十年期二氧化碳升高条件下的土壤有机碳:碳库规模不变,但稳定性降低

Fanbo Song , Xue Han , Meng Yuan , Yingchun Li , Ning Hu , Awais Shakoor , Adnan Mustafa , Yidong Wang
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引用次数: 0

摘要

大气二氧化碳浓度升高条件下土壤有机碳(SOC)的动态变化已被广泛报道,但其中主动组分和被动组分的行为仍未得到充分探讨。在此,我们利用在华北平原耕地上进行的为期 10 年的自由空气二氧化碳富集实验(550 ± 17 ppm)中的三对 SOC 活性组分和被动组分对这一问题进行了研究。我们发现,十年的二氧化碳升高增加了根系生物量、根系渗出率和微生物生物量,但对 SOC 池的大小影响不大。由于根系C输入的增加,二氧化碳升高增加了易氧化有机碳(ROOC)和颗粒有机碳(POC),但可能由于碳输入引起的正向引物效应,它们的成对被动组分减少了。我们的研究结果表明,在二氧化碳升高的条件下,SOC 池的稳定性降低。这对更好地预测 SOC 对未来气候变化的反馈意义重大。
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Soil organic carbon under decadal elevated CO2: Pool size unchanged but stability reduced

Soil organic carbon (SOC) dynamics under elevated atmospheric CO2 concentration has been widely reported, however, in which the behaviors of active and passive fractions remain inadequately explored. Here we studied this issue using three pairs of active and passive fractions of SOC under a 10-year free-air CO2 enrichment experiment (550 ​± ​17 ​ppm) in a cropland in the North China Plain. We found that decadal elevated CO2 increased the root biomass, root exudation rate and microbial biomass, but had little effects on SOC pool size. Elevated CO2 increased the readily oxidizable organic carbon (ROOC) and particulate organic carbon (POC) due to the increments of root C input, but decreased their paired passive fractions possibly because of the carbon input-induced positive priming effect. Our results indicate the reduced stability of SOC pool under elevated CO2. This is significant for better predicting SOC feedback to future climate change.

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