Terraforming & Geoengineering

Terraforming Mars: Mass, Forcing, And Industrial Throughput Constraints

By Keith Cowing
Status Report
astro-ph.EP
March 4, 2026
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Terraforming Mars: Mass, Forcing, And Industrial Throughput Constraints
In a futuristic world where teleportation technology has become a reality, a bustling cityscape filled with towering skyscrapers and advanced architecture stands in the background. Amidst this backdrop, a group of diverse individuals, each with unique appearances and expressions, gather around a central chamber equipped with shimmering teleportation devices. The scene captures various stages of teleportation – from individuals floating mid-air before vanishing, to others appearing instantly in their destinations. The lighting is dramatic, with neon lights flickering and casting shadows across the faces of the teleportees. The camera moves between subjects, capturing moments of awe and excitement as they teleport, emphasizing the rapidity and efficiency of the new technology. The futuristic cityscape provides a vivid contrast to the serene yet chaotic scene within the teleportation chamber. Cinematic and high-tech visual style, focusing on the emotional impact of teleportation on the characters. Medium shot and wide shots showcasing the teleportation process. — astro-ph.EP

Terraforming Mars can be evaluated with a small set of system-level feasibility constraints linking (i) target pressures and compositions to required atmospheric inventories, (ii) target surface temperatures to required radiative control authority, (iii) inventories and radiative agents to sustained industrial throughput and power over a build time, and (iv) persistence against collapse, escape, and geochemical sinks.

We use transparent order-of-magnitude scalings to map proposed levers (endogenous CO2 release, synthetic super-greenhouse gases, CO2-H2 CIA, engineered aerosols/nanoparticles, orbital mirrors/albedo modification, and regional solid-state greenhouse “paraterraforming”) onto common metrics {M, τIR/ΔFTOAM˙, P}.

We find: (1) human-relevant pressures imply exaton-class inventories, Matm≃4πR2MarsPs/gMars∼1017-1018 kg; (2) accessible CO2 plausibly provides ≲20 mbar, yielding ≲10 K warming under present insolation; (3) achieving Ts ~ 250-273 K at current insolation requires an effective IR opacity target τIR,eff∼2–4 (uncertain at the ~30-50% level but not altering mass-scale conclusions); (4) breathable endpoints are dominated by O2 and buffer-gas mass and by a minimum oxygenation work ≳1025 J, implying M˙∼107-108 kg\,s−1 and multi-102 TW to PW-class average power for century-to-millennial build times.

We conclude that regional habitability gains via paraterraforming are plausible on near-term industrial scales, whereas global transformation of Mars requires multi-century planetary industry and becomes credible only under conditions of (a) massive exogenous volatile supply or much larger discovered inventories, and (b) sustained high-authority climate control and retention against sinks and loss.

Slava G. Turyshev

Comments: 24 pages, 2 figures, and 10 tables
Subjects: Earth and Planetary Astrophysics (astro-ph.EP); Instrumentation and Methods for Astrophysics (astro-ph.IM)
Cite as: arXiv:2603.00402 [astro-ph.EP] (or arXiv:2603.00402v1 [astro-ph.EP] for this version)
https://doi.org/10.48550/arXiv.2603.00402
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Submission history
From: Slava G. Turyshev
[v1] Sat, 28 Feb 2026 01:30:06 UTC (51 KB)
https://arxiv.org/abs/2603.00402
Astrobiology,

Explorers Club Fellow, ex-NASA Space Station Payload manager/space biologist, Away Teams, Journalist, Lapsed climber, Synaesthete, Na’Vi-Jedi-Freman-Buddhist-mix, ASL, Devon Island and Everest Base Camp veteran, (he/him) 🖖🏻