The study of natural dolomite as a prospective material for CO2 capture employing a novel approach to the evaluation of breakthrough curves

dc.contributor.authorImrichová, Annacs
dc.contributor.authorSokola, Patrikcs
dc.contributor.authorMásilko, Jiřícs
dc.contributor.authorBaláš, Marekcs
dc.contributor.authorCába, Vladislavcs
dc.contributor.authorKarásková, Kateřinacs
dc.contributor.authorŠvec, Jiřícs
dc.contributor.authorPtáček, Petrcs
dc.coverage.issueDecembercs
dc.coverage.volume24cs
dc.date.accessioned2026-03-13T10:53:44Z
dc.date.issued2025-12-01cs
dc.description.abstractThe capture of carbon dioxide (CO2) is a critical technology for addressing climate change and sustainability objectives. In this study, the performance of natural dolomite as an effective sorbent for repeated CO2 capture was evaluated. The results suggested that an optimal calcination temperature of 850 degrees C was beneficial for minimizing surface sintering of the dolomite, thereby facilitating effective decarbonation. Breakthrough curve analysis was conducted to evaluate the dynamic adsorption performance of dolomite at varying CO2 concentrations (10 %, 12 %, and 16 %). To assess the progress of gas adsorption onto regenerated dolomite, an innovative method of curve fitting using the modified Avrami equation was employed, which provided three essential parameters for the adsorption process: retention time, rate constant, and Avrami coefficient. A steady decrease in breakthrough time and adsorption efficiency was found to be correlated with sintering and surface area loss. The maximum CO2 adsorption capacity was achieved during the second or third cycle for all three measured CO2 concentrations; however, performance gradually deteriorated in subsequent cycles due to surface sintering and a reduction in specific surface area. TPD and BET analyses supported the conclusion that the surface area decreased with repeated regeneration, and the basic active sites were reduced.en
dc.formattextcs
dc.format.extent1-13cs
dc.format.mimetypeapplication/pdfcs
dc.identifier.citationOpen Ceramics. 2025, vol. 24, issue December, p. 1-13.en
dc.identifier.doi10.1016/j.oceram.2025.100844cs
dc.identifier.issn2666-5395cs
dc.identifier.orcid0009-0005-3530-5677cs
dc.identifier.orcid0000-0002-9764-9505cs
dc.identifier.orcid0000-0001-9587-5843cs
dc.identifier.orcid0000-0002-4968-1535cs
dc.identifier.orcid0000-0002-8409-992Xcs
dc.identifier.orcid0000-0002-2943-9864cs
dc.identifier.orcid0000-0003-0586-7693cs
dc.identifier.other199180cs
dc.identifier.researcheridQ-1628-2018cs
dc.identifier.scopus25621858200cs
dc.identifier.scopus35077163600cs
dc.identifier.scopus56338516900cs
dc.identifier.urihttps://hdl.handle.net/11012/256419
dc.language.isoencs
dc.publisherElseviercs
dc.relation.ispartofOpen Ceramicscs
dc.relation.urihttps://www.sciencedirect.com/science/article/pii/S2666539525001117cs
dc.rightsCreative Commons Attribution 4.0 Internationalcs
dc.rights.accessopenAccesscs
dc.rights.sherpahttp://www.sherpa.ac.uk/romeo/issn/2666-5395/cs
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/cs
dc.subjectDolomiteen
dc.subjectRegenerationen
dc.subjectAvrami equationen
dc.subjectAdsorptionen
dc.subjectBreakthrough curvesen
dc.subjectCarbon dioxideen
dc.titleThe study of natural dolomite as a prospective material for CO2 capture employing a novel approach to the evaluation of breakthrough curvesen
dc.type.driverarticleen
dc.type.statusPeer-revieweden
dc.type.versionpublishedVersionen
eprints.grantNumberinfo:eu-repo/grantAgreement/GA0/GA/GA24-12423Scs
sync.item.dbidVAV-199180en
sync.item.dbtypeVAVen
sync.item.insts2026.03.13 11:53:44en
sync.item.modts2026.03.13 11:32:52en
thesis.grantorVysoké učení technické v Brně. Fakulta chemická. Ústav chemie materiálůcs
thesis.grantorVysoké učení technické v Brně. Fakulta strojního inženýrství. Energetický ústavcs

Files

Original bundle

Now showing 1 - 1 of 1
Loading...
Thumbnail Image
Name:
1s2.0S2666539525001117main.pdf
Size:
10.64 MB
Format:
Adobe Portable Document Format
Description:
file 1s2.0S2666539525001117main.pdf