Institute of Integrative Biology, ETH Zurich, Univeritätstrasse 16, 8092, Zurich, Switzerland.
Department of Ecology, Evolution, and Behavior, University of Minnesota, 1479 Gortner Ave. St, Paul, MN, 55108, USA.
Ecol Lett. 2019 Jun;22(6):936-945. doi: 10.1111/ele.13258. Epub 2019 Mar 18.
Soil stores approximately twice as much carbon as the atmosphere and fluctuations in the size of the soil carbon pool directly influence climate conditions. We used the Nutrient Network global change experiment to examine how anthropogenic nutrient enrichment might influence grassland soil carbon storage at a global scale. In isolation, enrichment of nitrogen and phosphorous had minimal impacts on soil carbon storage. However, when these nutrients were added in combination with potassium and micronutrients, soil carbon stocks changed considerably, with an average increase of 0.04 KgCm year (standard deviation 0.18 KgCm year ). These effects did not correlate with changes in primary productivity, suggesting that soil carbon decomposition may have been restricted. Although nutrient enrichment caused soil carbon gains most dry, sandy regions, considerable absolute losses of soil carbon may occur in high-latitude regions that store the majority of the world's soil carbon. These mechanistic insights into the sensitivity of grassland carbon stocks to nutrient enrichment can facilitate biochemical modelling efforts to project carbon cycling under future climate scenarios.
土壤储存的碳大约是大气的两倍,土壤碳库的大小波动直接影响气候条件。我们利用营养网络全球变化实验来研究人为营养富集如何在全球范围内影响草原土壤碳储存。氮磷单独富集对土壤碳储存的影响很小。然而,当这些养分与钾和微量元素一起添加时,土壤碳储量发生了显著变化,平均增加了 0.04 KgCm 年(标准偏差 0.18 KgCm 年)。这些影响与初级生产力的变化无关,表明土壤碳分解可能受到限制。虽然养分富集使大多数干燥、沙质地区的土壤碳增加,但在储存了世界上大部分土壤碳的高纬度地区,可能会发生相当大的土壤碳绝对损失。这些关于草原碳储量对养分富集敏感性的机制见解可以促进生物化学模型的努力,以预测未来气候情景下的碳循环。