Abstract

The paper analyzes the change in the entropy production of an open thermodynamic forest ecosystem, in which processes associated with the entry of a negative entropy flow into it can be realized. Using the example of computer modeling of the dynamics of effective specific entropy production for a single-pedigree stand, it is shown for the first time that the specific entropy production as a function of time corresponds to the Prigogine-Glensdorf principle, and the time to reach a stationary state coincides with experimental values from forestry tables.

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