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R correlation coefficient

Fig. 7. Toxicity of chlorine to aquatic organisms, (a) Time-dependent mortaUty (50%) of four example species in various levels of total residual chlorine in the laboratory, where for A, A.losa aestivalis and B, Salmogairdnerii r (correlation coefficient of the curve) = —0.96 and for C, P/euroneetesplatessa and D, Salmo trutta r = —0.98. (b) A summary of chlorine toxicity to freshwater species, indicating overall no-effect thresholds for acute and chronic exposures. Numbers indicate where more than one test yielded the same result. A different summary figure appHes to marine organisms because of differences in the... Fig. 7. Toxicity of chlorine to aquatic organisms, (a) Time-dependent mortaUty (50%) of four example species in various levels of total residual chlorine in the laboratory, where for A, A.losa aestivalis and B, Salmogairdnerii r (correlation coefficient of the curve) = —0.96 and for C, P/euroneetesplatessa and D, Salmo trutta r = —0.98. (b) A summary of chlorine toxicity to freshwater species, indicating overall no-effect thresholds for acute and chronic exposures. Numbers indicate where more than one test yielded the same result. A different summary figure appHes to marine organisms because of differences in the...
Table I. Simple regression of TOW-ISO data and time for Campeche PCGM coastal test station in a period of 2 years. Equation t = a + b TOW-ISO, r = correlation coefficient, r2 = percentage of variation explained by the independent variable, P = Statistical... Table I. Simple regression of TOW-ISO data and time for Campeche PCGM coastal test station in a period of 2 years. Equation t = a + b TOW-ISO, r = correlation coefficient, r2 = percentage of variation explained by the independent variable, P = Statistical...
Symbols p— Raman depolarization ratio, r - correlation coefficient... [Pg.263]

Sc = water solubility of crystalline dye in mol/m3 mp = melting point in degrees C R = correlation coefficient... [Pg.483]

The online statistical calculations can be performed at http //members.aol.com/ johnp71/javastat.html. To carry out linear regression analysis as an example, select Regression, correlation, least squares curve-fitting, nonparametric correlation, and then select any one of the methods (e.g., Least squares regression line, Least squares straight line). Enter number of data points to be analyzed, then data, x and y . Click the Calculate Now button. The analytical results, a (intercept), b (slope), f (degrees of freedom), and r (correlation coefficient) are returned. [Pg.27]

Tab. 3.2 Statistical parameters (n, number of data points r, correlation coefficient s, standard error) of regression equations relating bioactivity data [6] to experimental hydro-phobicity parameters. (Reprinted from Tab. 4 of ref. 5, with permission from Elsevier Science)... Tab. 3.2 Statistical parameters (n, number of data points r, correlation coefficient s, standard error) of regression equations relating bioactivity data [6] to experimental hydro-phobicity parameters. (Reprinted from Tab. 4 of ref. 5, with permission from Elsevier Science)...
Note r = correlation coefficient n = number of compounds analyzed, p = net charge on P, Kcorr = hydrolysis rate corrected for fraction of compound sorbed to sediment. K"corr represents a sediment-catalyzed transformation and rates of hydrolysis in the overlying water phase will be much lower than predicted using these QSARs. [Pg.330]

Figure 7.17 Estimated accretion rates of intertidal salt marshes on the coast of Rhode Island (USA). Despite having well-developed exponential decay curves of excess 210Pb in most marsh sediment cores, indicating a relatively a constant rate of sediment accretion, some variations in the log excess 210Pb indicate that accretion may not have been constant through time. R = correlation coefficient, I = inventories of excess 210Pb (dpm cm-2) (Benninger, 1979 Olsen et al., 1985). (Modified from Bricker-Urso et al., 1989.)... Figure 7.17 Estimated accretion rates of intertidal salt marshes on the coast of Rhode Island (USA). Despite having well-developed exponential decay curves of excess 210Pb in most marsh sediment cores, indicating a relatively a constant rate of sediment accretion, some variations in the log excess 210Pb indicate that accretion may not have been constant through time. R = correlation coefficient, I = inventories of excess 210Pb (dpm cm-2) (Benninger, 1979 Olsen et al., 1985). (Modified from Bricker-Urso et al., 1989.)...
Solvent, 50E, a (v/v) mixture of 50% aqueous-50% EtOH, 80E a (v/v) mixture of 20% aqueous-80% EtOH. R, correlation coefficient SD, standard deviation n, number of substituents included in the correlation. Correlation (overall p) for three aryl-substituents, Yukawa et al. (1966) data taken from Deno and Evans (1957), Deno and Schriesheim (1955), Deno etal. (1955,1959). Fujio et al. (1997c). Murata et al. (1990a). [Pg.274]


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