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采用生命周期评价方法,对排水后的温带农业泥炭地上轮作的一年生作物与在沼泽地栽培中种植的黄花茅的温室气体排放进行比较。

Comparison of GHG emissions from annual crops in rotation on drained temperate agricultural peatland with production of reed canary grass in paludiculture using an LCA approach.

作者信息

Thers Henrik, Knudsen Marie Trydeman, Lærke Poul Erik

机构信息

Department of Agroecology, University of Aarhus, Blichers allé 20, DK-8830, Tjele, Denmark.

出版信息

Heliyon. 2023 Jun 15;9(6):e17320. doi: 10.1016/j.heliyon.2023.e17320. eCollection 2023 Jun.

Abstract

Drained peat soils contribute significantly to global human-caused CO emissions and reducing peat degradation via rewetting is high on the political agenda. Ceasing agricultural activities on rewetted soils might lead to land owner resistance and high societal expenses to compensate farmers. Continued biomass production adapted for wet conditions on peat soils potentially minimizes these costs and helps supplying the growing demand for e.g. materials, fuels and feed. Here we used a life cycle assessment approach (cradle to farm gate) to investigate the greenhouse gas (GHG) emissions related to three cases by applying IPCC (Intergovernmental Panel on Climate Change) emission factors and specific site conditions at a bog and a fen site that represent widely distributed temperate peat soils. Besides soil emissions, upstream emissions from input, operational emissions and emission related to rewetting construction work were included. The analyzed systems were deeply drained cash cropping on agricultural bog (potatoes ( L.), spring barley ( L.) and oat ( L.), permanent Reed canary grass (RCG) ( L.) production on non-drained bog and permanent RCG production on shallow-drained fen. The annual mean water table depths (WTD) were -70, -38 (estimated) and -13 cm, respectively. Results showed estimated GHG emissions of 40.5, 26.1 and 20.6 Mg COeq ha, respectively, corresponding to a 35% GHG reduction for the non-drained bog case as compared to the drained bog case, despite that the obtained WTD due to ceased drainage did not adhere to the IPCC rewetting threshold of -30 cm. Emissions related to crop management represented 7, 14 and 19% of total emissions. In the RCG cultivation on fen case, the WTD were controlled primarily by the water table of the nearby stream and total GHG emissions were even lower as compared to the RCG production on the non-drained bog reflecting the difference in WTD. Rewetting projects need to include careful knowledge of the specific peat area to foresee the actual reduction potential.

摘要

排水后的泥炭土对全球人为造成的二氧化碳排放有重大贡献,通过重新湿润来减少泥炭退化是一项重要的政治议程。在重新湿润的土地上停止农业活动可能会导致土地所有者的抵制,并需要高昂的社会成本来补偿农民。在泥炭土上继续开展适应湿润条件的生物质生产,有可能将这些成本降至最低,并有助于满足对材料、燃料和饲料等不断增长的需求。在此,我们采用生命周期评估方法(从摇篮到农场大门),通过应用政府间气候变化专门委员会(IPCC)的排放因子以及代表广泛分布的温带泥炭土的一个沼泽地和一个湿地的特定场地条件,来调查与三种情况相关的温室气体(GHG)排放。除了土壤排放外,还包括投入的上游排放、运营排放以及与重新湿润建设工作相关的排放。所分析的系统包括在农业沼泽地上深度排水种植经济作物(马铃薯(茄属)、春大麦(大麦属)和燕麦(燕麦属))、在未排水的沼泽地上永久性种植虉草(虉草属)以及在浅排水的湿地上永久性种植虉草。年平均地下水位深度(WTD)分别为 -70厘米、-38厘米(估计值)和 -13厘米。结果显示,估计的温室气体排放量分别为40.5、26.1和20.6 公吨二氧化碳当量/公顷,与排水沼泽地情况相比,未排水沼泽地情况的温室气体排放量减少了35%,尽管由于停止排水而获得的地下水位深度未达到IPCC重新湿润阈值 -30厘米。与作物管理相关的排放在总排放量中占7%、14%和19%。在湿地种植虉草的情况下,地下水位主要由附近溪流的水位控制,与未排水沼泽地种植虉草相比,总温室气体排放量甚至更低,这反映了地下水位的差异。重新湿润项目需要仔细了解特定泥炭区域的情况,以预见实际的减排潜力。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ea34/10333457/524f47fadbdb/gr1.jpg

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