Volatile evolution during thermal treatment of oily sludge from a petroleum refinery wastewater treatment Plant: TGA-MS, Py-GC(EGA)/MS and kinetics study

被引:30
作者
Fan, Nie [1 ,2 ]
Yuguo, Li [3 ]
Kun, Tong [1 ,2 ]
Baichun, Wu [1 ,2 ]
Mingdong, Zhang [1 ,2 ]
Wen, Ren [1 ,2 ]
Shuixiang, Xie [1 ,2 ]
Xingchun, Li [1 ,2 ]
机构
[1] State Key Lab Petr Pollut Control, Beijing, Peoples R China
[2] CNPC Res Inst Safety & Environm Technol Co Ltd, Beijing, Peoples R China
[3] China Univ Petr, Beijing, Peoples R China
关键词
Oil sludge; Thermal treatment; Pyrolysis; Volatile evolution; Evolved gas analysis; SEWAGE-SLUDGE; PYROLYSIS CHARACTERISTICS; CATALYTIC PYROLYSIS; DECOMPOSITION;
D O I
10.1016/j.fuel.2020.118332
中图分类号
TE [石油、天然气工业]; TK [能源与动力工程];
学科分类号
0807 ; 0820 ;
摘要
The volatile evolution during thermal treatment of an oily sludge derived from petroleum refinery wastewater treatment plant was investigated by in-situ pyrolytic and kinetic analysis. According to kinetic mechanism model, it was found that the internal diffusion had a great influence on volatile release during 120-360 degrees C, while the devolatilization rate during 360-550 degrees C would more depend on the concentration of remaining hydrocarbons. By Py-GC/MS, oils were trapped and analyzed respectively during 60-360 degrees C and 360-550 degrees C, and above 300 compounds were identified and semi-quantified of the volatiles. During 60-360 degrees C, the detected volatile was mainly composed of saturated aliphatics, accounting for 68.69%. More proportion of light chain aliphatic hydrocarbons and monoaromtics were observed during 360-550 degrees C, and the relative content of unsaturated aliphatics increased to 33.81%. From the evolution profiles of typical oil products, the volatile release during 120-360 degrees C would follow the order of molecular weight. But during 360-550 degrees C, as a result of increasing thermal-cracking degree, the release peaks of the different volatile species were corresponded to similar temperature. The gaseous and sulfur-containing compounds were also traced. Among them, CO2 was the main product above 550 degrees C for the decomposition of minerals, and sulfur-containing compounds were mainly generated during < 450 degrees C.
引用
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页数:10
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