Environmental Media Assessment Group-MD B243-01, National Center for Environmental Assessment, Office of Research and Development, U.S. EPA, Research Triangle Park, NC 27711, USA.
Ecol Lett. 2010 Jul;13(7):819-28. doi: 10.1111/j.1461-0248.2010.01482.x. Epub 2010 May 12.
Nitrogen (N) effects on ecosystem carbon (C) budgets are critical to understand as C sequestration is considered as a mechanism to offset anthropogenic CO(2) 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.
氮(N)对生态系统碳(C)预算的影响至关重要,因为碳封存被认为是抵消人为 CO2 排放的一种机制。地上 C 和 N 循环之间的相互作用比地下过程更为明显。通过综合多个陆地生态系统的数据,我们量化了氮添加对地下 C 循环的响应。我们发现,氮添加增加了地上凋落物的输入(增加 20%),但对细根没有影响。氮添加抑制了微生物活性,表现为微生物呼吸(减少 8%)和微生物生物量碳(减少 20%)减少。尽管氮添加没有改变土壤呼吸,但溶解有机碳浓度增加了 18%,这表明 C 淋溶损失可能会增加。氮添加增加了有机层的 C 含量(增加 17%),但对矿质土壤层没有影响。总的来说,我们的荟萃分析表明,氮添加将通过增加有机层的 C 含量来增加短期地下 C 储存。然而,由于矿质土壤 C 含量没有明显变化,长期碳固存的响应很难预测。