Physical Transformation AtlasPTA
Pathway · p-463a71ab6b · candidate

Incident radiation flux → Chemical fuel

Incident radiation fluxPhotothermal absorptionTemperature gradientThermochemical redox cycleChemical fuel (H₂, CO, syngas)Chemical fuel

Epistemic state of the route

known constituent relations
5 / 5 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 Concentrating solar-thermal plant · 2/5 relations shared
route-level evidence
0 sources for the complete composition · 4 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.11 × C.20 · Incident radiation flux × Photothermalfamily: PhotothermalD.11 × C.29 · Incident radiation flux × 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).

  • Landsberg limit · formula-bound · hard, applies to this route
    η ≤ 1 − (4/3)(T_c/T_s) + (1/3)(T_c/T_s)⁴ for conversion of blackbody radiation at T_s with a sink at T_c; 93.3 % at 6000 K / 300 K
  • Carnot limit · formula-bound · hard, applies to this route
    η ≤ 1 − T_c/T_h for any heat engine between reservoirs at T_h and T_c

Steps

  1. 01
    radiative → thermal
    • an absorber with high solar absorptance; selective surfaces suppress re-emission
    illumination required
    refs [1] [2]
  2. 02
    thermal → thermal
    refs [1]
  3. 03
    thermal → 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 K
    refs [3] [4]
  4. 04
    chemical → chemical
    refs [4]
  5. 05
    chemical → chemical
    refs [3]

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 · 4

  1. [1]
    A. Bejan. Advanced Engineering Thermodynamics (4th ed.) (2016)
    Wiley · doi:10.1002/9781119245964 · crossref ✓ 2026-09-19 · record
  2. [2]
    P. T. Landsberg, G. Tonge. Thermodynamic energy conversion efficiencies (1980)
    Journal of Applied Physics 51, R1–R20 · doi:10.1063/1.328187 · crossref ✓ 2026-09-19 · record
  3. [3]
    A. Steinfeld. Solar thermochemical production of hydrogen––a review (2005)
    Solar Energy 78, 603-615 · doi:10.1016/j.solener.2003.12.012 · crossref ✓ 2026-09-20 · record
  4. [4]
    S. Abanades. Redox Cycles, Active Materials, and Reactors Applied to Water and Carbon Dioxide Splitting for Solar Thermochemical Fuel Production: A Review (2022)
    Energies 15, 7061 · doi:10.3390/en15197061 · crossref ✓ 2026-09-20 · record

Cite this route

Physical Transformation Atlas (2026). route p-463a71ab6b: Incident radiation flux → Photothermal absorption → 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/463a71ab6b

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.