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                        The random errors in filling a 250-mL flask might be ±0.05 mL, or only 0.02% of the total volume
                       of the flask. The random error in filling a transfer pipette should not exceed 0.006 mL, giving an error
                       of about 0.024% of the total volume (Miller and Miller, 1984). The error in reading a burette (of the
                       conventional variety graduated in 0.1-mL divisions) is perhaps ±0.02 mL. Each titration involves two
                       such readings (the errors of which are not simply additive). If the titration volume is about 25 mL, the
                       percentage error is again very small. (The titration should be arranged so that the volume of titrant is
                       not too small.)
                        In skilled hands, with all precautions taken, volumetric analysis should have a relative standard
                       deviation of not more than about 0.1%. (Until recently, such precision was not available in instrumental
                       analysis.)
                        Systematic errors can be due to calibration, temperature effects, errors in the glassware, drainage
                       errors in using volumetric glassware, failure to allow a meniscus in a burette to stabilize, blowing out
                       a pipette that is designed to drain, improper glassware cleaning methods, and “indicator errors.” These
                       are not subject to prediction by the propagation of error formulas.




                       Comments
                       The general propagation of error model that applies exactly to all linear models z = f(x 1 , x 2 ,…, x n ) and
                       approximately to nonlinear models (provided the relative standard deviations of the measured variables
                       are less than about 15%) is:

                                          σ z ≈  ( ∂z/∂x 1 ) σ 1 + ( ∂z/∂x 2 ) σ 2 + … + ( ∂z/∂x n ) σ n 2
                                                                               2
                                                                  2
                                                                2
                                            2
                                                       2
                                                     2
                       where the partial derivatives are evaluated at the expected value (or average) of the x i . This assumes that
                       there is no correlation between the x’s. We shall look at this and some related ideas in Chapter 49.
                       References

                       Betz Laboratories (1980). Betz Handbook of Water Conditioning, 8th ed., Trevose, PA, Betz Laboratories.
                       Langlier, W. F. (1936). “The Analytical Control of Anticorrosion in Water Treatment,” J. Am. Water Works
                           Assoc., 28, 1500.
                       Miller, J. C. and J. N. Miller (1984). Statistics for Analytical Chemistry, Chichester, England, Ellis Horwood
                           Ltd.
                       Ryznar, J. A. (1944). “A New Index for Determining the Amount of Calcium Carbonate Scale Formed by
                           Water,” J. Am. Water Works Assoc., 36, 472.
                       Spencer, G. R. (1983). “Program for Cooling-Water Corrosion and Scaling,” Chem. Eng., Sept. 19, pp. 61–65.




                       Exercises


                        10.1  Titration. A titration analysis has routinely been done with a titrant strength such that con-
                             centration is calculated from C = 20(y 2  − y 1 ), where (y 2  − y 1 ) is the difference between the final
                             and initial burette readings. It is now proposed to change the titrant strength so that C =
                             40(y 2  − y 1 ). What effect will this have on the standard deviation of measured concentrations?
                        10.2   Flow Measurement. Two flows (Q 1  = 7.5 and Q 2  = 12.3) merge to form a larger flow. The
                             standard deviation of measurement on flows 1 and 2 are 0.2 and 0.3, respectively. What is
                             the standard deviation of the larger downstream flow? Does this standard deviation change
                             when the upstream flows change?

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