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The European carbon balance. Part 2: croplands

机译:欧洲碳平衡。第2部分:农田

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We estimated the long-term carbon balance [net biome production (NBP)] of European (EU-25) croplands and its component fluxes, over the last two decades. Net primary production (NPP) estimates, from different data sources ranged between 490 and 846 gC m-2 yr-1, and mostly reflect uncertainties in allocation, and in cropland area when using yield statistics. Inventories of soil C change over arable lands may be the most reliable source of information on NBP, but inventories lack full and harmonized coverage of EU-25. From a compilation of inventories we infer a mean loss of soil C amounting to 17 g m-2 yr-1. In addition, three process-based models, driven by historical climate and evolving agricultural technology, estimate a small sink of 15 g C m-2 yr-1 or a small source of 7.6 g C m-2 yr-1. Neither the soil C inventory data, nor the process model results support the previous European-scale NBP estimate by Janssens and colleagues of a large soil C loss of 90 +/- 50 gC m-2 yr-1. Discrepancy between measured and modeled NBP is caused by erosion which is not inventoried, and the burning of harvest residues which is not modeled. When correcting the inventory NBP for the erosion flux, and the modeled NBP for agricultural fire losses, the discrepancy is reduced, and cropland NBP ranges between -8.3 +/- 13 and -13 +/- 33 g C m-2 yr-1 from the mean of the models and inventories, respectively. The mean nitrous oxide (N2O) flux estimates ranges between 32 and 37 g C Eq m-2 yr-1, which nearly doubles the CO2 losses. European croplands act as small CH4 sink of 3.3 g C Eq m-2 yr-1. Considering ecosystem CO2, N2O and CH4 fluxes provides for the net greenhouse gas balance a net source of 42-47 g C Eq m-2 yr-1. Intensifying agriculture in Eastern Europe to the same level Western Europe amounts is expected to result in a near doubling of the N2O emissions in Eastern Europe. N2O emissions will then become the main source of concern for the impact of European agriculture on climate.
机译:我们估算了过去20年中欧洲(EU-25)农田及其组成通量的长期碳平衡[净生物群落生产(NBP)]。来自不同数据源的净初级生产(NPP)估计值介于490至846 gC m-2 yr-1之间,并且在使用产量统计数据时,大多数数据反映了分配和耕地面积的不确定性。耕地上土壤碳变化的清单可能是有关NBP的最可靠信息来源,但是清单缺乏对EU-25的完整统一的报道。从清单汇编中,我们推断出土壤碳的平均损失量为17 g m-2 yr-1。此外,在历史气候和不断发展的农业技术的驱动下,三种基于过程的模型估算出一个小的汇源为15 g C m-2 yr-1或一个小来源为7.6 g C m-2 yr-1。土壤C的库存数据或过程模型结果均不支持Janssens及其同事先前在欧洲范围进行的NBP估算,即90 +/- 50 gC m-2 yr-1的大量土壤C损失。测量和建模的NBP之间的差异是由未盘点的侵蚀和未建模的收获残留物燃烧引起的。当校正侵蚀通量的库存NBP和农业火灾损失的模型NBP时,差异减小,农田NBP介于-8.3 +/- 13和-13 +/- 33 g C m-2 yr-1之间分别来自模型和库存的均值。一氧化二氮(N2O)的平均通量估计值介于32至37 g C Eq m-2 yr-1之间,几乎使CO2损失增加了一倍。欧洲农田作为CH4 m-2 yr-1 Eq的小型CH4汇。考虑到生态系统的CO2,N2O和CH4通量,为温室气体净平衡提供了42-47 g C Eq m-2 yr-1的净源。东欧的农业集约化程度将达到西欧的水平,这将导致东欧的N2O排放量增加近一倍。然后,N2O排放将成为关注欧洲农业对气候影响的主要来源。

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