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ENVIRONMENTAL CONSEQUENCES in rocky mountain coniferous ...

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understory biomass density, X2 represents soil nutrient concentration, Xg represents<br />

average soil moisture content, and XI+, Xg, ... Xn represent the rema<strong>in</strong>der of the<br />

forest environment be<strong>in</strong>g considered. Suppose further that we know the level of soil<br />

nutrients 1 imi ts understory growth <strong>in</strong> this situation, and that a1 1 other environmental<br />

components that would promote growth are at or above critical levels while all that<br />

would retard growth are at or below critical levels (e.g. , <strong>in</strong>creas<strong>in</strong>g soil moisture<br />

would not accelerate growth). In this situation, we would simply conclude that the<br />

change <strong>in</strong> XI, say AX1, over the ensu<strong>in</strong>g time period, At, would be determ<strong>in</strong>ed by the<br />

level of nutrients, X2, dur<strong>in</strong>g the same period. The amount of change, AX1 = AX129<br />

would be based on data from the research literature or, <strong>in</strong> its absence, on profes-<br />

sional op<strong>in</strong>ion. This same thought process would be followed for each of the n<br />

environmental components. result<strong>in</strong>g <strong>in</strong> an estimate of AXi for each, and a corre-<br />

spond<strong>in</strong>g estimate of its new status, or<br />

where Xi is the status of the ith component at t<strong>in</strong>e t; and Xi,t+At is the status<br />

, t<br />

of the ith component at some later time, t + At (fig. 11 ).<br />

Figure 10. --Pt-edictions based on -<br />

Zimit<strong>in</strong>a <strong>in</strong>teractions.<br />

I I I<br />

t t +at Time<br />

-<br />

x 1<br />

Figure 11. --IZZustration of quat ti on 4.<br />

- 508-

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