Nielsen C K, Elsgaard L, Jørgensen U, Lærke P E
Department of Agroecology, Faculty of Technology, Aarhus University, Blichers Alle 20, 8830 Tjele, Denmark; CBIO, Centre for Circular Bioeconomy, Aarhus University, Denmark.
Department of Agroecology, Faculty of Technology, Aarhus University, Blichers Alle 20, 8830 Tjele, Denmark.
Sci Total Environ. 2023 Oct 20;896:165083. doi: 10.1016/j.scitotenv.2023.165083. Epub 2023 Jun 29.
In view of climate considerations regarding the management of peatlands, there is a need to assess whether rewetting can mitigate greenhouse gas (GHG) emissions, and notably how site-specific soil-geochemistry will influence differences in emission magnitudes. However, there are inconsistent results regarding the correlation of soil properties with heterotrophic respiration (R) of carbon dioxide (CO), methane (CH), and nitrous oxide (NO) from bare peat. In this study, we determined 1) soil-, and site-specific geochemical components as drivers for emissions from R on five Danish fens and bogs, and 2) emission magnitudes under drained and rewetted conditions. For this, a mesocosm experiment was performed under equal exposure to climatic conditions and water table depths controlled to either -40 cm, or -5 cm. For the drained soils, we found that annual cumulative emissions, accounting for all three gases, were dominated by CO, contributing with, on average, 99 % to a varying global warming potential (GWP) of 12.2-16.9 t COeq ha yr. Rewetting lowered annual cumulative emissions from R by 3.2-5.1 t COeq ha yr for fens and bogs, respectively, despite a high variability of site-specific CH emissions, contributing with 0.3-3.4 t CO ha yr to the GWP. Overall, analyses using generalized additive models (GAM) showed that emission magnitudes were well explained by geochemical variables. Under drained conditions, significant soil-specific predictor variables for CO flux magnitudes were pH, phosphorus (P), and the soil substrate's relative water holding capacity (WHC). When rewetted, CO and CH emissions from R were affected by pH, WHC, as well as contents of P, total carbon and nitrogen. In conclusion, our results found the highest GHG reduction on fen peatlands, further highlighting that peat nutrient status and acidity, and the potential availability of alternative electron acceptors, might be used as proxies for prioritising peatland areas for GHG mitigation efforts by rewetting.
鉴于泥炭地管理方面的气候考量,有必要评估重新湿润是否能减少温室气体(GHG)排放,尤其是特定场地的土壤地球化学将如何影响排放规模的差异。然而,关于裸泥炭中土壤性质与二氧化碳(CO₂)、甲烷(CH₄)和一氧化二氮(N₂O)的异养呼吸(R)之间的相关性,研究结果并不一致。在本研究中,我们确定了:1)丹麦五个沼泽和泥炭地中,作为R排放驱动因素的土壤和特定场地地球化学成分;2)排水和重新湿润条件下的排放规模。为此,在相同气候条件和控制地下水位深度为-40厘米或-5厘米的条件下进行了中宇宙实验。对于排水后的土壤,我们发现,三种气体的年度累积排放量中,CO₂占主导,平均贡献率为99%,对12.2-16.9吨CO₂当量公顷·年的全球变暖潜能值(GWP)有不同贡献。重新湿润分别使沼泽和泥炭地的R年度累积排放量降低了3.2-5.1吨CO₂当量公顷·年。尽管特定场地的CH₄排放量变化很大,对GWP的贡献为0.3-3.4吨CO₂公顷·年。总体而言,使用广义相加模型(GAM)的分析表明,地球化学变量能够很好地解释排放规模。在排水条件下,CO₂通量规模的显著土壤特定预测变量是pH值、磷(P)和土壤基质的相对持水量(WHC)。重新湿润时,R的CO₂和CH₄排放受pH值、WHC以及P、总碳和氮含量的影响。总之,我们的研究结果发现,沼泽泥炭地的温室气体减排效果最佳,进一步凸显泥炭养分状况和酸度,以及替代电子受体的潜在可用性,可作为通过重新湿润来优先确定泥炭地温室气体减排区域的指标。