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Regular solution model to predict the asphaltenes flocculation and sediments formation during hydrocracking of heavy oil

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dc.contributor Казанский федеральный университет
dc.contributor.author Felix Lugo Jose Guillermo
dc.contributor.author Ancheyta Juarez Jorge
dc.date.accessioned 2026-08-25T11:11:07Z
dc.date.available 2026-08-25T11:11:07Z
dc.date.issued 2020
dc.identifier.citation Felix G., Ancheyta J. Regular solution model to predict the asphaltenes flocculation and sediments formation during hydrocracking of heavy oil // Fuel. - 260 (2020). - 116160.
dc.identifier.uri https://dspace.kpfu.ru/xmlui/handle/net/186098
dc.description.abstract Experiments of hydrocracking of heavy crude oil were carried out in a 1.8 L batch reactor with a mineral dispersed catalyst. Sediments content was analyzed at different reaction times (2-5 h) and temperatures (360-400 ?C). A regular solution model and a kinetic model were applied to predict the flocculation of asphaltenes to form sediments. It was observed that as the temperature increases the solubility parameter of the SARA fractions decreased. Enhanced sediments formation was found when the saturates/asphaltenes ratio increased indicating that the insolubility of asphaltenes in the crude oil depends on saturates fraction. The calculated values obtained with the thermodynamic-kinetic model showed good accuracy with respect to experimental data, particularly at high conversion, which is the most important issue in commercial hydrocracking units.
dc.language.iso en
dc.relation.ispartofseries Fuel
dc.rights только для КФУ
dc.subject Regular solution model
dc.subject Sediments
dc.subject Asphaltenes
dc.subject Hydrocracking
dc.subject.other Химия
dc.title Regular solution model to predict the asphaltenes flocculation and sediments formation during hydrocracking of heavy oil
dc.type Article
dc.contributor.org Институт геологии и нефтегазовых технологий
dc.description.pages 116160-116160
dc.relation.ispartofseries-volume 260
dc.pub-id 329240
dc.identifier.doi 10.1016/j.fuel.2019.116160


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