Trends of Future Emission Legislation and its Measurement Requirements

2004 ◽  
Author(s):  
Engeljehringer Kurt
MTZ worldwide ◽  
2009 ◽  
Vol 70 (3) ◽  
pp. 10-17
Author(s):  
Hans-Jürgen Brüne ◽  
Josef Honeder ◽  
Peter Raschl ◽  
Michael Schinnerl ◽  
Rüdiger Tangemann

Author(s):  
Michael Neitz ◽  
Franz-Josef Quadflieg ◽  
Ludger Ruhkamp ◽  
Christoph Steffens ◽  
Peter Wartmann

The paper is a contribution to the discussion about a suitable future engine architecture, which has to cope with two contrary demands: the high mechanical and thermal loads in the engine and the need for a cost efficient, light weight engine design. Based on combustion related requirements of future emission legislation and expected performance requirements, a possible scenario of engine types and displacements is described. Features of a proposed bottom and top end concept — such as liner and crankcase concept, cylinder head bolt pattern, cylinder head concept, and suitable materials — are discussed, with the target to define a solution especially capable of high cylinder peak pressures and cost efficient at the same time.


Author(s):  
Guohua Jing ◽  
Johannes W. Schwank ◽  
Alexander J Hill ◽  
Huawang Zhao ◽  
Lei Ma ◽  
...  

Future emission standards are becoming increasingly stringent. Around 50% of targeted tailpipe emissions are emitted during the cold-start period, mainly due to the ineffectiveness of catalytic converters in the after-treatment...


Atmosphere ◽  
2021 ◽  
Vol 12 (6) ◽  
pp. 707
Author(s):  
Petros Vasilakos ◽  
Yongtao Hu ◽  
Armistead Russell ◽  
Athanasios Nenes

Formation of aerosol from biogenic hydrocarbons relies heavily on anthropogenic emissions since they control the availability of species such as sulfate and nitrate, and through them, aerosol acidity (pH). To elucidate the role that acidity and emissions play in regulating Secondary Organic Aerosol (SOA), we utilize the 2013 Southern Oxidant and Aerosol Study (SOAS) dataset to enhance the extensive mechanism of isoprene epoxydiol (IEPOX)-mediated SOA formation implemented in the Community Multiscale Air Quality (CMAQ) model (Pye et al., 2013), which was then used to investigate the impact of potential future emission controls on IEPOX OA. We found that the Henry’s law coefficient for IEPOX was the most impactful parameter that controls aqueous isoprene OA products, and a value of 1.9 × 107 M atm−1 provides the best agreement with measurements. Non-volatile cations (NVCs) were found in higher-than-expected quantities in CMAQ and exerted a significant influence on IEPOX OA by reducing its production by as much as 30% when present. Consistent with previous literature, a strong correlation of isoprene OA with sulfate, and little correlation with acidity or liquid water content, was found. Future reductions in SO2 emissions are found to not affect this correlation and generally act to increase the sensitivity of IEPOX OA to sulfate, even in extreme cases.


Fuel ◽  
2021 ◽  
Vol 299 ◽  
pp. 120879
Author(s):  
Guofan Qu ◽  
Anren Yao ◽  
Chao Chen ◽  
Jiachao Ren ◽  
Chunde Yao
Keyword(s):  

2019 ◽  
Author(s):  
Ulrike Niemeier ◽  
Claudia Timmreck ◽  
Kirstin Krüger

Abstract. In 1963 a series of eruptions of Mt. Agung, Indonesia, resulted in the 3rd largest eruption of the 20th century and claimed about 1900 lives. Two eruptions of this series injected SO2 into the stratosphere, a requirement to get a long lasting stratospheric sulfate layer. The first eruption on March 17th injected 4.7 Tg SO2 into the stratosphere, the second eruption 2.3 Tg SO2 on May, 16th. In recent volcanic emission data sets these eruption phases are merged together to one large eruption phase for Mt. Agung in March 1963 with an injection rate of 7 Tg SO2. The injected sulfur forms a sulfate layer in the stratosphere. The evolution of sulfur is non-linear and depends on the injection rate and aerosol background conditions. We performed ensembles of two model experiments, one with a single and a second one with two eruptions. The two smaller eruptions result in a lower burden, smaller particles and 0.1 to 0.3 Wm−2 (10–20 %) lower radiative forcing in monthly mean global average compared to the individual eruption experiment. The differences are the consequence of slightly stronger meridional transport due to different seasons of the eruptions, lower injection height of the second eruption and the resulting different aerosol evolution. The differences between the two experiments are significant but smaller than the variance of the individual ensemble means. Overall, the evolution of the volcanic clouds is different in case of two eruptions than with a single eruption only. We conclude that there is no justification to use one eruption only and both climatic eruptions should be taken into account in future emission datasets.


2015 ◽  
Vol 17 ◽  
pp. 14-25 ◽  
Author(s):  
Laurence Stevens ◽  
Christa Sys ◽  
Thierry Vanelslander ◽  
Edwin van Hassel

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