Abstract
Analysis of variance (ANOVA) is a method of decomposing the total variation displayed by a set of observations (as measured by the sums of squares of differences from the mean) into components associated with defined sources of variation. The relative magnitude of the contribution of each source to the overall observed total variation may thereby be determined. The technique was introduced by the English statistician, (Sir) Ronald Alymer Fisher (1890–1962) in the early 1920s and was widely taken up following later publication of Fisher (1925a). The technique was first introduced into geology by the American statistician, Churchill Eisenhart (1913–1994) (Eisenhart 1935). Classical applications include the investigation of whether a statistically significant difference exists between samples of nominally similar composition (Eisenhart 1935), and the magnitude of variation introduced by different human operators in determination of physical sample composition by modal analysis, determination of grain size, shape, orientation, density, porosity, etc. (Griffiths and Rosenfeld 1954). More recently, it has been widely used in the estimation of relative magnitudes of sources of sampling and analytical (chemical) variance in regional- or local-scale environmental geochemical surveys (Miesch 1967a, b, 1976a, b; Garrett and Goss 1979; Thompson and Ramsay 1995; Ramsay et al. 1995). Garrett and Goss (1980a, b) provided a program for analysis of variance of unbalanced nested sampling designs (UANOVA); see also Goss and Garrett (1978).
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Howarth, R.J. (2017). U. In: Dictionary of Mathematical Geosciences . Springer, Cham. https://doi.org/10.1007/978-3-319-57315-1_21
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