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Correlation matrix sample

Optimizing the GC instrument is crucial for the quantitation of sulfentrazone and its metabolites. Before actual analysis, the temperatures, gas flow rates, and the glass insert liner should be optimized. The injection standards must have a low relative standard deviation (<15%) and the calibration standards must have a correlation coefficient of at least 0.99. Before injection of the analysis set, the column should be conditioned with a sample matrix. This can be done by injecting a matrix sample extract several times before the standard, repeating this conditioning until the injection standard gives a reproducible response and provides adequate sensitivity. [Pg.576]

The symmetric sample correlation matrix R (or p) is similarly defined by its current element... [Pg.204]

Defining sx and sy as the diagonal matrices of sample standard deviations on x and y, respectively, the sample correlation matrix would be... [Pg.204]

Greenfield ef. ai.l l) observed a reduction of signal intensity that correlates with sample intake effects from the modified solution viscosity and/or surface tension of mineral acids. This, coupled with peristaltic pumping of solutions into the nebulizer, considerably reduces physical interferences. Increased salt concentration also has an effect on solution physical properties. In the experience of these authors, the high levels of salt in the matrix also increases the noise from the nebulizer system. This degradation of nebulizer performance, which is not necessarily accompanied by a proportional reduction in sensitivity, is the cause of the observed deterioration of detection limits in real samples as opposed to ideal solutions. [Pg.128]

The second difference is that the correlations between samples are calculated rather than the correlations between elements. In the terminology of Rozett and Peterson ( ), the correlation between elements would be an R analysis while the correlation between samples would be a Q analysis. Thus, the applications of factor analysis discussed above are R analyses. Imbrle and Van Andel ( 6) and Miesch (J 7) have found Q-mode analysis more useful for interpreting geological data. Rozett and Peterson (J ) compared the two methods for mass spectrometric data and concluded that the Q-mode analysis provided more significant informtlon. Thus, a Q-mode analysis on the correlation about the origin matrix for correlations between samples has been made (18,19) for aerosol composition data from Boston and St. Louis. [Pg.35]

The analyst should check the Shepard diagram that represents a step line so-called D-hat values. If all reproduced distances fall onto the step-line, then the rank ordering of distances (or similarities) would be perfectly reproduced by the dimensional model, while deviations from the step-line mean lack of fit. The interpretation of the dimensions usually represents the final step of this multivariate procedure. As in factor analysis, the final orientation of axes in the plane (or space) is mostly the result of a subjective decision by the researcher since the distances between objects remain invariable regardless of the type of the rotation. However, it must be remembered that MDS and FA are different methods. FA requires that the underlying data be distributed as multivariate normal, whereas MDS does not impose such a restriction. MDS often yields more interpretable solutions than FA because the latter tends to extract more factors. MDS can be applied to any kind of distances or similarities (those described in cluster analysis), whereas FA requires firstly the computation of the correlation matrix. Figure 7.3 shows the results of applying MDS to the samples described in the CA and FA sections (7.3.1 and 7.3.2). [Pg.165]

Correlation coefficient between samples. A correlation coefficient of 1 implies that samples have identical characteristics, which all objects have with themselves. Some workers use the square or absolute value of a correlation coefficient, and it depends on the precise physical interpretation as to whether negative correlation coefficients imply similarity or dissimilarity. In this text we assume that the more negative is the correlation coefficient, the less similar are the objects. The correlation matrix is presented in Table 4.17. Note that the top right-hand side is not presented as it is the same as the bottom left-hand side. The higher is the correlation coefficient, the more similar are the objects. [Pg.225]

It is fairly evident that because of the complex interactions of deposi-tionally influenced and metamorphically influenced properties, the fundamental chemical-structural properties will need to be related to each other in a complex statistical fashion. A multivariate correlation matrix such as that pioneered by Waddell (8) appears to be an absolute requirement. However, characterization parameters far more sophisticated than those employed by Waddell are required. One can hope that, as correlations between parameters become evident, certain key properties will be discovered that will allow coal scientists and technologists to identify and classify vitrinites uniquely. Measurement of reflectance or other optical properties, if carried out properly, possibly on somewhat modified samples, might prove valuable in this respect. It then would not be necessary for every laboratory to have supersophisticated analytical equipment at its disposal in order to classify a coal properly. By properly identifying and classifying the vitrinite in a coal, one then could estimate accurately the many other vitrinite properties available in the multivariate correlation matrix. [Pg.11]

Table 2 The matrix of correlations between objects from Table 1, (a). Samples A and D, B and C form new objects and a new correlation matrix can be calculated, (b). Sample E then joins AD and F joins BC to provide the final step and apparent correlation matrix, (c)... Table 2 The matrix of correlations between objects from Table 1, (a). Samples A and D, B and C form new objects and a new correlation matrix can be calculated, (b). Sample E then joins AD and F joins BC to provide the final step and apparent correlation matrix, (c)...
The original MCDA approach is focused on the point estimate of the BR score. Conditional on the value functions and weights selected, an interval estimate can be constructed for S, AS, and to account for the sampling variation of the data. The correlation matrix needs to be estimated or a resampling-based method can be employed to construct the interval estimate. [Pg.278]

To compare the scent profiles of individuals we selected 11 compounds and calculated their relative peak areas. Principal Component Analysis (PCA) was used to compare the individual peak areas of the four individuals. PCA is a multivariate statistical method which reduces the dimensions of a single group of data by producing a smaller number of abstract variables (Jolliffe, 1986). For this analysis we used multiple samples of each individual and calculated all factors on the basis of a correlation matrix. The resulting first and second factor accounted for a total of 99.17 % of the variance in proportional peak area. [Pg.94]

Figure 3 The original data, X, comprising n objects or samples described by m variables, is converted to a dispersion (covariance or correlation) matrix C. The eigenvalues, A, and eigenvectors, L, are extracted from C. A reduced set of eigenvectors, L, i.e., selected and the original data projected into this new, lower-dimensional pattern space Y. Figure 3 The original data, X, comprising n objects or samples described by m variables, is converted to a dispersion (covariance or correlation) matrix C. The eigenvalues, A, and eigenvectors, L, are extracted from C. A reduced set of eigenvectors, L, i.e., selected and the original data projected into this new, lower-dimensional pattern space Y.

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