Nuclear binding-energy difference → Chemical fuel
Nuclear binding-energy differenceRadioactive decayBeta particlesRadioisotope heatingTemperature gradientThermochemical redox cycleChemical fuel (H₂, CO, syngas)Chemical fuel
Epistemic state of the route
- known constituent relations
- 7 / 7 established or replicated · weakest constituent established
- constituent maturity floor
- K4 · experimentally observed
- search for this exact route
- Not assessed — complete composition not searched.
- recorded-pathway overlap
- shares relations, in order, with Radioluminescent (beta-photovoltaic) nuclear battery · 2/7 relations shared
- route-level evidence
- 0 sources for the complete composition · 3 cited by the constituent steps
- boundaries and interfaces
- BOUNDARY compatible · no region transition
Explorematrix context · physics checks · steps · route evidence · constituent evidence · cite
Matrix context
D = disequilibrium row · C = coupling family column. A cell reads the state of the atlas for that pair.
D.20 × C.27 · Nuclear binding-energy difference × Nuclear heatfamily: Nuclear heatD.20 × C.29 · Nuclear binding-energy difference × Thermochemicalfamily: Thermochemical
Typed bounds on this route
Every limit the atlas holds for this route, as constraint records: reached through bounded_by claims on the route's own entities. Hard bounds (an upper bound or a formula) decide the thermodynamic-bound check above; benchmarks, constitutive relations and resource limits are listed and never decisive. No prose limit exists anywhere (pass 42).
- Carnot limit · formula-bound · hard, applies to this routeη ≤ 1 − T_c/T_h for any heat engine between reservoirs at T_h and T_c
Steps
- 01nuclear → nuclearradioisotope requiredrefs [1]
- 02nuclear → nuclear
- beta emitters such as tritium, Ni-63, Pm-147, Sr-90
refs [1] - 03nuclear → thermal
- beta particles stopped within the source and its cladding; in practice RTG heat comes from alpha emitters (see the alpha claim)
radioisotope requiredrefs [1] - 04thermal → thermalrefs [1]
- 05thermal → chemical · loss to thermal
- a redox-active metal oxide (ceria, ferrites) reduced at 1400–1800 K, typically in a solar receiver, and re-oxidised by H₂O or CO₂ at 800–1200 K
above ~700 Krefs [2] [3] - 06chemical → chemicalrefs [3]
- 07chemical → chemicalrefs [2]
Evidence for the complete composition · 0
No source on record for this exact composition. The sources below support the individual steps, not the route as a whole.
Evidence for the constituent relations · 3
- [1]M. A. Prelas, et al.. A review of nuclear batteries (2014)
- [2]A. Steinfeld. Solar thermochemical production of hydrogen––a review (2005)
- [3]S. Abanades. Redox Cycles, Active Materials, and Reactors Applied to Water and Carbon Dioxide Splitting for Solar Thermochemical Fuel Production: A Review (2022)
Cite this route
Physical Transformation Atlas (2026). route p-ffa311f9d8: Nuclear binding-energy difference → Radioactive decay → Beta particles → Radioisotope heating → Temperature gradient → Thermochemical redox cycle → Chemical fuel (H₂, CO, syngas) → Chemical fuel. Dataset revision rbfbfcbb70e57 (hash of the canonical data). https://physical-transformation-atlas.wldud5192.workers.dev/path/ffa311f9d8
Ids and matrix addresses are stable across revisions; the revision hash identifies the exact canonical files the record was compiled from and is meta.data_hash in every /api export. Reuse terms: see the license field in any export.