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THE GREAT LAKES

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knowledge of the entropy flow, the total yalue of the timedependent<br />

entropy is unknown, and that means it is<br />

impossible to predict favored trajectories and outcomes.<br />

Thus, thermodynamics does not provide a general theory of<br />

evolution in far from equilibrium situations.<br />

A few systems have predictable evolutionary<br />

trajectories and outcomes no matter how far from<br />

equilibrium they are. These include<br />

1) the isolated system (system exchanges neither energy<br />

nor materials with the surroundings); and<br />

2) the closed and open systems (a system exchanging energy<br />

but no materials with the surroundinqs, and a system<br />

exchanging both energy and mateGials with- the<br />

surroundings, respectively) in which all the rate<br />

. processes have linear phenomenological (rate) laws.<br />

An isolated system has no entropy flow, and evolves to a<br />

state of maximum entropy whereupon it ceases to change.<br />

Ecological examples are organism death and species<br />

extinction in isolated environments. Closed and open<br />

systems with only linear rate laws evolve through a suite<br />

of predictable steady states to a final steady state of<br />

minimum free energy (not always a thermodynamic<br />

equilibrium) consistent with any external constraints on<br />

energy and material flows. An analysis of force-flux<br />

relationships in systems with linear phenomenological laws<br />

shows that both entropy flow and entropy production are<br />

positive. All final states are stable and withstand<br />

perturbations or fluctuations in various parameters.<br />

Ecological examples include autotrophic growth in a<br />

nutrient-limited environment and diffusional processes in<br />

marine plankton leading to patchy and nonpatchy<br />

biogeographic distributions.<br />

Most ecological systems of interest are open and have<br />

some nonlinear dynamics. What happens then? A unique<br />

thermodynamic equilibrium still exists. Near to<br />

equilibrium, the f orce-f lux relationships are linear, a<br />

consequence of truncating the Taylor series expansions of<br />

these relationships at the linear terms. Thus, nonlinear<br />

systems have linear dynamics and behave like linear<br />

systems: they follow the thermodynamic branch. Far from<br />

equilibrium, the f orce-f lux equations are nonlinear.<br />

Depending on the nonlinearities, the analysis may reveal<br />

one or more of the following:

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