A global perspective on belowground carbon dynamics under nitrogen enrichment

被引:677
作者
Liu, Lingli [1 ]
Greaver, Tara L. [1 ]
机构
[1] US EPA, Environm Media Assessment Grp, Natl Ctr Environm Assessment, Off Res & Dev, Res Triangle Pk, NC 27711 USA
关键词
Carbon sequestration; climate change; DOC; ecosystem C balance; fine root; litter; microbial activity; mineral soil; organic soil; soil respiration; DISSOLVED ORGANIC-CARBON; ATMOSPHERIC CO2; SOIL ACIDIFICATION; SUGAR MAPLE; PINE FOREST; DEPOSITION; METAANALYSIS; TEMPERATE; ADDITIONS; PLANT;
D O I
10.1111/j.1461-0248.2010.01482.x
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
P>Nitrogen (N) effects on ecosystem carbon (C) budgets are critical to understand as C sequestration is considered as a mechanism to offset anthropogenic CO2 emissions. Interactions between aboveground C and N cycling are more clearly characterized than belowground processes. Through synthesizing data from multiple terrestrial ecosystems, we quantified the responses of belowground C cycling under N addition. We found that N addition increased litter input from aboveground (+20%) but not from fine root. N addition inhibited microbial activity as indicated by a reduction in microbial respiration (-8%) and microbial biomass carbon (-20%). Although soil respiration was not altered by N addition, dissolved organic carbon concentration was increased by 18%, suggesting C leaching loss may increase. N addition increased the C content of the organic layer (+17%) but not the mineral soil layer. Overall, our meta-analysis indicates that N addition will increase short term belowground C storage by increasing C content of organic layer. However, it is difficult to predict the response of long term C sequestration since there is no significant change in mineral soil C content.
引用
收藏
页码:819 / 828
页数:10
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