cycling along an urban–rural transect in southern China
219
Citations
74
References
2010
Year
BiogeochemistryEngineeringPlant UptakeTerrestrial EcosystemNitrogen DepositionForestryPlant N UptakeBiogeochemical CycleNutrient CycleTerrestrial Ecosystem ProductivitySoil Biogeochemical CyclingForest EcosystemsLand DegradationForest SoilEarth ScienceUrban–rural TransectForest Nitrogen Cycling
Abstract There is increasing concern over the impact of atmospheric nitrogen (N) deposition on forest ecosystems in the tropical and subtropical areas. In this study, we quantified atmospheric N deposition and revealed current plant and soil N status in 14 forests along a 150 km urban to rural transect in southern China, with an emphasis on examining whether foliar δ 15 N can be used as an indicator of N saturation. Bulk deposition ranged from 16.2 to 38.2 kg N ha −1 yr −1 , while the throughfall covered a larger range of 11.7–65.1 kg N ha −1 yr −1 . Foliar N concentration, NO 3 − leaching to stream, and soil NO 3 − concentration were low and NO 3 − production was negligible in some rural forests, indicating that primary production in these forests may be limited by N supply. But all these N variables were enhanced in suburban and urban forests. Across the study transect, throughfall N input was correlated positively with soil nitrification and NO 3 − leaching to stream, and negatively with pH values in soil and stream water. Foliar δ 15 N was between −6.6‰ and 0.7‰, and was negatively correlated with soil NO 3 − concentration and NO 3 − leaching to stream across the entire transect, demonstrating that an increased N supply does not necessarily increase forest δ 15 N values. We proposed several potential mechanism that could contribute to the δ 15 N pattern, including (1) increased plant uptake of 15 N‐depleted soil NO 3 − , (2) foliage uptake of 15 N‐depleted NH 4 + , (3) increased utilization of soil inorganic N relative to dissolved organic N, and (4) increased fractionation during plant N uptake under higher soil N availability.
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