Agostini Francesco, Gregory Andrew S, Richter Goetz M
Department of Sustainable Soils and Grassland Systems, Rothamsted Research, Harpenden, Hertfordshire, AL5 2JQ UK.
Bioenergy Res. 2015;8(3):1057-1080. doi: 10.1007/s12155-014-9571-0. Epub 2015 Jan 15.
Soil organic carbon (SOC) changes associated with land conversion to energy crops are central to the debate on bioenergy and their potential carbon neutrality. Here, the experimental evidence on SOC under perennial energy crops (PECs) is synthesised to parameterise a whole systems model and to identify uncertainties and knowledge gaps determining PECs being a sink or source of greenhouse gas (GHG). For and willow ( spp.) and their analogues (switchgrass, poplar), we examine carbon (C) allocation to above- and belowground residue inputs, turnover rates and retention in the soil. A meta-analysis showed that studies on dry matter partitioning and C inputs to soils are plentiful, whilst data on turnover are rare and rely on few isotopic C tracer studies. Comprehensive studies on SOC dynamics and GHG emissions under PECs are limited and subsoil processes and C losses through leaching remain unknown. Data showed dynamic changes of gross C inputs and SOC stocks depending on stand age. C inputs and turnover can now be specifically parameterised in whole PEC system models, whilst dependencies on soil texture, moisture and temperature remain empirical. In conclusion, the annual net SOC storage change exceeds the minimum mitigation requirement (0.25 Mg C ha year) under herbaceous and woody perennials by far (1.14 to 1.88 and 0.63 to 0.72 Mg C ha year, respectively). However, long-term time series of field data are needed to verify sustainable SOC enrichment, as the physical and chemical stabilities of SOC pools remain uncertain, although they are essential in defining the sustainability of C sequestration (half-life >25 years).
与土地转变为能源作物相关的土壤有机碳(SOC)变化是生物能源及其潜在碳中性辩论的核心。在此,对多年生能源作物(PEC)下SOC的实验证据进行了综合,以参数化一个全系统模型,并确定决定PEC是温室气体(GHG)汇还是源的不确定性和知识空白。对于柳枝稷和柳树( spp.)及其类似物(柳枝稷、杨树),我们研究了碳(C)在地上和地下残茬输入、周转率以及在土壤中的保留情况。一项荟萃分析表明,关于干物质分配和土壤C输入的研究很多,而关于周转率的数据很少,且依赖于少数同位素C示踪研究。对PEC下SOC动态和GHG排放的全面研究有限,亚表层土壤过程以及通过淋溶造成的C损失仍然未知。数据显示,总C输入和SOC储量随林分年龄而动态变化。现在可以在整个PEC系统模型中对C输入和周转率进行具体参数化,而对土壤质地、湿度和温度的依赖性仍基于经验。总之,草本和木本多年生植物下的年度SOC净储量变化远远超过了最低减排要求(0.25 Mg C ha 年)(分别为1.14至1.88和0.63至0.72 Mg C ha 年)。然而,需要长期的田间数据序列来验证SOC的可持续富集,因为SOC库的物理和化学稳定性仍然不确定,尽管它们对于定义碳固存的可持续性(半衰期>25年)至关重要。