Radiative imbalance with the sky → Electrical work
Radiative imbalance with the skyRadiative sky coolingTemperature gradientAlkali-metal thermal-to-electric conversionIonic currentElectrical work
Epistemic state of the route
- known constituent relations
- 3 / 5 established or replicated · weakest constituent demonstrated
- 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 AMTEC cell · 3/5 relations shared
- route-level evidence
- 0 sources for the complete composition · 6 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.21 · Radiative imbalance with the sky × Electrochemicalfamily: Electrochemical
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
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 → electrical · loss to thermal
- sodium at 900–1300 K on the hot side of a β″-alumina electrolyte and a condenser at 400–700 K
above ~700 K · liquidrefs [5] - 04electrical → electricalrefs [5]
- 05electrical → electrical · loss to thermal
- electrodes exchange the ionic current for an electronic current through the external load
refs [6]
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 · 6
- [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]T. Cole. Thermoelectric energy conversion with solid electrolytes (1983)
- [6]A. J. Bard, L. R. Faulkner. Electrochemical Methods: Fundamentals and Applications (2nd ed.) (2001)
Cite this route
Physical Transformation Atlas (2026). route p-944bb9e97c: Radiative imbalance with the sky → Radiative sky cooling → Temperature gradient → Alkali-metal thermal-to-electric conversion → Ionic current → Electrical work. Dataset revision rbfbfcbb70e57 (hash of the canonical data). https://physical-transformation-atlas.wldud5192.workers.dev/path/944bb9e97c
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.