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
相关论文
共 87 条
[1]   NITROGEN SUPPLY EFFECTS ON PRODUCTIVITY AND POTENTIAL LEAF-LITTER DECAY OF CAREX SPECIES FROM PEATLANDS DIFFERING IN NUTRIENT LIMITATION [J].
AERTS, R ;
VANLOGTESTIJN, R ;
VANSTAALDUINEN, M ;
TOET, S .
OECOLOGIA, 1995, 104 (04) :447-453
[2]   A review of nitrogen fertilizer and conservation tillage effects on soil organic carbon storage [J].
Alvarez, R .
SOIL USE AND MANAGEMENT, 2005, 21 (01) :38-52
[3]  
[Anonymous], ECOSYSTEMS
[4]  
[Anonymous], ORGANIC MATTER TURNO
[5]   Major contribution of roots to soil carbon storage inferred from maize cultivated soils [J].
Balesdent, J ;
Balabane, M .
SOIL BIOLOGY & BIOCHEMISTRY, 1996, 28 (09) :1261-1263
[6]   Nitrogen mineralization in density fractions of soil organic matter from maize and legume cropping systems [J].
Barrios, E ;
Buresh, RJ ;
Sprent, JI .
SOIL BIOLOGY & BIOCHEMISTRY, 1996, 28 (10-11) :1459-1465
[7]   Controls on nitrogen cycling in terrestrial ecosystems: A synthetic analysis of literature data [J].
Booth, MS ;
Stark, JM ;
Rastetter, E .
ECOLOGICAL MONOGRAPHS, 2005, 75 (02) :139-157
[8]  
Carreiro MM, 2000, ECOLOGY, V81, P2359, DOI 10.1890/0012-9658(2000)081[2359:MESELD]2.0.CO
[9]  
2
[10]  
Chapin FS., 2002, Principles of Terrestrial Ecosystem Ecology, P46