The Physics of Sustainability: Material and Power Constraints for the Long Term
José Halloy, Petros Chatzimpiros, François Graner, Thomas Gregor
TL;DR
The paper reframes sustainability as a biophysical problem grounded in the Earth’s status as a materially closed but energetically open system driven by a solar flux of approximately $10^{17}$ W. It contrasts slow, circular biogeochemical cycling with fast, stock-based industrial metabolism, highlighting a systemic overshoot of planetary boundaries and the limits of green-growth rhetoric. The authors advocate a dual path: (i) degrowth to reduce total material and power throughput within biospheric limits, and (ii) life-compatible technologies that operate on renewable solar fluxes, with low power density and circular materiality. Together, these shifts provide a framework for long-term viability, requiring interdisciplinary collaboration and a redefinition of energy transition beyond conventional electrification and substitution.
Abstract
Much of today's sustainability discourse emphasizes efficiency, clean technologies, and smart systems, but largely underestimates fundamental physical constraints relating to energy-matter interactions. These constraints stem from the fact that Earth is a materially closed yet energetically open system, driven by the sustained but low power-density flux of solar radiation. This Perspective reframes sustainability within these axiomatic limits, integrating relevant timescales and orders of magnitude. We argue that fossil-fueled industrial metabolism is inherently incompatible with long-term viability, while post-fossil systems are surface-, materials-, and power-intensive. Long-term sustainability must therefore be defined not only by how much energy or material is used, but also by how it is used: favoring organic, carbon-based chemistry with limited reliance on purified metals, operating at low power density, and maintaining low throughput rates. Achieving this requires radical technological shifts toward life-compatible systems and biogeochemical circular processes, and, likely as a consequence, a paradigm change toward degrowth to a steady-state. These two shifts are mutually reinforcing and together provide the necessary foundation for any viable future.
