Radiative imbalance with the sky → Chemical fuel
Radiative imbalance with the skyRadiative sky coolingTemperature gradientSoret effectConcentration gradientChemiosmosisChemical fuel
Epistemic state of the route
- known constituent relations
- 6 / 6 established or replicated · weakest constituent replicated
- constituent maturity floor
- K4 · experimentally observed
- search for this exact route
- Not assessed — complete composition not searched.
- recorded-pathway overlap
- shares its closing relations with Chemiosmotic ATP synthesis · 2/6 relations shared
- route-level evidence
- 0 sources for the complete composition · 8 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.12 × C.20 · Radiative imbalance with the sky × Photothermalfamily: PhotothermalD.12 × C.33 · Radiative imbalance with the sky × Thermodiffusivefamily: ThermodiffusiveD.12 × C.30 · Radiative imbalance with the sky × Biologicalfamily: Biological
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).
- Radiative cooling power bound · resource-bound · listed, never decisivenet cooling power ≲ 100–150 W/m² under a clear sky
- 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
- Onsager–Casimir reciprocity · constitutive-relation · listed, never decisiveL_ij(B) = ε_i ε_j L_ji(−B): the cross-coefficients of coupled linear transport are equal up to the time-reversal parities ε of the variables and reversal of the magnetic field; L_ij = L_ji is the zero-field, even-parity case
Steps
- 01radiative → thermal
- an emitter with high emissivity in the 8–13 µm window and high solar reflectance
- a clear sky; humidity and cloud close the window
refs [1] [2] [3] - 02thermal → thermal
- the cooled surface sits a few kelvin below ambient air
refs [1] [4] [3] - 03thermal → chemical · loss to thermal
- a liquid mixture or solution under a steady temperature gradient
liquid · temperature gradient requiredrefs [5] [6] - 04
- 05chemical → chemical · loss to thermal
- a proton gradient across a membrane containing ATP synthase
aqueous medium required · selective membrane required · room temperaturerefs [7] [8] - 06chemical → chemical · loss to thermal
- ATP synthesised from ADP and phosphate
refs [7] [8]
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 · 8
- [1]A. P. Raman et al.. Passive radiative cooling below ambient air temperature under direct sunlight (2014)
- [2]Y. Zhai et al.. Scalable-manufactured randomized glass-polymer hybrid metamaterial for daytime radiative cooling (2017)
- [3]J.-l. Kou et al.. Daytime radiative cooling using near-black infrared emitters (2017)
- [4]A. P. Raman, W. Li, S. Fan. Generating light from darkness (2019)
- [5]C. Soret. Sur l'état d'équilibre que prend au point de vue de sa concentration une dissolution saline primitivement homogène dont deux parties sont portées à des températures différentes (1879)
- [6]S. R. de Groot, P. Mazur. Non-Equilibrium Thermodynamics (1962)
- [7]P. Mitchell. Coupling of phosphorylation to electron and hydrogen transfer by a chemi-osmotic type of mechanism (1961)
- [8]D. G. Nicholls, S. J. Ferguson. Bioenergetics (4th ed.) (2013)
Cite this route
Physical Transformation Atlas (2026). route p-2285331ae7: Radiative imbalance with the sky → Radiative sky cooling → Temperature gradient → Soret effect → Concentration gradient → Chemiosmosis → Chemical fuel. Dataset revision rbfbfcbb70e57 (hash of the canonical data). https://physical-transformation-atlas.wldud5192.workers.dev/path/2285331ae7
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.