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McKay, Donald. "Front matter" Multimedia Environmental Models ...

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ates can thus be used to estimate mass transfer coefficients for other solutes having<br />

similar (large) H such as alkanes. Indeed, an ingenious experimental approach for<br />

determining k 2 for oxygen is to use a volatile hydrocarbon, such as propane, as a<br />

tracer, thus avoiding the complications of biotic oxygen consumption or generation,<br />

which confound environmental measurements of oxygen concentration change. It is<br />

erroneous to use k 2 to estimate the rate of volatilization of a chemical with low H,<br />

since k 2 contains negligible air phase resistance information. A correction should<br />

also be applied for the effect of molecular diffusivity, preferably using the dimensionless<br />

form of diffusivity, the Schmidt number raised to a power such as –0.5 or<br />

–0.67.<br />

This technique of probing interfacial MTCs by measuring N for various chemicals<br />

can be applied in other areas. When chemical is taken up by fish, it appears<br />

that it passes through one or more water layers and one or more organic membranes<br />

in series. By analogy with air-water transfer, we can write an organic membranewater<br />

transfer equation simply by replacing subscript A by subscript M, giving<br />

where<br />

©2001 CRC Press LLC<br />

N = k OWA(C W – C M/K OW)<br />

1/k OW = 1/k W + 1/k MK MW<br />

or more conveniently changing to an overall organic phase MTC, k OM,<br />

where<br />

N = k OMA(C WK MW – C M)<br />

1/k OM = 1/k M + K MW/k W<br />

A plot of 1/k OM versus K MW, the organic-water or octanol-water partition coefficient,<br />

gives 1/k M as intercept and 1/k W as slope. This is essentially the fish bioconcentration<br />

equation (discussed in more detail in Chapter 8) in disguise, which is<br />

conventionally written<br />

dC F/dt = k 1C W – k 2C F<br />

where V F is fish volume and C O is C F/L, where L is the volume fraction lipid<br />

(equivalent to octanol) in the fish. It follows that<br />

dC F/dt = (k OMA/V F)(C WK MW – C F/L)<br />

k 1 is obviously K OWk OMA/V F, and k 2 is [k OMA/(V FL)]. k 1/k 2 is then LK OW, the bioconcentration<br />

factor. The area of the respiring gill surface is uncertain as is k OM, so<br />

it is convenient to lump these uncertainties in one unknown k 2. This suggests plotting

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