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

贯通 横断面 自行车 环境科学 浸出(土壤学) 土壤酸化 亚热带 硝化作用 氮气 沉积(地质) 土壤pH值 生态系统 土壤水分 水文学(农业) 农学 环境化学 生态学 林业 土壤科学 化学 地理 生物 地质学 古生物学 岩土工程 有机化学 沉积物
作者
Yunting Fang,Muneoki Yoh,Keisuke Koba,Weixing Zhu,Yu Takebayashi,Yihua Xiao,Chunyi Lei,Jiangming Mo,Wei Zhang,X. L. Lu
出处
期刊:Global Change Biology [Wiley]
卷期号:17 (2): 872-885 被引量:206
标识
DOI:10.1111/j.1365-2486.2010.02283.x
摘要

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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