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Fractal dimension of large aggregates under different flocculation conditions

dc.contributor.authorMoruzzi, Rodrigo B. [UNESP]
dc.contributor.authorde Oliveira, André L. [UNESP]
dc.contributor.authorda Conceição, Fabiano T. [UNESP]
dc.contributor.authorGregory, John
dc.contributor.authorCampos, Luiza C.
dc.contributor.institutionUniversidade Estadual Paulista (Unesp)
dc.contributor.institutionUniversity College London
dc.date.accessioned2018-12-11T16:48:33Z
dc.date.available2018-12-11T16:48:33Z
dc.date.issued2017-12-31
dc.description.abstractThe two-dimensional fractal dimension (Df) of large aggregates of kaolin (> 540 μm) during the shear flocculation process for kaolin solution was investigated using non-intrusive in situ image-based acquisition system. Separate experiments were also carried out for three different sized sub-ranges of large aggregates (0.540–1.125 mm; 1.125–1.750 mm; 1.750–2.375 mm). Digital images were taken at a frequency of 10 Hz for 10 s for each different pairs of gradients of velocity (Gf) of 20 and 60 s− 1 and flocculation times of 2; 3; 4; 5; 10; 20; 30; 60; 120 and 180 min. For the same conditions, particle size distribution (PSD) was also determined. Under the investigated conditions, the lowest Gf produced the greatest Df (1.69) at a flocculation time of 30 min for the whole range of aggregates. Also, the evolution of the longest length of aggregate (l) and Df with time, showed that the dynamic steady-state was reached at different times for each shear rate and l ranges. However, Df varied for each size sub-range (ca. 1.1 to 1.8). Finally, the behavior of the aggregate structure may be understood by the predominance of different aggregation mechanisms such as cluster-cluster for Gf of 60 s− 1 and particle-cluster for Gf of 20 s− 1.en
dc.description.affiliationUniversidade Estadual Paulista (UNESP) Instituto de Geociências e Ciências Exatas
dc.description.affiliationDepartment of Civil Environmental and Geomatic Engineering University College London
dc.description.affiliationUnespUniversidade Estadual Paulista (UNESP) Instituto de Geociências e Ciências Exatas
dc.description.sponsorshipFundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)
dc.description.sponsorshipIdFAPESP: 2013/01634-3
dc.description.sponsorshipIdFAPESP: 2013/21355-1
dc.description.sponsorshipIdFAPESP: 2013/25641-9
dc.description.sponsorshipIdFAPESP: 2010/50694-0
dc.format.extent807-814
dc.identifierhttp://dx.doi.org/10.1016/j.scitotenv.2017.07.194
dc.identifier.citationScience of the Total Environment, v. 609, p. 807-814.
dc.identifier.doi10.1016/j.scitotenv.2017.07.194
dc.identifier.file2-s2.0-85026476600.pdf
dc.identifier.issn1879-1026
dc.identifier.issn0048-9697
dc.identifier.scopus2-s2.0-85026476600
dc.identifier.urihttp://hdl.handle.net/11449/169978
dc.language.isoeng
dc.relation.ispartofScience of the Total Environment
dc.relation.ispartofsjr1,546
dc.rights.accessRightsAcesso abertopt
dc.sourceScopus
dc.subjectAggregates
dc.subjectFlocculation
dc.subjectFractal dimension
dc.subjectShear rate
dc.titleFractal dimension of large aggregates under different flocculation conditionsen
dc.typeArtigopt
dspace.entity.typePublication
relation.isOrgUnitOfPublication4763ec56-704e-41e0-9685-b5bef5946feb
relation.isOrgUnitOfPublication.latestForDiscovery4763ec56-704e-41e0-9685-b5bef5946feb
unesp.campusUniversidade Estadual Paulista (UNESP), Instituto de Geociências e Ciências Exatas, Rio Claropt

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