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Sometime during the mid-1970's it became apparent that ecological
modeling in the form of a set of coupled, deterministic differential
equations was not going to be the panacea for analyzing whole
ecosystems. In the search for alternative methods of describing
the behavior of total ecosystems, various computations performed
on the underlying network of flows have figured prominently (SCOR,
1981). The intention in writing these subroutines has been to
collect the various algorithms into a single large program which
allows an investigator to choose that analysis which best serves
his needs. It is also hoped that by comparing the results of different
methods (sometimes operating at different levels of aggregation)
new insights will appear which would not have been possible by
confining one's attention to a single approach.
Four types of analyses are performed by this routine. The outputs
are presented in ascending degree of network aggregation. First,
input-output structure matrices are calculated, allowing one to
look in detail at the effects any particular flow or transformation
might have on any other given species or flow. Next, the graph
is mapped into a concatonated trophic chain (after Lindeman).
Then all the simple, directed biogeochemical cycles are identified
and separated from their supporting dissipative flows. Finally,
global variables describing the state of development of the network
are presented.
(Adapted from the documentation)
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