Abstract
The practical and theoretical effects of using non-point support data for estimating variograms or on the kriging equations when estimating spatial averages, i.e., block kriging, are well-known. Under an assumption of lognormality the proportional effect is also wellknown. While other transformations are commonly used in statistics only the log and indicator transforms are widely used in geostatistics, the latter has the advantage of generally not requiring an inverse transform.. Additional theoretical and empirical results are presented on the interrelationship between non-point support data, non-linear transformations and variogram estimation, modeling. The non-point support data may incorporate spatial averages or compositing of point support data.
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© 1994 Springer Science+Business Media Dordrecht
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Myers, D.E. (1994). Change of Support and Transformations. In: Dimitrakopoulos, R. (eds) Geostatistics for the Next Century. Quantitative Geology and Geostatistics, vol 6. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-0824-9_30
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DOI: https://doi.org/10.1007/978-94-011-0824-9_30
Publisher Name: Springer, Dordrecht
Print ISBN: 978-94-010-4354-0
Online ISBN: 978-94-011-0824-9
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