Fates of atmospheric deposited nitrogen in an Asian tropical primary forest

FOREST ECOLOGY AND MANAGEMENT

卷:411

Article

Wang, Ang^1,6,7  Zhu, Weixing^1,3  Gundersen, Per⁴  Phillips, Oliver L.⁵  Chen, Dexiang²  Fang, Yunting^1,6 

[1] Chinese Acad Sci, Inst Appl Ecol, CAS Key Lab Forest Ecol & Management, Shenyang 110164, Liaoning, Peoples R China

[2] Chinese Acad Forestry, Res Inst Trop Forestry, Guangzhou 510520, Guangdong, Peoples R China

[3] SUNY Binghamton, Dept Biol Sci, Binghamton, NY 13902 USA

[4] Univ Copenhagen, Dept Geosci & Nat Resource Management, DK-1958 Frederiksberg C, Denmark

[5] Univ Leeds, Sch Geog, Leeds LS2 9JT, W Yorkshire, England

[6] Qingyuan Forest CERN, Shenyang 110016, Liaoning, Peoples R China

[7] Univ Chinese Acad Sci, Coll Resources & Environm, Beijing 100049, Peoples R China

关键词: N-15 tracer;    Nitrogen deposition;    Nitrogen retention;    Plant uptake;    Carbon sequestration;    Total ecosystem recovery;   

DOI  :  10.1016/j.foreco.2018.01.029

来源: Elsevier

【 摘 要 】

The impacts of increasing nitrogen (N) deposition on forest ecosystems, including on carbon (C) sequestration, largely depend on the extent to which forests are N-limited and so whether and where deposited N is retained within the ecosystem. The N-15 tracer method can provide excellent insight into the ecosystem fates of N, but while it has been extensively used in temperate forests it has yet to be sufficiently employed in tropical forests, which are often thought not to be N-limited. Here, we used stable isotope (NH4+)-N-15 and (NO3-)-N-15 tracers applied as solutions to the forest floor to examine the fates of different forms of N in a tropical montane primary forest with low background atmospheric N deposition (6 kg N ha(-1) yr(-1)) in China. We found that a substantial amount of 15N was assimilated by plants over time and significantly more N-15 was recovered following (NO3-)-N-15 addition than following (NH4+)-N-15 addition: 7% and 16% of N-15 were recovered three months after the respective (NH4+)-N-15 and (NO3-)-N-15 tracer additions and 11% and 29% respectively after one year. In contrast to plants, the organic layer was only an important short-term sink for deposited N: while 21% and 12% of the N-15 from (NH4+)-N-15 and (NO3-)-N-15 additions were accumulated in the organic layer after three months, more than half of the retained N-15 was lost after one year. Mineral soil was the largest sink for deposited N, and the N-15 retained in soil was relatively stable over time for both N forms, with 39% and 32% of the initial N-15 input recovered after one year for (NH4+)-N-15 and (NO3-)-N-15 tracer additions, respectively. Overall, the total ecosystem N-15 recovery one year after the (NH4+)-N-15 and (NO3-)-N-15 tracer additions was large (60% and 66% respectively), and not significantly different from total recovery after three months, suggesting that a large proportion of deposited N could be retained in the longer term. Based on the measured fate of N-15 one year after labeling and the C:N ratios of different plant components, this tropical forest's carbon sequestration efficiency is calculated to be 17 kg C per kg N added, comparable to the values reported for temperate and boreal forests in Europe and North America and indicating substantial N limitation of this tropical forest. Our results suggest that anthropogenic N input in moderate levels may contribute to enhance C sequestration in some tropical forests, without significant long-term loss of N to the environment.

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