Radiative imbalance with the sky → Mechanical work
Radiative imbalance with the skyRadiative sky coolingTemperature gradientThermo-osmosisFluid flowAerodynamic and hydrodynamic liftMechanical motionMechanical work
Epistemic state of the route
- known constituent relations
- 7 / 7 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 relations, in order, with Thermal-osmosis electrokinetic generator · 2/7 relations shared
- route-level evidence
- 0 sources for the complete composition · 10 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.37 · Radiative imbalance with the sky × Thermo-osmoticfamily: Thermo-osmoticD.12 × C.24 · Radiative imbalance with the sky × Turbomachineryfamily: Turbomachinery
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
- Betz limit · upper-bound · hard, filtered out by its applicabilityC_p ≤ 16/27 ≈ 59.3% of the kinetic power through the rotor disc
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 → kinetic · loss to thermal
- a membrane separating two reservoirs of the same liquid at different temperatures; the flow direction depends on the membrane–liquid interaction
selective membrane required · temperature gradient required · liquidrefs [5] [6] - 04kinetic → kineticConfined in a nanochannel (Zhao 2020) or collected as a pressurised bulk flow: Straub et al. 2016 measured 3.53 W/m² of hydraulic power from the thermo-osmotic flux, so the produced flow can load a turbine.refs [5] [7]
- 05kinetic → mechanical · loss to thermal
- a rotor or vane in the produced stream at a working angle of attack; the driven flow must carry a directed momentum flux for a blade to load
bulk flow requiredrefs [8] [9] - 06mechanical → mechanicalrefs [9]
- 07mechanical → mechanical · loss to thermalrefs [10]
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 · 10
- [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]V. M. Barragán, S. Kjelstrup. Thermo-osmosis in Membrane Systems: A Review (2017)
- [6]S. R. de Groot, P. Mazur. Non-Equilibrium Thermodynamics (1962)
- [7]A. P. Straub et al.. Harvesting low-grade heat energy using thermo-osmotic vapour transport through nanoporous membranes (2016)
- [8]A. Betz. Das Maximum der theoretisch möglichen Ausnützung des Windes durch Windmotoren (1920)
- [9]S. L. Dixon, C. A. Hall. Fluid Mechanics and Thermodynamics of Turbomachinery (7th ed.) (2014)
- [10]A. Bejan. Advanced Engineering Thermodynamics (4th ed.) (2016)
Cite this route
Physical Transformation Atlas (2026). route p-b778e6a6d6: Radiative imbalance with the sky → Radiative sky cooling → Temperature gradient → Thermo-osmosis → Fluid flow → Aerodynamic and hydrodynamic lift → Mechanical motion → Mechanical work. Dataset revision rbfbfcbb70e57 (hash of the canonical data). https://physical-transformation-atlas.wldud5192.workers.dev/path/b778e6a6d6
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.