How does the earth system generate and maintain thermodynamic disequilibrium and what does it imply for the future of the planet?
Axel Kleidon

TL;DR
This paper applies non-equilibrium thermodynamics to quantify Earth's chemical disequilibrium, highlighting life as the main energy source, and discusses sustainable human energy use and planetary engineering to maintain Earth's free energy generation.
Contribution
It introduces a thermodynamic framework to quantify Earth's disequilibrium and demonstrates that life significantly drives free energy generation, with implications for sustainable future energy strategies.
Findings
Life generates orders of magnitude more free energy than abiotic processes.
Earth's maximum thermodynamic efficiency is much less than Carnot limit.
Human activity consumes significant free energy, affecting Earth's energy budget.
Abstract
The chemical composition of the earths atmosphere far from equilibrium is unique in the solar system and has been attributed to the presence of widespread life. Here I show that this perspective can be quantified using non-equilibrium thermodynamics. Generating disequilibrium in a thermodynamic variable requires the extraction of power from another thermodynamic gradient, and the second law of thermodynamics imposes fundamental limits on how much power can be extracted. When applied to complex earth system processes, where several irreversible processes compete to deplete the same gradients, it is easily shown that the maximum thermodynamic efficiency is much less than the classic Carnot limit, so that the ability of the earth system to generate power and disequilibrium is limited. This approach is used to quantify how much free energy is generated by various earth system processes to…
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