Minor stimulation of soil carbon storage by nitrogen addition: A meta-analysis

被引:432
作者
Lu, Meng [1 ,2 ,3 ]
Zhou, Xuhui [1 ]
Luo, Yiqi [1 ,2 ]
Yang, Yuanhe [1 ]
Fang, Changming [2 ]
Chen, Jiakuan [2 ]
Li, Bo [2 ]
机构
[1] Univ Oklahoma, Dept Bot & Microbiol, Norman, OK 73019 USA
[2] Fudan Univ, Inst Biodivers Sci, Coastal Ecosyst Res Stn Yangtze River Estuary, Minist Educ,Key Lab Biodivers Sci & Ecol Engn, Shanghai 200433, Peoples R China
[3] Fudan Univ, Dept Environm Sci & Engn, Shanghai 200433, Peoples R China
基金
美国国家科学基金会;
关键词
Carbon sequestration; N addition; Aboveground C pool; Belowground C pool; Litter C pool; DOC; Microbial biomass C; ORGANIC-MATTER; ELEVATED CO2; TERRESTRIAL ECOSYSTEMS; COMMUNITY COMPOSITION; LITTER DECOMPOSITION; PRIMARY PRODUCTIVITY; MICROBIAL BIOMASS; FOREST ECOSYSTEMS; CYCLE FEEDBACKS; CLIMATE;
D O I
10.1016/j.agee.2010.12.010
中图分类号
S [农业科学];
学科分类号
09 ;
摘要
It is a well-established concept that nitrogen (N) limits plant growth and ecosystem production. However, whether N limits land carbon (C) sequestration - particularly in soil, the largest pool in the land - remains highly controversial. We conducted a meta-analysis to synthesize 257 studies published in the literature with 512 paired comparisons to quantify the changes of ecosystem C processes in response to N addition. Our results show that N addition significantly increased aboveground, belowground, and litter C pools by 35.7, 23.0, and 20.9%, respectively, across all the studies. Despite the substantial increases in C inputs from vegetation to soil system, N addition resulted in no significant change in C storage of both organic horizon and mineral soil in forests and grasslands, but a significant 3.5% increase in agricultural ecosystems, largely due to less contribution from aboveground production and increases in DOC and soil respiration. Thus, N stimulation of C storage primarily occurred in plant pools but little in soil pools. Moreover, N-induced change in soil C storage was positively related to changes in belowground production but not to those in aboveground growth. Our global synthesis also suggests that earth system models need to treat soil C inputs from aboveground and belowground sources differentially for soil C sequestration in response to N deposition and fertilization. (C) 2010 Elsevier B.V. All rights reserved.
引用
收藏
页码:234 / 244
页数:11
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