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ENVIRONMENTAL CONSEQUENCES in rocky mountain coniferous ...

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DISCUSSION<br />

It is important to note that for the unlikely situation where<strong>in</strong> the change <strong>in</strong><br />

state of a particular component, Xi, dur<strong>in</strong>g any time <strong>in</strong>terval, At, is unaffected by<br />

either its own state or the state of any other environmental component (i<br />

b = 0; j = 1 ,... ,n) equation 12 merely predicts that<br />

i j<br />

.em, that<br />

or that the change <strong>in</strong> Xi dur<strong>in</strong>g the <strong>in</strong>terval from t to t+At equals the change <strong>in</strong> Xi<br />

dur<strong>in</strong>g the previous <strong>in</strong>terval from t-At to t--not an unreasonable outcome.<br />

Note also that, for the situation where<strong>in</strong> the change <strong>in</strong> state of the ith component<br />

is affected only by its current state, and not by the state of any other<br />

component, equation 12 reduces to<br />

An example of this latter situation would be one where the rate of growth <strong>in</strong><br />

population of a particular organism is either retarded or accelerated only by the<br />

level of its current popul ation--the exponential growth function.<br />

F<strong>in</strong>ally, we should elaborate on the mean<strong>in</strong>g of the biits, and the correspond<strong>in</strong>g<br />

challenge to researchers and staff special i sts. ~eferr<strong>in</strong>~- to figure 14, note that<br />

b is the <strong>in</strong>stantaneous slope of dXi/dt under the condition that noth<strong>in</strong>g <strong>in</strong> the<br />

ij<br />

environment is chang<strong>in</strong>g except X and dXi/dt. Similarily bix is the <strong>in</strong>stantaneous<br />

j<br />

slope of dXi/dt given that noth<strong>in</strong>g is chang<strong>in</strong>g except Xk and dX 1 ./dt. When us<strong>in</strong>g a<br />

1 <strong>in</strong>ear approximation as <strong>in</strong>dicated <strong>in</strong> figure 13, however, we are actually def<strong>in</strong><strong>in</strong>g<br />

b as the average slope of the dXi'/dt vs. X . relationship dur<strong>in</strong>g the time <strong>in</strong>terval<br />

i j 3<br />

At. The units of byj are the dimensions of dXi/dt divided by the dimensions of X j'<br />

Geometrical <strong>in</strong>terpretation of first partial derivatives<br />

Figure 14. --&ornetria2 <strong>in</strong>teqpretation of<br />

first partial deriva+iues.

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