Temperature gradient → Mechanical work
Temperature gradientMarangoni effectFluid flowFlow-induced vibrationMechanical vibrationResonant vibrationMechanical 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
- shares relations, in order, with Electromagnetic vibration harvester · 2/7 relations shared
- route-level evidence
- 0 sources for the complete composition · 7 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.01 × C.34 · Temperature gradient × Marangonifamily: Marangoni
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).
- 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
- 01thermal → kinetic · loss to thermal
- thermocapillary case: surface tension falls with temperature, so a temperature gradient along the interface drives flow toward the cold side
liquid · temperature gradient requiredrefs [1] [2] - 02
- 03kinetic → mechanical · loss to thermal
- a bluff or flexible body in the produced stream at a Reynolds number where vortex shedding locks to a structural mode
bulk flow requiredrefs [3] - 04mechanical → mechanicalrefs [3]
- 05mechanical → mechanical · loss to thermal
- a cantilever or seismic mass with natural frequency near the excitation
solidrefs [4] [5] - 06mechanical → mechanicalrefs [6] [5]
- 07mechanical → mechanical · loss to thermalrefs [7]
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 · 7
- [1]L. E. Scriven, C. V. Sternling. The Marangoni Effects (1960)
- [2]Q. Dai et al.. Directional interfacial motion of liquids: Fundamentals, evaluations, and manipulation strategies (2021)
- [3]H. B. Radousky, H. Liang. Energy harvesting: an integrated view of materials, devices and applications (2012)
- [4]S. Roundy, P. K. Wright, J. Rabaey. A study of low level vibrations as a power source for wireless sensor nodes (2003)
- [5]A. Erturk, D. J. Inman. Piezoelectric Energy Harvesting (2011)
- [6]S. P. Beeby, et al.. A micro electromagnetic generator for vibration energy harvesting (2007)
- [7]A. Bejan. Advanced Engineering Thermodynamics (4th ed.) (2016)
Cite this route
Physical Transformation Atlas (2026). route p-1e5ebf4009: Temperature gradient → Marangoni effect → Fluid flow → Flow-induced vibration → Mechanical vibration → Resonant vibration → Mechanical motion → Mechanical work. Dataset revision rbfbfcbb70e57 (hash of the canonical data). https://physical-transformation-atlas.wldud5192.workers.dev/path/1e5ebf4009
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.