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

被引:179
|
作者
Fang, Yunting [1 ,2 ]
Yoh, Muneoki [2 ]
Koba, Keisuke [2 ]
Zhu, Weixing [3 ]
Takebayashi, Yu [2 ]
Xiao, Yihua [4 ]
Lei, Chunyi [5 ]
Mo, Jiangming [1 ]
Zhang, Wei [1 ]
Lu, Xiankai [1 ]
机构
[1] Chinese Acad Sci, Key Lab Vegetat Restorat & Management Degraded Ec, S China Bot Garden, Guangzhou 510650, Guangdong, Peoples R China
[2] Tokyo Univ Agr & Technol, Dept Environm & Nat Resource Sci, Fuchu, Tokyo 1838509, Japan
[3] SUNY Binghamton, Dept Biol Sci, Binghamton, NY 13902 USA
[4] CAF, Res Inst Trop Forestry, Guangzhou 510520, Guangdong, Peoples R China
[5] Heishiding Nat Reserve, Zhaoqing 526536, Guangdong, Peoples R China
基金
中国国家自然科学基金;
关键词
nitrogen deposition; nitrogen isotope; nitrogen saturation; soil nitrogen availability; tropical and subtropical forests; N-15; NATURAL-ABUNDANCE; PLANT NITROGEN; ISOTOPIC COMPOSITION; MYCORRHIZAL FUNGI; TROPICAL FOREST; GLOBAL PATTERNS; SOIL-NITROGEN; FOLIAR N-15; LAND-USE; NITRATE;
D O I
10.1111/j.1365-2486.2010.02283.x
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
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.
引用
收藏
页码:872 / 885
页数:14
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