dc.contributorTras Os Montes & Alto Douro Univ
dc.contributorUniv Coimbra
dc.contributorUniversidade Estadual Paulista (Unesp)
dc.date.accessioned2014-05-20T15:24:28Z
dc.date.accessioned2022-10-05T16:28:38Z
dc.date.available2014-05-20T15:24:28Z
dc.date.available2022-10-05T16:28:38Z
dc.date.created2014-05-20T15:24:28Z
dc.date.issued2005-05-01
dc.identifierMathematical Geology. New York: Springer/plenum Publishers, v. 37, n. 4, p. 393-417, 2005.
dc.identifier0882-8121
dc.identifierhttp://hdl.handle.net/11449/35075
dc.identifier10.1007/s11004-005-5955-1
dc.identifierWOS:000230653300005
dc.identifier7206664999934534
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/3907090
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.
dc.languageeng
dc.publisherSpringer
dc.relationMathematical Geology
dc.rightsAcesso restrito
dc.sourceWeb of Science
dc.subjectcorrespondence analysis
dc.subjectcluster analysis
dc.subjectdiscriminant analysis
dc.subjectsurface mapping tools
dc.subjectregionalized classification
dc.subjecthydrodynamic dispersion
dc.titleTwo-way regionalized classification of multivariate datasets and its application to the assessment of hydrodynamic dispersion
dc.typeArtigo


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