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农业甲烷排放与潜在减排形式。

Agricultural methane emissions and the potential formitigation.

机构信息

Institute of Biological and Environmental Sciences, University of Aberdeen, 23 St Machar Drive, Aberdeen AB24 3UU, UK.

School of Geosciences and Edinburgh Centre for Carbon Innovation, University of Edinburgh, High School Yards, Edinburgh EH1 1LZ, UK.

出版信息

Philos Trans A Math Phys Eng Sci. 2021 Nov 15;379(2210):20200451. doi: 10.1098/rsta.2020.0451. Epub 2021 Sep 27.

DOI:10.1098/rsta.2020.0451
PMID:34565225
Abstract

Agriculture is the largest anthropogenic source of methane (CH), emitting 145 Tg CHy to the atmosphere in 2017. The main sources are enteric fermentation, manure management, rice cultivation and residue burning. There is significant potential to reduce CH from these sources, with bottom-up mitigation potentials of approximately 10.6, 10, 2 and 1 Tg CHy from rice management, enteric fermentation, manure management and residue burning. Other system-wide studies have assumed even higher potentials of 4.8-47.2 Tg CHy from reduced enteric fermentation, and 4-36 Tg CHy from improved rice management. Biogas (a methane-rich gas mixture generated from the anaerobic decomposition of organic matter and used for energy) also has the potential to reduce unabated CH emissions from animal manures and human waste. In addition to these supply side measures, interventions on the demand-side (shift to a plant-based diet and a reduction in total food loss and waste by 2050) would also significantly reduce methane emissions, perhaps in the order of greater than 50 Tg CHy. While there is a pressing need to reduce emissions of long-lived greenhouse gases (CO and NO) due to their persistence in the atmosphere, despite CH being a short-lived greenhouse gas, the urgency of reducing warming means we must reduce any GHG emissions we can as soon as possible. Because of this, mitigation actions should focus on reducing emissions of all the three main anthropogenic greenhouse gases, including CH. This article is part of a discussion meeting issue 'Rising methane: is warming feeding warming? (part1)'.

摘要

农业是甲烷(CH)的最大人为排放源,2017 年向大气中排放了 145 太克 CH。主要来源是反刍动物发酵、粪便管理、水稻种植和残茬燃烧。从这些来源减少 CH 排放的潜力很大,水稻管理、反刍动物发酵、粪便管理和残茬燃烧的减排潜力分别约为 10.6、10、2 和 1 太克 CH。其他全系统研究假设通过减少反刍动物发酵和改善水稻管理,分别有 4.8-47.2 太克 CH 和 4-36 太克 CH 的减排潜力。沼气(一种由有机物在厌氧分解过程中产生的富含甲烷的气体混合物,用于能源)也有可能减少动物粪便和人类废物未减排的 CH 排放。除了这些供应方面的措施外,需求方面的干预措施(转向植物性饮食和到 2050 年减少食物总损失和浪费)也将显著减少甲烷排放,或许超过 50 太克 CH。尽管 CH 是一种短寿命温室气体,但由于其在大气中存在的持久性,减少长期温室气体(CO 和 NO)排放的紧迫性迫在眉睫,尽管如此,由于减少变暖的紧迫性意味着我们必须尽快减少任何温室气体排放。因此,缓解行动应侧重于减少所有三种主要人为温室气体(包括 CH)的排放。本文是讨论会议议题“甲烷排放上升:变暖是否在助长变暖?(第一部分)”的一部分。

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