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低地农业集水区地表水的间接一氧化二氮排放:对农业温室气体预算的重大贡献?

Indirect nitrous oxide emissions from surface water bodies in a lowland arable catchment: a significant contribution to agricultural greenhouse gas budgets?

机构信息

School of Environmental Sciences, University of East Anglia, Norwich Research Park, Norwich, NR4 7TJ, UK.

出版信息

Environ Sci Technol. 2012 Aug 7;46(15):8156-63. doi: 10.1021/es3012244. Epub 2012 Jul 25.

Abstract

In the UK agriculture is by far the largest source of nitrous oxide (N(2)O) emissions. Direct N(2)O emissions as a result of nitrogen (N) application to soils have been well documented in the UK, whereas indirect emissions produced in surface waters and groundwaters from leached N are much less understood with limited data to support IPCC emission factors. Indirect emissions were studied in surface waters in the Upper Thurne, a lowland drained arable catchment in eastern England. All surface waters were found to have dissolved N(2)O concentrations above that expected if in equilibrium with ambient concentrations, demonstrating all surface waters were acting as a source of N(2)O. The drainage channels represented 86% of the total indirect N(2)O flux, followed by wetland areas, 11%, and the river, 3%. The dense drainage network was found to have the highest dissolved N(2)O concentrations of all the water bodies studied with a combined N(2)O flux of 16 kg N(2)O-N per day in March 2007. Such indirect fluxes are comparable to direct fluxes per hectare and represent a significant proportion of the total N(2)O flux for this catchment. Separate emission factors were established for the three different surface water types within the same catchment, suggesting that the one emission factor used in the Intergovernmental Panel on Climate Change (IPCC) methodology for predicting all indirect N(2)O emissions is inappropriate.

摘要

在英国,农业是一氧化二氮(N2O)排放的最大来源。英国已经有大量文献记载了由于向土壤施氮而直接产生的 N2O 排放,而从淋滤氮产生的地表水和地下水中的间接排放则知之甚少,因为支持政府间气候变化专门委员会(IPCC)排放因子的相关数据有限。间接排放是在英格兰东部低地可耕地集水区上特恩河(Upper Thurne)的地表水进行研究的。所有地表水的溶解 N2O 浓度均高于与环境浓度平衡时的预期浓度,这表明所有地表水都成为了 N2O 的来源。排水渠占总间接 N2O 通量的 86%,其次是湿地,占 11%,河流占 3%。研究发现,密集的排水网络中所有水体的溶解 N2O 浓度最高,在 2007 年 3 月的一天中,其总 N2O 通量为 16 千克 N2O-N。这样的间接通量与每公顷的直接通量相当,占该集水区总 N2O 通量的很大一部分。在同一集水区内,对三种不同的地表水类型分别建立了单独的排放因子,这表明政府间气候变化专门委员会(IPCC)预测所有间接 N2O 排放的方法中使用的单一排放因子是不恰当的。

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