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Modeling Tools for Environmental Engineers and Scientists

Modeling Tools for Environmental Engineers and Scientists

Modeling Tools for Environmental Engineers and Scientists

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ChemicalinjectionAirMassinjectedm1AqueousphasecontentX1GasphasecontentY1Ym2X2Y2Waterm3X3Y3m4X4Y4Magneticstirrerm5X5Y500XFigure 4.1 Linear partitioning in air-water binary system.where, K a–w is the nondimensional air-water partition coefficient (–). Similarpartitioning phenomena can be observed between other phases as well. Someof the more common two-phase environmental systems <strong>and</strong> the appropriatepartition coefficients <strong>for</strong> those systems are summarized in Appendix 4.1. It isimperative that these definitions be used consistently to avoid confusionabout units <strong>and</strong> inverse ratios, i.e., K 1–2 vs. K 2–1 .Experimentally measured data <strong>for</strong> many of these partition coefficients canbe found in h<strong>and</strong>books <strong>and</strong> the literature. Alternatively, structure activity relationship(SAR) or property activity relationship (PAR) methods have alsobeen proposed to estimate them from molecular structures or other physicochemicalproperties. A comprehensive compilation of such estimation methodscan be found in Lyman et al. (1982).4.3.1 STEADY STATE AND EQUILIBRIUMThe concept of steady state has been referred to previously, implying nochanges with passage of time. The equilibrium conditions discussed abovealso imply no change of state with passage of time. The following illustrationadapted from Mackay (1991) provides a clear underst<strong>and</strong>ing of the similarities<strong>and</strong> differences between the two concepts.Consider the oxygen concentrations in the water <strong>and</strong> air, first, in a closedair-water binary system as shown in Figure 4.2(a). After a sufficiently longtime, the system will reach equilibrium conditions with an oxygen contentof 8.6 × 10 –3 mole/L <strong>and</strong> 2.9 × 10 –4 mole/L in the gas <strong>and</strong> aqueous phase,respectively. The system will remain under these conditions, seen as steadystate. Consider now the flow system in Figure 4.2(b). The flow rates remainconstant with time, keeping the oxygen contents the same as be<strong>for</strong>e. The systemnot only is at steady state, but also is at equilibrium, because the ratio of© 2002 by CRC Press LLC

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