Processing of natural and casing-head gases by the gas-phase oxidation

2021 ◽  
Vol 21 (4) ◽  
pp. 227-237
Author(s):  
V. S. Arutyunov ◽  
V. I. Savchenko ◽  
I. V. Sedov ◽  
A. V. Nikitin

The paper considers the growing importance of gas chemistry for the world economy and the related necessity of developing new, particularly noncatalytic technologies for the conversion of natural gas and other hydrocarbon gases into chemical products. The available and promising noncatalytic processes of their conversion into syngas as well as the direct methods for the synthesis of chemical products from methane, which is the main component of natural gas, are discussed.

1996 ◽  
Vol 65 (3) ◽  
pp. 197-224 ◽  
Author(s):  
Vladimir S Arutyunov ◽  
Valentin Ya Basevich ◽  
Vladimir I Vedeneev

2017 ◽  
Vol 348 ◽  
pp. 265-275 ◽  
Author(s):  
N. Alonso-Fagúndez ◽  
M. Ojeda ◽  
R. Mariscal ◽  
J.L.G. Fierro ◽  
M. López Granados

2011 ◽  
Vol 11 (21) ◽  
pp. 11055-11067 ◽  
Author(s):  
K. Salo ◽  
M. Hallquist ◽  
Å. M. Jonsson ◽  
H. Saathoff ◽  
K.-H. Naumann ◽  
...  

Abstract. The aim of this study was to investigate oxidation of SOA formed from ozonolysis of α-pinene and limonene by hydroxyl radicals. This paper focuses on changes of particle volatility, using a Volatility Tandem DMA (VTDMA) set-up, in order to explain and elucidate the mechanism behind atmospheric ageing of the organic aerosol. The experiments were conducted at the AIDA chamber facility of Karlsruhe Institute of Technology (KIT) in Karlsruhe and at the SAPHIR chamber of Forchungzentrum Jülich (FZJ) in Jülich. A fresh SOA was produced from ozonolysis of α-pinene or limonene and then aged by enhanced OH exposure. As an OH radical source in the AIDA-chamber the ozonolysis of tetramethylethylene (TME) was used while in the SAPHIR-chamber the OH was produced by natural light photochemistry. A general feature is that SOA produced from ozonolysis of α-pinene and limonene initially was rather volatile and becomes less volatile with time in the ozonolysis part of the experiment. Inducing OH chemistry or adding a new portion of precursors made the SOA more volatile due to addition of new semi-volatile material to the aged aerosol. The effect of OH chemistry was less pronounced in high concentration and low temperature experiments when lower relative amounts of semi-volatile material were available in the gas phase. Conclusions drawn from the changes in volatility were confirmed by comparison with the measured and modelled chemical composition of the aerosol phase. Three quantified products from the α-pinene oxidation; pinonic acid, pinic acid and methylbutanetricarboxylic acid (MBTCA) were used to probe the processes influencing aerosol volatility. A major conclusion from the work is that the OH induced ageing can be attributed to gas phase oxidation of products produced in the primary SOA formation process and that there was no indication on significant bulk or surface reactions. The presented results, thus, strongly emphasise the importance of gas phase oxidation of semi- or intermediate-volatile organic compounds (SVOC and IVOC) for atmospheric aerosol ageing.


1995 ◽  
Vol 34 (4) ◽  
pp. 1044-1059 ◽  
Author(s):  
Rune Lodeng ◽  
Odd A. Lindvaag ◽  
Paal Soraker ◽  
Per T. Roterud ◽  
Olav T. Onsager

2008 ◽  
Vol 112 (48) ◽  
pp. 19102-19112 ◽  
Author(s):  
K. Bhattacharyya ◽  
S. Varma ◽  
A. K. Tripathi ◽  
S. R. Bharadwaj ◽  
A. K. Tyagi

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