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dc.contributor.authorMalutta, Simonept_BR
dc.contributor.authorChaffe, Pedro Luiz Borgespt_BR
dc.contributor.authorBonumá, Nadia Bernardipt_BR
dc.contributor.authorKobiyama, Masatopt_BR
dc.date.accessioned2021-01-09T04:19:03Zpt_BR
dc.date.issued2020pt_BR
dc.identifier.issn0273-1223pt_BR
dc.identifier.urihttp://hdl.handle.net/10183/217184pt_BR
dc.description.abstractThis work is a review of the use of hysteresis to quantify sediment discharge dynamics. We reviewed 71 journal articles from the year 1953 to the present day focusing on two topics: the factors that influence hysteresis; and hysteresis quantification. The main factors influencing hysteresis are: (a) magnitude and sequence of events; (b) sediment particle size distribution; (c) basin size; and (d) land use and sediment source. Hysteresis quantification can be done using several different methods that can be grouped as: (a) hysteresis indexes; (b) statistical analysis; and (c) uncertainty analysis. Most studies were conducted in Western Europe and the USA. The studies, in general, show how the factors listed above influence the shape and patterns of hysteresis. However, the sediment dynamics are complex, and the hysteresis patterns may be linked to many other factors, such as slope and drainage systems. The quantification of hysteresis still appears, mainly with the hysteresis index and statistical analysis. Therefore, there are still many other factors that influence hysteresis patterns, as well as hysteresis rates and uncertainty analyses.en
dc.format.mimetypeapplication/pdfpt_BR
dc.language.isoengpt_BR
dc.relation.ispartofWater science and technology. Vol. 81, n. 12 (jun. 2020), p. 2471–2487pt_BR
dc.rightsOpen Accessen
dc.subjectHysteresisen
dc.subjectHisteresept_BR
dc.subjectSedimenten
dc.subjectTransporte de sedimentospt_BR
dc.subjectRevisão de literaturapt_BR
dc.subjectTurbidityen
dc.titleHysteresis analysis to quantify and qualify the sediment dynamics : state of the artpt_BR
dc.typeArtigo de periódicopt_BR
dc.identifier.nrb001118492pt_BR
dc.type.originEstrangeiropt_BR


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