2014
DOI: 10.1016/j.fuel.2013.11.013
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A comparison of the structure and reactivity of five Jordanian oil shales from different locations

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Cited by 23 publications
(29 citation statements)
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“…As the temperature was increased, the Colorado conversions rose much more rapidly than those of Julia Creek, and at 425°C were considerably higher in N 2 and roughly equivalent in H 2 . The distinctly higher atomic H/C ratio of the Colorado oil shale did not lead to a higher reactivity over the whole temperature range; a similar lack of dependence of reactivity on atomic H/C ratio has been previously noted for some Jordanian oil shales [27]. The Fischer assay oil yield obtained for a number of Colorado Mahogany Zone oil shales was about 66 wt.% dmmf [43], much higher than the oil yield of Colorado oil shale under N 2 at temperatures up to 425°C.…”
Section: Characterization Of the Oil Shalessupporting
confidence: 80%
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“…As the temperature was increased, the Colorado conversions rose much more rapidly than those of Julia Creek, and at 425°C were considerably higher in N 2 and roughly equivalent in H 2 . The distinctly higher atomic H/C ratio of the Colorado oil shale did not lead to a higher reactivity over the whole temperature range; a similar lack of dependence of reactivity on atomic H/C ratio has been previously noted for some Jordanian oil shales [27]. The Fischer assay oil yield obtained for a number of Colorado Mahogany Zone oil shales was about 66 wt.% dmmf [43], much higher than the oil yield of Colorado oil shale under N 2 at temperatures up to 425°C.…”
Section: Characterization Of the Oil Shalessupporting
confidence: 80%
“…However, for Julia Creek the TGA volatiles yield (66 wt.% dmmf) was much higher than the 40 wt.% dmmf predicted from the Fischer assay oil yield [32]. As previously noted [27], the loss of weight in 550-950°C has been correlated with the CO 2 from the carbonate present, but the correlation is imperfect; in particular, the loss of weight in this temperature range from Julia Creek oil shale was less than would have been predicted from the inorganic carbon content (Table 1). Since the weight loss in 120-550°C was greater than predicted by Fischer assay, it is possible that some of the carbonate decomposed below 550°C.…”
Section: Characterization Of the Oil Shalessupporting
confidence: 53%
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