4.8 Article

Nitrogen deposition and forest nitrogen cycling along an urban-rural transect in southern China

Journal

GLOBAL CHANGE BIOLOGY
Volume 17, Issue 2, Pages 872-885

Publisher

WILEY
DOI: 10.1111/j.1365-2486.2010.02283.x

Keywords

nitrogen deposition; nitrogen isotope; nitrogen saturation; soil nitrogen availability; tropical and subtropical forests

Funding

  1. National Natural Science Foundation of China [40703030, 30725006]
  2. Provincial Natural Science Foundation of Guangdong [8351065005000001, 7006915]
  3. Pearl River Delta Forest Ecosystem Research Station, CAF of Japan Society for Promotion of Science (JSPS) [21310008, 19310019]
  4. Ministry of Education, Culture, Sports, Science and Technology, Japan
  5. JSPS [20-08421]
  6. [187801172]
  7. [20780113]
  8. Grants-in-Aid for Scientific Research [19310019] Funding Source: KAKEN

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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 delta 15N 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, NO3- leaching to stream, and soil NO3- concentration were low and NO3- 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 NO3- leaching to stream, and negatively with pH values in soil and stream water. Foliar delta 15N was between -6.6 parts per thousand and 0.7 parts per thousand, and was negatively correlated with soil NO3- concentration and NO3- leaching to stream across the entire transect, demonstrating that an increased N supply does not necessarily increase forest delta 15N values. We proposed several potential mechanism that could contribute to the delta 15N pattern, including (1) increased plant uptake of 15N-depleted soil NO3-, (2) foliage uptake of 15N-depleted NH4+, (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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