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dc.contributor.authorPacheco, FAL-
dc.contributor.authorLandim, PMB-
dc.date.accessioned2014-05-20T15:24:28Z-
dc.date.accessioned2016-10-25T17:58:42Z-
dc.date.available2014-05-20T15:24:28Z-
dc.date.available2016-10-25T17:58:42Z-
dc.date.issued2005-05-01-
dc.identifierhttp://dx.doi.org/10.1007/s11004-005-5955-1-
dc.identifier.citationMathematical Geology. New York: Springer/plenum Publishers, v. 37, n. 4, p. 393-417, 2005.-
dc.identifier.issn0882-8121-
dc.identifier.urihttp://hdl.handle.net/11449/35075-
dc.identifier.urihttp://acervodigital.unesp.br/handle/11449/35075-
dc.description.abstractZones of mixing between shallow groundwaters of different composition were unravelled by two-way regionalized classification, a technique based on correspondence analysis (CA), cluster analysis (ClA) and discriminant analysis (DA), aided by gridding, map-overlay and contouring tools. The shallow groundwaters are from a granitoid plutonite in the Funda o region (central Portugal). Correspondence analysis detected three natural clusters in the working dataset: 1, weathering; 2, domestic effluents; 3, fertilizers. Cluster analysis set an alternative distribution of the samples by the three clusters. Group memberships obtained by correspondence analysis and by cluster analysis were optimized by discriminant analysis, gridded memberships as follows: codes 1, 2 or 3 were used when classification by correspondence analysis and cluster analysis produced the same results; code 0 when the grid node was first assigned to cluster 1 and then to cluster 2 or vice versa (mixing between weathering and effluents); code 4 in the other cases (mixing between agriculture and the other influences). Code-3 areas were systematically surrounded by code-4 areas, an observation attributed to hydrodynamic dispersion. Accordingly, the extent of code-4 areas in two orthogonal directions was assumed proportional to the longitudinal and transverse dispersivities of local soils. The results (0.7-16.8 and 0.4-4.3 m, respectively) are acceptable at the macroscopic scale. The ratios between longitudinal and transverse dispersivities (1.2-11.1) are also in agreement with results obtained by other studies.en
dc.format.extent393-417-
dc.language.isoeng-
dc.publisherSpringer-
dc.sourceWeb of Science-
dc.subjectcorrespondence analysispt
dc.subjectcluster analysispt
dc.subjectdiscriminant analysispt
dc.subjectsurface mapping toolspt
dc.subjectregionalized classificationpt
dc.subjecthydrodynamic dispersionpt
dc.titleTwo-way regionalized classification of multivariate datasets and its application to the assessment of hydrodynamic dispersionen
dc.typeoutro-
dc.contributor.institutionTras Os Montes & Alto Douro Univ-
dc.contributor.institutionUniv Coimbra-
dc.contributor.institutionUniversidade Estadual Paulista (UNESP)-
dc.description.affiliationTras Os Montes & Alto Douro Univ, Dept Geol, P-5000 Vila Real, Portugal-
dc.description.affiliationUniv Coimbra, Geophys Ctr, P-3000 Coimbra, Portugal-
dc.description.affiliationSão Paulo State Univ, Dept Appl Geol, BR-13506900 Rio Claro, SP, Brazil-
dc.description.affiliationUnespSão Paulo State Univ, Dept Appl Geol, BR-13506900 Rio Claro, SP, Brazil-
dc.identifier.doi10.1007/s11004-005-5955-1-
dc.identifier.wosWOS:000230653300005-
dc.rights.accessRightsAcesso restrito-
dc.relation.ispartofMathematical Geology-
Appears in Collections:Artigos, TCCs, Teses e Dissertações da Unesp

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