Skip to main content
Log in

Scale Effect on Principal Component Analysis for Vector Random Functions

  • Published:
Mathematical Geology Aims and scope Submit manuscript

Abstract

Principal component analysis (PCA) is commonly applied without looking at the “spatial support” (size and shape, of the samples and the field), and the cross-covariance structure of the explored attributes. This paper shows that PCA can depend on such spatial features. If the spatial random functions for attributes correspond to largely dissimilar variograms and cross-variograms, the scale effect will increase as well. On the other hand, under conditions of proportional shape of the variograms and cross-variograms (i.e., intrinsic coregionalization), no scale effect may occur. The theoretical analysis leads to eigenvalue and eigenvector functions of the size of the domain and sample supports. We termed this analysis “growing scale PCA,” where spatial (or time) scale refers to the size and shape of the domain and samples. An example of silt, sand, and clay attributes for a second-order stationary vector random function shows the correlation matrix asymptotically approaches constants at two or three times the largest range of the spherical variogram used in the nested model. This is contrary to the common belief that the correlation structure between attributes become constant at the range value. Results of growing scale PCA illustrate the rotation of the orthogonal space of the eigenvectors as the size of the domain grows. PCA results are strongly controlled by the multivariate matrix variogram model. This approach is useful for exploratory data analysis of spatially autocorrelated vector random functions.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

REFERENCES

  • Basilevsky, A., 1994, Statistical factor analysis and related methods, theory and applications: John Wiley & Sons, New York, 737 p.

    Google Scholar 

  • Davis, B. M., and Greenes, K. A., 1983, Estimation using spatially distributed multivariate data. An example with coal quality: Math. Geology, v. 15, n. 2, p. 287–300.

    Google Scholar 

  • Goovaerts, P., 1993, Spatial orthogonality of the principal components computed from coregionalized variables: Math. Geology, v. 25, no. 3, p. 281–301.

    Google Scholar 

  • Goulard, M., and Voltz, M., 1992, Linear coregionalization: Tools for estimation and choice of cross-variogram matrix: Math. Geology, v. 24, no. 3, p. 269–286.

    Google Scholar 

  • Journel, A. G., and Huijbregts, Ch. J., 1978, Mining geostatistics: Academic Press, New York, 600 p.

    Google Scholar 

  • Mardia, K. V., Kent, J. T., and Bibby, J. M., 1979, Multivariate analysis: Academic Press, London, 521 p.

    Google Scholar 

  • Myers, D. E., 1994, The linear model and simultaneous diagonalization of the variogram matrix function, in Fabbri, A. G., and Royer, J. J., eds., 3rd CODATA Conference on Geomathematics and Geostatistics: Sci. de la terre, Sér. Inf., Nancy, v. 32, p. 125–139.

  • Preisendorfer, R., 1988, Principal component analysis in meteorology and oceanography: Elsevier, New York, 425 p.

    Google Scholar 

  • Sandjivy, L., 1984, The factorial kriging analysis of regionalized data. Its application to geochemical prospecting, in Verly, G., and others, eds., Geostatistics for Natural Resources Characterization: NATO-ASI Series C., v. 122, Reidel Publ. Co., Dordrecht, p. 559–572.

    Google Scholar 

  • Vargas-Guzmán, J. A., Warrick, A. W., and Myers, D. E., 1999, Multivariate correlation in the framework of support and spatial scales of variability: Math. Geology, v. 31, no. 1, p. 85–103.

    Google Scholar 

  • Wackernagel, H., 1985, The inference of the linear model of coregionalization in the case of a geochemical data set: Ecole des Mines de Paris, Centre de Geostatisque et de Morphologie Mathematique, Fontainebleau, 14 p.

    Google Scholar 

  • Wackernagel, H., 1995, Multivariate geostatistics: Springer, Berlin, 256 p.

    Google Scholar 

  • Warrick, A. W., Musil, S. A., Artiola, J. F., Hendricks, D. E., and Myers, D. E., 1990, Sampling strategies for hydrological properties and chemical constituents in the upper vadose zone, final technical report: University of Arizona, Tucson, Arizona, p. 117.

    Google Scholar 

  • Xie, T., and Myers, D. E., 1995, Fitting matrix valued variogram models by simultaneous diagonalization. I Theory: Math. Geology, v. 27, no. 7, p. 867–876.

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Rights and permissions

Reprints and permissions

About this article

Cite this article

Vargas-Guzmán, J.A., Warrick, A.W. & Myers, D.E. Scale Effect on Principal Component Analysis for Vector Random Functions. Mathematical Geology 31, 701–722 (1999). https://doi.org/10.1023/A:1007532527596

Download citation

  • Issue Date:

  • DOI: https://doi.org/10.1023/A:1007532527596

Navigation