Concentration gradient → Mechanical work
Concentration gradientOsmosisOsmotic pressure differencePressure-retarded osmosisHydraulic pressureAerodynamic and hydrodynamic liftMechanical motionMechanical work
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
- none recorded
- route-level evidence
- 0 sources for the complete composition · 5 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.03 × C.22 · Concentration gradient × Osmotic / salinity-gradientfamily: Osmotic / salinity-gradientD.03 × C.24 · Concentration gradient × 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).
- Free energy of mixing · resource-bound · listed, never decisiveW ≤ −ΔG_mix ≈ 0.8 kWh per m³ of fresh water into seawater
- Betz limit · upper-bound · hard, filtered out by its applicabilityC_p ≤ 16/27 ≈ 59.3% of the kinetic power through the rotor disc
Steps
- 01chemical → osmoticaqueous medium required · selective membrane requiredrefs [1]
- 02
- 03osmotic → mechanical · loss to thermalaqueous medium required · selective membrane requiredrefs [2] [3]
- 04mechanical → mechanicalrefs [2] [3]
- 05mechanical → mechanical · loss to thermal
- pressurised water expanded through a reaction or impulse turbine
liquid · bulk flow requiredrefs [4] - 06mechanical → mechanicalrefs [4]
- 07mechanical → mechanical · loss to thermalrefs [5]
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 · 5
- [1]A. J. Bard, L. R. Faulkner. Electrochemical Methods: Fundamentals and Applications (2nd ed.) (2001)
- [2]S. Loeb. Osmotic power plants (1975)
- [3]B. E. Logan, M. Elimelech. Membrane-based processes for sustainable power generation using water (2012)
- [4]S. L. Dixon, C. A. Hall. Fluid Mechanics and Thermodynamics of Turbomachinery (7th ed.) (2014)
- [5]A. Bejan. Advanced Engineering Thermodynamics (4th ed.) (2016)
Cite this route
Physical Transformation Atlas (2026). route p-1237087cfc: Concentration gradient → Osmosis → Osmotic pressure difference → Pressure-retarded osmosis → Hydraulic pressure → Aerodynamic and hydrodynamic lift → Mechanical motion → Mechanical work. Dataset revision rbfbfcbb70e57 (hash of the canonical data). https://physical-transformation-atlas.wldud5192.workers.dev/path/1237087cfc
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.