Two-way regionalized classification of multivariate datasets and its application to the assessment of hydrodynamic dispersion

被引:39
作者
Pacheco, FAL [1 ]
Landim, PMB
机构
[1] Tras Os Montes & Alto Douro Univ, Dept Geol, P-5000 Vila Real, Portugal
[2] Univ Coimbra, Geophys Ctr, P-3000 Coimbra, Portugal
[3] Sao Paulo State Univ, Dept Appl Geol, BR-13506900 Rio Claro, SP, Brazil
来源
MATHEMATICAL GEOLOGY | 2005年 / 37卷 / 04期
关键词
correspondence analysis; cluster analysis; discriminant analysis; surface mapping tools; regionalized classification; hydrodynamic dispersion;
D O I
10.1007/s11004-005-5955-1
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Zones 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.
引用
收藏
页码:393 / 417
页数:25
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