Thermal hazards of benzaldehyde oxime: Based on decomposition products and kinetics analysis by Adiabatic calorimeter

Author(s):  
Xiao-Qiao Zhao ◽  
Wen-Qian Wu ◽  
Hua-bo Li ◽  
Zi-Chao Guo ◽  
Wang-Hua Chen ◽  
...  
2014 ◽  
Vol 592-594 ◽  
pp. 2557-2560
Author(s):  
Velayuthan Sreekantan Smitha ◽  
Mahadevan Surianarayanan ◽  
Hariharan Seshadri ◽  
Nyaya Valiveti Lakshman ◽  
Asit Baran Mandal

The exothermic behavior of Tributyl Phosphate (TBP) with nitric acid at elevated temperatures is a serious cause of concern in nuclear industry as well as in various other industries where it is the principal extractant. In this study, the comparative study of thermal hazard of TBP and one of its major decomposition products, Dibutyl phosphate, (DBP) has been investigated under adiabatic conditions. Parameters such as comparative self-heat rate and pressure rise were deduced using world’s benchmark adiabatic calorimeter, Accelerating Rate Calorimeter (ARC). FTIR spectrum of the products obtained after ARC experiments pertaining to TBP and DBP are compared.


1989 ◽  
Vol 4 ◽  
pp. 244-248 ◽  
Author(s):  
Donald L. Wolberg

The minerals pyrite and marcasite (broadly termed pyritic minerals) are iron sulfides that are common if not ubiquitous in sedimentary rocks, especially in association with organic materials (Berner, 1970). In most marine sedimentary associations, pyrite and marcasite are associated with organic sediments rich in dissolved sulfate and iron minerals. Because of the rapid consumption of sulfate in freshwater environments, however, pyrite formation is more restricted in nonmarine sediments (Berner, 1983). The origin of the sulfur in nonmarine environments must lie within pre-existing rocks or volcanic detritus; a relatively small, but significant contribution may derive from plant and animal decomposition products.


CIM Journal ◽  
2016 ◽  
Vol 7 (1) ◽  
pp. 43-51 ◽  
Author(s):  
A. A. Baba ◽  
L. Ibrahim ◽  
R. B. Bale ◽  
A. G. F. Alabi ◽  
F. A. Adekola ◽  
...  

2019 ◽  
Vol 70 (8) ◽  
pp. 3085-3088
Author(s):  
Carmen Eugenia Stavarache ◽  
Yasuaki Maeda ◽  
Mircea Vinatoru

Neat nitrobenzene was continuously irradiated at two ultrasonic frequencies: 40 and 200 kHz, under air and argon atmosphere, respectively. Samples taken at intervals of 1, 5, 10 and 24 h were analyzed by GC-MS and decomposition products were identified. Possible reaction mechanisms are discussed. Presence of air as dissolved gas leads to oxygenated compounds such as 1,4-benzoquinone, 2,4-dinitrophenol, m-dinitrobenzene while argon inhibits the decomposition of nitrobenzene, especially at sonication times under 5 h. Based on the nature of the compounds identified we advanced a mechanism, involving a divergent splitting of unstable radical cation of NB in air and argon respectively. Thus, under air, the phenyl cation formation is preferred leading to 1,4-benzoquinone nitro-biphenyls and dinitrobenzene, while under argon, the phenyl radical formation seems to be favored, leading to phenol and diphenyl ether. The oxygenated compounds detected under argon clearly are a consequence of the nitro group splitting.


1996 ◽  
Vol 34 (9) ◽  
pp. 157-164 ◽  
Author(s):  
Kim C.-H. ◽  
M. Hosomi ◽  
A. Murakami ◽  
M. Okada

Effects of clay on fouling due to organic substances and clay were evaluated by model fouling materials and kaolin. Model fouling materials selected were protein, polysaccharide, fulvic acid, humic acid and algogenic matter (EOM:ectracellular organic matter, microbial decomposition products) and kaolin was selected as the clay material. Polysulfone membrane (MWCO(Molecular Weight Cut-Off) 10,000, 50,000 and 200,000) was used as an ultrafiltration membrane. In particular, the flux measurement of solutions containing algogenic matter used an ultrafiltration membrane of MWCO 50,000. The flux of protein and polysaccharide with coexistence of kaolin increased in the case of the ratio of MW/MWCO being greater than one, but did not increase in the case of the MW/MWCO ratio being below one. In contrast, the flux of fulvic acid and humic acid with coextence of kaolin decreased regardless of the ratio of MW/MWCO. The addition of dispersion agent and coagulant in the organic substances and kaolin mixture solution changed the size distribution of kaolin, and resulted in a change of the flux. EOM and microbial decomposition products decreased with the increase of the fraction of organic matter having molecular weight more than MWCO of membrane. The flux of the algogenic organic matter with coexistence of kaolin decreased with the increase of the amount of kaolin. It was suggested that the decline of the flux with coexistence of kaolin was due to the change of the resistance of the kaolin cake layer corresponding to the change in kaolin size distribution with charge.


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