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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
unesp.campusUniversidade Estadual Paulista (UNESP), Instituto de Geociências e Ciências Exatas, Rio Claropt

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