2000
DOI: 10.1016/s0306-2619(99)00038-0
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Investigation of oil-shale pyrolysis processing conditions using thermogravimetric analysis

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Cited by 145 publications
(67 citation statements)
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“…Firstly, in lower-temperature region, from ambient temperature up to 200 °C, weight loss attributes to the loss of external moisture, of interlayer water from clay minerals and decomposition of some minor mineral matters [19]. Usually, the weight loss at this stage is used to measure water content.…”
Section: Tg and Dtg Curves Of Oil Shale Pyrolysismentioning
confidence: 99%
“…Firstly, in lower-temperature region, from ambient temperature up to 200 °C, weight loss attributes to the loss of external moisture, of interlayer water from clay minerals and decomposition of some minor mineral matters [19]. Usually, the weight loss at this stage is used to measure water content.…”
Section: Tg and Dtg Curves Of Oil Shale Pyrolysismentioning
confidence: 99%
“…Thermogravimetric analysis (TGA) of oil shale samples has been extensively used as a means of determining pyrolysis characteristics and also to determine kinetic parameters [3][4][5][6][7][8]. Non-isothermal thermogravimetry (TG) has been applied in the study of the kinetics of thermal decomposition of Green River oil shale kerogen [3].…”
Section: Introductionmentioning
confidence: 99%
“…It was observed that the magnitude of the total mass loss was mainly dependent on the final temperature, as well as, to a lesser extent, on the heating rate employed. Williams and Ahmad [8] studied oil shale samples in a thermogravimetric analyzer in relation to heating rate and temperature using nonisothermal and isothermal analysis respectively. The main region of mass loss corresponding to hydrocarbon oil and gas release was between 473-893 K, and a significant mass loss at higher temperatures was attributed to carbonate decomposition.…”
Section: Introductionmentioning
confidence: 99%
“…Oil shale pyrolysis using thermogravimetric 20 analysis has been previously investigated 9,49,50 . It was found that, depending on the oil shale 21 type, its decomposition exhibits either single or a two-stage evolution of hydrocarbon material, in 22 the temperature range of 250 -620ºC.…”
mentioning
confidence: 99%
“…At temperatures higher than 600ºC, thermal decomposition 1 of carbonates takes place, due to the presence of minerals, such as calcite or dolomite. 2 Thermal treatment of fresh oil shale under nitrogen flow showed a two-stage decomposition 3 process ( Figure 4A and B) where the transformation step at 720ºC is most likely due to 4 carbonates decomposition 49 . Afterwards, an oxidation step allowed the combustion of residual 5 carbon from refractory material, such as heavy oils, tar-mats, coke 10 .…”
mentioning
confidence: 99%