中国燃煤发电厂的素排放:演变,驱动力和未来趋势
Zhiqiang Fu1,2, Zehui Yao1,2, Junqi Yang1,2
1State Key Joint Laboratory of Environmental Simulation & Pollution Control, School of Environment, Beijing Normal University, Beijing 100875, China.
Environmental science & technology
|January 17, 2025
概括
煤电厂是大气中素的主要来源. 这项研究量化了中国的这些排放,发现它们将在2030年之前达到峰值,并随着气候政策的推进而下降.
科学领域:
- 大气化学 大气化学
- 环境科学 环境科学
- 气候变化研究 气候变化研究
背景情况:
- 大气中的素 (F,Cl,Br,I) 显著影响大气化学和气候.
- 燃煤发电厂 (CFPP) 是这些素的关键人为来源.
- 关于中国CFPP素排放的综合数据有限.
研究的目的:
- 制定一个详细的素排放清单从中国的CFPPs.
- 分析这些排放的时空变化,驱动因素和未来趋势.
- 根据气候和空气污染控制情景来预测排放轨迹.
主要方法:
- 利用多源数据和质量平衡方法来估计排放.
- 分析了时间 (2018-2022) 和空间排放模式.
- 基于气候目标和污染控制措施,模拟未来的排放趋势.
主要成果:
- 素排放量在2018-2022年间波动,其中2022年的总量为:F (6,875.7),Cl (24,872.4),Br (1,127.9) 和I (476.7).
- 排放集中在煤炭资源和高能耗地区.
- 煤炭消费量增加,而污染控制和技术改善了减少.
结论:
- 中国的CFPP素排放量预计将在2030年之前达到峰值,然后急剧下降,到2050年接近消除.
- 协同作用的空气污染物和碳控制技术提供了最大的减排潜力.
- 有效的政策实施对于减轻素影响至关重要.
相关概念视频
The Carbon Cycle
Carbon is the basis of all organic matter on Earth, and is recycled through the ecosystem in two primary processes: one in which carbon is exchanged among living organisms, and one in which carbon is cycled over long periods of time through fossilized organic remains, weathering of rocks, and volcanic activity. Human activities, including increased agricultural practices and the burning of fossil fuels, has greatly affected the balance of the natural carbon cycle.
Global Climate Change
Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
Hess's Law
There are two ways to determine the amount of heat involved in a chemical change: measure it experimentally, or calculate it from other experimentally determined enthalpy changes. Some reactions are difficult, if not impossible, to investigate and make accurate measurements for experimentally. And even when a reaction is not hard to perform or measure, it is convenient to be able to determine the heat involved in a reaction without having to perform an experiment.
Halogens
Group 17 elements, known as halogens, are nonmetals. At room temperature, fluorine and chlorine are gases, bromine is a liquid, and iodine a solid. Astatine is a highly unstable radioactive element, so currently, most of its properties are unknown due to its short half-life. Tennessine is a synthetic element also predicted to be in this group.
Radical Substitution: Halogenation of Alkanes and Alkyl Substituents
In the presence of heat or light, alkanes react with molecular halogens to form alkyl halides by a substitution reaction called radical halogenation. This reaction has three steps: initiation, propagation, and termination, as seen in the radical chlorination of methane to produce methyl chloride.
In the initiation step of the reaction, the chlorine molecule undergoes homolytic cleavage in the presence of light or heat, forming two highly reactive chlorine radicals. Propagation occurs in two...
In the initiation step of the reaction, the chlorine molecule undergoes homolytic cleavage in the presence of light or heat, forming two highly reactive chlorine radicals. Propagation occurs in two...
Radical Halogenation: Thermodynamics
The thermodynamic favorability of a reaction is determined by the change in Gibbs free energy (ΔG). ΔG has two components- enthalpy (ΔH) and entropy (ΔS). The entropy component is negligible for alkane halogenation because the number of reactants and product molecules are equal. In this case, the ΔG is governed only by the enthalpy component. The most crucial factor that determines ΔH is the strength of the bonds. ΔH can be determined by comparing the energy between bonds broken and bonds...


