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

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models. Most interest is in LRT in the atmosphere but, in some cases, oceans and<br />

rivers can play a significant role. Even migrating biota can contribute to LRT. The<br />

most promising approach is to consider the fate of chemical in a parcel of Lagrangian<br />

air passing over soil or water and subject to degradation, deposition, and reevaporation.<br />

Such systems have been suggested by Van Pul (1998), Bennett et al. (1999),<br />

and Beyer et al. (2000). Beyer et al. (2000) showed that a LRT distance in air can<br />

be deduced from a simple Level III model as the product of the wind velocity, the<br />

overall persistence or residence time of the chemical, and the fraction of the chemical<br />

in the atmosphere.<br />

A model, TaPL3 (Transport and Pesistence Level 3), can be used for a Level III<br />

evalution of persistence and LRT. It is available on the website.<br />

It is expected that new models will be developed to assist in the evaluation of<br />

these attributes, especially in situations where there is no easy method of obtaining<br />

the required information from environmental monitoring data.<br />

©2001 CRC Press LLC<br />

8.16 GLOBAL MODELS<br />

The ultimate mass balance model of chemical fate is one that describes the<br />

dynamic behavior of the substance in the entire global environment. At present, only<br />

relatively simplistic treatments of chemical fate at this scale have been accomplished,<br />

but it is likely that more complex and accurate models will be produced in the future.<br />

Meteorologists can now describe the dynamic behavior of the atmosphere in some<br />

detail. Oceanographers are able to describe ocean currents. Ultimately, there may<br />

be linked meteorological/oceanographic/terrestrial models in which the ultimate fate<br />

of 100 kg of DDT applied in Mexico can be predicted over the decades in which it<br />

migrates globally.<br />

The obvious ethical implication is that a nation should not use a substance in<br />

such a way that other nations suffer significant exposure and adverse effects. These<br />

situations have already occurred with acid rain and Arctic and Antarctic contamination<br />

by persistent organic substances.<br />

The construction of global-scale models opens up many new and interesting<br />

prospects. It appears that there is a global fractionation phenomenon as a result of<br />

chemicals migrating at different rates and tending to condense at lower temperatures.<br />

Chemicals that do reach cold regions may be better preserved there because of the<br />

reduced degradation rates. Chemicals appear to be subject to “grasshopping” (or<br />

“kangarooing” in the Southern Hemisphere) as they journey, deposit, evaporate, and<br />

continue hopping from place to place until they are ultimately degraded as shown<br />

in Figure 8.13.<br />

Accounts of these phenomena, and models that attempt to quantify them, are<br />

given in a series of papers by Wania and Mackay (1993, 1996, 1999) and Wania et<br />

al. (1996). The most successful modeling to date has been of a-HCH, which was<br />

produced as an impurity in the insecticide, technical lindane (Wania and Mackay,<br />

1999) but is no longer produced. An interesting insight from that study is an assertion<br />

that, despite a-HCH never having been used in the Arctic, about half the remaining<br />

mass on this planet now resides in the arctic oceans. This GloboPOP model is

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