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

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that all water will spend 100 days in the lake. Some will bypass in only 10 days,<br />

and some will persist in backwaters for 1000 days but, on average, the residence<br />

time will be 100 days.<br />

The reason that this concept is so important is that chemicals exhibit variable<br />

lifetimes, ranging from hours to decades. As a result, the amount of chemical present<br />

in the environment, i.e., the inventory of chemical, varies greatly between chemicals.<br />

We tend to be most concerned about persistent and toxic chemicals, because relatively<br />

small emission rates (E) can result in large amounts (M) present in the<br />

environment. This translates into high concentrations and possibly severe adverse<br />

effects. A further consideration is that chemicals that survive for prolonged periods<br />

in the environment have the opportunity to make long and often tortuous journeys.<br />

If applied to soil, they may evaporate, migrate onto atmospheric particles, deposit<br />

on vegetation, be eaten by cows, be transferred to milk, and then consumed by<br />

humans. Chemicals may migrate up the food chain from water to plankton to fish<br />

to eagles, seals, and bears. Short-lived chemicals rarely survive long enough to<br />

undertake such adventures (or misadventures).<br />

This lengthy justification leads to the conclusion that, if we are going to discharge<br />

a chemical into the environment, it is prudent to know<br />

1. how long the chemical will survive, i.e., t, and<br />

2. what causes its removal or “death”<br />

This latter knowledge is useful, because it is likely that situations will occur in<br />

which a common removal mechanism does not apply. For example, a chemical may<br />

be potentially subject to rapid photolysis, but this is not of much relevance in long,<br />

dark arctic winters or in deep, murky sediments.<br />

In the process of quantifying this effect, we will introduce rate constants, advective<br />

flow rates and, ultimately, using the fugacity concept, quantities called D values,<br />

which prove to be immensely convenient. Indeed, armed with Z values and D values,<br />

the environmental scientist has a powerful set of tools for calculation and interpretation.<br />

It transpires that there are two primary mechanisms by which a chemical is<br />

removed from our environment: advection and reaction, which we discuss individually<br />

and then in combination.<br />

©2001 CRC Press LLC<br />

6.2 ADVECTION<br />

Strangely, “advection” is a word rarely found in dictionaries, so a definition is<br />

appropriate. It means the directed movement of chemical by virtue of its presence<br />

in a medium that happens to be flowing. A lazy canoeist is advected down a river.<br />

PCBs are advected from Chicago to Buffalo in a westerly wind. The rate of advection<br />

N (mol/h) is simply the product of the flowrate of the advecting medium, G (m3 /h),<br />

and the concentration of chemical in that medium, C (mol/m3),<br />

namely,<br />

N = GC mol/h

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